Braxiosaurus - Brachiosaurus

Braxiosaurus
Vaqtinchalik diapazon: Kech yura, 154–153 Ma
Brachiosaurus mount.jpg
Ning qayta tiklangan nusxasi holotip tashqi skelet Tabiat tarixi dala muzeyi
Ilmiy tasnif tahrirlash
Qirollik:Animalia
Filum:Chordata
Klade:Dinozavrlar
Klade:Saurischia
Suborder:Sauropodomorpha
Klade:Sauropoda
Oila:Brachiosauridae
Tur:Braxiosaurus
Riggs, 1903[1]
Turlar:
B. altitoraks
Binomial ism
Brachiosaurus altithorax
Riggz, 1903 yil[1]

Braxiosaurus (/ˌbrækmenəˈsɔːrəs/) a tur ning sauropod dinozavr yashagan Shimoliy Amerika davomida Kech yura, taxminan 154-153 million yil oldin. Bu birinchi edi tasvirlangan amerikalik paleontolog tomonidan Elmer S. Riggz yilda 1903 topilgan qoldiqlardan Kolorado daryosi g'arbiy qismida vodiy Kolorado, Qo'shma Shtatlar. Riggs dinozavrga nom berdi Brachiosaurus altithorax; The umumiy ism bu Yunoncha "qo'l kertenkele" uchun, uning mutanosib ravishda uzun qo'llariga nisbatan va aniq ism "chuqur ko'krak" degan ma'noni anglatadi. Braxiosaurus uzunligi 18 dan 21 metrgacha (59 va 69 fut) bo'lgan deb taxmin qilinadi; vazn hisob-kitoblari 28,3 dan 58 metrik tonnagacha (31,2 va 64 qisqa tonnalar). Uning nomutanosib uzun bo'yni, kichik bosh suyagi va umumiy hajmi katta edi, bularning barchasi sauropodlarga xosdir. Atipik ravishda, Braxiosaurus orqa oyoqlarga qaraganda uzunroq oyoq-qo'llari bor edi, bu esa tik moyillikka olib keldi magistral va mutanosib ravishda qisqaroq quyruq.

Braxiosaurus ning ismdoshlari oila Brachiosauridae, shu kabi bir nechta boshqa sauropodlarni o'z ichiga oladi. Ning eng mashhur tasvirlari Braxiosaurus aslida asoslangan Giraffatitan, brachiosaurid dinozavrining bir turi Tendaguru shakllanishi ning Tanzaniya. Giraffatitan dastlab nemis paleontologi tomonidan tasvirlangan Verner Yanensch turlari sifatida 1914 yilda Braxiosaurus, B. brancai, lekin 2009 yilda o'z turiga o'tdi. Boshqa uchta turi Braxiosaurus Afrika va Evropada topilgan qoldiqlarga asoslangan holda nomlangan; ikkitasi endi haqiqiy deb hisoblanmaydi, uchinchisi esa alohida turga aylandi, Lusotitan.

The turdagi namunalar ning B. altitoraks hali ham eng to'liq namunadir va faqat bir nechta boshqa namunalar bu turga mansub deb hisoblanib, uni noyob siyrakli sauropodlardan biriga aylantiradi. Morrison shakllanishi. Bu yuqori deb hisoblanadi brauzer, ehtimol erdan 9 metr (30 fut) balandlikda o'simliklarni kesish yoki sug'urish. Boshqa sauropodlardan farqli o'laroq, u orqa oyoqlarda o'stirishga yaroqsiz edi. U dinozavrning misoli sifatida ishlatilgan ektotermik uning kattaligi va shunga mos keladigan ehtiyoj tufayli em-xashak, ammo so'nggi tadqiqotlar shuni ko'rsatadiki issiq qonli. Eng ikonik va dastlab ulardan biri deb hisoblanganlar orasida eng katta dinozavrlar, Braxiosaurus ichida paydo bo'ldi ommaviy madaniyat, xususan, 1993 yilgi filmda Yura parki.

Kashfiyot tarixi

Holotip namunasi

Qazish paytida holotip material, bilan orqa umurtqalari, sakrum, ilium va qovurg'alar ko'rinishida

Jins Braxiosaurus qisman asoslanadi postkranial skeletlari topildi 1900 vodiysida Kolorado daryosi yaqin Fruita, Kolorado.[2] Keyinchalik holotip deb e'lon qilingan ushbu namuna Morrison Formatsiyasining Brushy havzasi a'zosi toshlaridan kelib chiqadi va shuning uchun kech Kimmeridyan yoshi, taxminan 154 dan 153 million yilgacha.[3] Amerikalik paleontolog tomonidan kashf etilgan Elmer S. Riggz va uning ekipaji Fild Kolumbiya muzeyidan (hozir Tabiat tarixi dala muzeyi ) ning Chikago,[1] u hozirda FMNH P 25107 sifatida kataloglangan.[4]

Riggs va kompaniya Riggs va Stanton Merill Bradbury, yaqin atrofdagi tish shifokori o'rtasidagi yaxshi yozishmalar natijasida ish olib borishdi. Grand Junction. 1899 yilning bahorida Riggz g'arbiy Kolorado shtatidagi merlarga maktublar yuborib, temir yo'l boshlaridan Utahning shimoliy-sharqiy qismiga olib borishi mumkin bo'lgan yo'llarni so'radi va u erda tosh qoldiqlarini topishga umid qildi. Eosen sutemizuvchilar.[5] U ajablanib, unga havaskor kollektsioner va G'arbiy Kolorado Ilmiy akademiyasining prezidenti Bredberi tomonidan dinozavr suyaklari 1885 yildan buyon Grand Junction yaqinida to'planganligi to'g'risida xabar berilgan.[2] Riggz bu da'voga shubha bilan qaragan, ammo uning yuqori darajadagi geologiya bo'yicha kuratori Oliver Kammings Farrington boshqa muassasalardan ustun turish uchun kollektsiyaga katta sauropod skeletini qo'shishni juda xohlagan va ekspeditsiyaga besh yuz dollar sarmoya kiritishga muzey rahbariyatini ishontirgan.[6] 1900 yil 20-iyunda etib kelib, ular tashlandiq Echki Ranchiga qarorgoh qurishdi.[7] Riggzning dala yordamchisi Garold Uilyam Menke ot ustida sayohat paytida FMNH P 25107 humerusini topdi,[1] 4-iyul kuni[8] "bu hali ham eng katta narsa!" deb xitob qilish. Dastlab Riggz topilmani yomon saqlanib qolgani uchun oldi Brontosaurus namunasi va yanada istiqbolli bo'lgan 12-karerni qazishga ustuvor ahamiyat berdi Morosaurus skelet. Bunga ishonch hosil qilib, 26 iyulda u 13-kareradagi humerusga qaytib keldi, u tez orada juda katta hajmga ega bo'lib, hayron bo'lgan Riggzga u yerdagi eng katta hayvonni topganiga ishontirdi.[9]

Elmer S. Riggz ’Tayyorlovchi, H. W. Menke, tomonidan yolg'on gapirgan humerus 1900 yilda qazish paytida

Sayt, Riggs Quarry 13, keyinchalik Riggs Hill deb nomlanuvchi kichik tepalikda joylashgan; u bugun plaket bilan belgilanadi. Ko'proq Braxiosaurus Riggz tepaligida toshqotganliklar haqida xabar berilgan, ammo tepalikdagi boshqa qoldiq topilmalar buzilgan.[8][10] Namunani qazish paytida Riggz humerusni uzunligi tufayli deformatsiyalangan femur deb noto'g'ri aniqladi va bu xuddi shu skeletning teng o'lchamdagi, yaxshi saqlanib qolgan haqiqiy femur topilganda aniqlandi. 1904 yilda Riggz ta'kidlagan: "Agar u bilan bog'liq bo'lgan qovurg'alarning g'ayrioddiy kattaligi bo'lmaganida, bu namuna juda yomon saqlanib qolgan Apatosaur sifatida tashlangan bo'lar edi". Laboratoriyada qazilma materiallar tayyorlangandan keyingina suyak humerus deb tan olindi.[11] Qazish ishlari ko'plab mehmonlarni jalb qildi, bu ishni kechiktirdi va suyaklarning talon-taroj qilinishini oldini olish uchun Menkeni joyni qo'riqlashga majbur qildi. 17-avgustda oxirgi suyak gips bilan ko'ylagi bilan qoplangan.[12] So'nggi o'n kunlik qidiruv safaridan so'ng, ekspeditsiya Grand Junctionga qaytib keldi va besh kun davomida barcha qoldiqlarni temir yo'l stantsiyasiga etkazish uchun guruh va vagon yolladi; yana bir hafta ularni 5,700 kilogramm (12,500 funt) og'irlikdagi o'ttiz sakkiz qutiga yig'ish uchun sarf qildi.[13] 10 sentyabrda Riggz 15-kuni etib kelgan poezdda Chikagoga jo'nab ketdi; temir yo'l kompaniyalari yo'lovchilarga ham, yuklarga ham bepul sayohat qilishlariga imkon beradi jamoat bilan aloqa imo-ishora.[14]

Holotip skeleti o'ng humerus (yuqori qo'l suyagi), o'ng femur (son suyagi), o'ng iliyum (son suyagi), o'ng korakoid (elka suyagi), sakrum (sonning birlashtirilgan umurtqalari), oxirgi etti ko'krak (magistral) va ikkita kaudal (quyruq) umurtqalari va bir nechta qovurg'alar.[1][4][15] Riggz korakoidni tananing chap tomonidan tasvirlangan,[1][11][15] ammo restudy uni to'g'ri korakoid ekanligini ko'rsatdi.[4] Kashfiyot paytida humerusning pastki uchi, sakrumning pastki qismi, ilium va saqlanib qolgan kaudal umurtqalari havoga ta'sir qildi va shu bilan ob-havo ta'sirida qisman zarar ko'rdi. Umurtqalar dastlabki anatomik holatidan biroz ozgina siljigan; ular yuqori tomonlari pastga yo'naltirilgan holda topilgan. Shu bilan birga, qovurg'alar, humerus va korakoidlar umurtqa pog'onasining chap tomoniga siljiydi, bu suv oqimi bilan transportni ko'rsatmoqda. Buni izolyatsiya qilingan ilium yana tasdiqlaydi Diplodokus aftidan umurtqa pog'onasiga, shuningdek atrofdagi jinslarning tarkibidagi o'zgarishlarga qarab siljigan. Namunaning o'zi mayda donali loyga solingan bo'lsa, u cho'ktirish vaqtidagi kam energiyali sharoitni ko'rsatsa-da, ettinchi umurtqada uning tagidagi toshlardan tashkil topgan ancha qo'pol cho'kindi qatlami va qumtosh yanada yuqoriroq, kuchli oqimlar ostida cho'kishni bildiradi. Ushbu dalillarga asoslanib, 1904 yilda Riggz skeletning yo'qolgan old qismini suv oqimi bilan yuvib tashlagan, orqa qismi esa allaqachon cho'kindi bilan qoplangan va shu tariqa saqlanib qolgan.[11]

O'ng tarafdagi Riggz va J. B. Ebbot 1899 yilda holotip suyaklari ustida ishlaydilar; hali ham ko'ylagi son suyagi chap tomonida ko'rish mumkin

Riggz 1901 yilda yangi topilma haqida qisqacha hisobotni e'lon qildi va bu erda humerusning femurga nisbatan g'ayritabiiy uzunligini va juda katta hajmini va natijada jirafaga o'xshash nisbatlarini, shuningdek dumining kamroq rivojlanishini ta'kidladi, ammo nashr etmadi yangi dinozavr uchun nom.[15] 1903 yilda u tur turlari Brachiosaurus altithorax.[1] Riggs avlod nomini Yunoncha brakion/ rβrap "qo'l" va ma'nosini anglatadi sauros/ dσrosho "kaltakesak" ma'nosini anglatadi, chunki u qo'llar uzunligi sauropod uchun g'ayrioddiy ekanligini tushungan.[1] The o'ziga xos epitet dan noan'anaviy darajada chuqur va keng ko'krak bo'shlig'i tufayli tanlangan Lotin balandlik "chuqur" va yunoncha ko'krak qafasi/ ξrapa, "ko'krak nishoni, kuyras, korslet".[16] Lotin ko'krak qafasi yunon tilidan olingan va tananing ko'krak qafasi uchun odatiy ilmiy belgiga aylangan. Riggzning 1901 va 1903 yildagi maqolalarining sarlavhalarida bu namunaning "taniqli eng katta dinozavr" ekanligi ta'kidlangan.[1][15] Riggz o'zining 1903 yildagi nashrini a-da batafsilroq tavsif bilan kuzatib bordi monografiya 1904 yilda.[11]

Holotipni tayyorlash 1900 yil kuzida Riggz tomonidan Field Museum uchun yig'ilganidan ko'p o'tmay boshlangan. Dastlab oyoq-qo'l elementlari qayta ishlandi. 1904 yilning qishida orqa va kestirib, yomon ob-havo sharoitida bo'lgan umurtqalarni Jeyms B. Abbott va C.T. Kline.[11] Har bir suyakni tayyorlash tugagandan so'ng, u tasviriy san'at saroyining 35-zalida shisha idishda namoyish etildi. Dunyolar Kolumbiya ko'rgazmasi, Dala muzeyining birinchi joylashgan joyi. 1908 yilga qadar Field Museum muzeyining yangi o'rnatilishi paytida 35-zalda barcha suyaklar birma-bir namoyish etilgan Apatosaurus Riggz 12-karerdan topgan namunasi ochilgan edi,[17] bugun FMNH P25112 sifatida kataloglangan va a Brontosaurus namunali.[18] Tog' yo'q Braxiosaurus skeletning atigi 20% tiklanganligi sababli urinishgan. 1993 yilda holotip suyaklari qolipga solindi va quyildi va etishmayotgan suyaklar tegishli materiallar asosida mujassamlashtirildi Brachiosaurus brancai (hozir Giraffatitan ) ichida Naturkunde für muzeyi, Berlin. Ushbu plastik skelet o'rnatildi va 1994 yilda Field Museum muzeyi binosining asosiy ko'rgazma zali Stenli Field Hallning shimoliy qismida namoyish etildi. Holotipning haqiqiy suyaklari o'rnatilgan gipsning ikkala uchida ikkita katta shisha idishda namoyish etildi. Tog' 1999 yilgacha bo'lgan, u B konkursiga ko'chirilgan United Airlines "Birinchi terminal O'Hare xalqaro aeroporti muzeyning yangi sotib olinishi uchun joy ajratish Tiranozavr skelet "Sue ".[19] Shu bilan birga, Field Museum muzey tashqarisida NW terastasida namoyish etilgan skeletning ikkinchi tashqi gipsini (tashqi foydalanish uchun mo'ljallangan) o'rnatdi.[20]Boshqa bir tashqi aktyorlar jo'natildi Disney hayvonot dunyosi "DinoLand, AQSh" uchun shlyuz belgisi sifatida xizmat qilish. "Oldengate ko'prigi" deb nomlanuvchi, Boneyard o'yin maydonchasi ostidagi qazib olinadigan karerning ikki qismini birlashtirgan.[21]

Tayinlangan material

Kompozit skelet diagrammasi, turli xil namunalarni ko'rsatadigan rang

Keyingi kashfiyotlari Braxiosaurus Shimoliy Amerikadagi materiallar juda kam uchraydi va bir nechta suyaklardan iborat. Bugungi kunga kelib, materialni faqat holotip materiali bilan qoplashda jinsga bir xil tarzda kiritish mumkin va elementlarning har qanday yo'naltirilishi bosh suyagi, bo'yin, orqa dorsal mintaqani hosil qiladi yoki distal a'zolar yoki oyoqlar taxminiy bo'lib qoladi. Shunga qaramay, material Kolorado shtatidan tasvirlangan,[4][22][23][24] Oklaxoma,[4][25] Yuta,[4][22] va Vayoming,[4][26] va tavsiflanmagan materiallar bir nechta boshqa saytlarda aytib o'tilgan.[4][3]

1883 yilda fermer Marshal Parker Felch, a fotoalbomlarni yig'uvchi amerikalik paleontolog uchun Otniel Charlz Marsh, yaqinidagi Felch karer 1-da sauropod bosh suyagi topilganligi haqida xabar berdi Garden Park, Kolorado. Bosh suyagi sarg'ish oq qumtoshdan, uzunligi 1 metr (3 fut) yaqinida topilgan 3 12 in) bachadon bo'yni umurtqasi, uni to'plashga urinish paytida vayron bo'lgan. Boshsuyagi 1986 YPM sifatida kataloglangan va Marshga yuborilgan Peabody tabiiy tarix muzeyi, uni 1891 yil skeletni tiklashga kiritgan Brontosaurus (ehtimol, Felch uni o'sha dinozavrga tegishli ekanligini aniqlagani uchun). Felch karerining bosh suyagi kranium, maxillae, o'ng postorbital, chap maxilla qismi, chapdan iborat skuamozal, tish shifokorlari va mumkin bo'lgan qisman pterygoid. Suyaklar taxminan Marsh uchun tayyorlangan edi, bu esa biroz zarar etkazdi. Felch tomonidan to'plangan namunalarning aksariyati yuborilgan Milliy tabiiy tarix muzeyi Marshning o'limidan keyin 1899 yilda, shu jumladan bosh suyagi, keyinchalik USNM 5730 sifatida kataloglangan.[27][28][29]

O. C. Marsh Eskirgan 1891 yil skelet rekonstruksiyasi Brontosaurus, Felch kareriga asoslangan noto'g'ri bosh suyagi bilan Braxiosaurus

1975 yilda amerikalik paleontologlar Jek Makintosh va Devid Berman Marshning bosh suyagini noto'g'ri tayinlaganligi yoki yo'qligi haqidagi tarixiy masalani o'rganib chiqishdi. Brontosaurus (o'sha paytda a kichik sinonim ning Apatosaurus) va Felch karerining bosh suyagini "general" deb topdi Kamarasaurus turi ", uning yonidan topilgan umurtqa pog'onasi tegishli ekanligini taxmin qilish bilan birga Braxiosaurus. Ularning fikriga ko'ra, agar Marsh o'zboshimchalik bilan Felch karerining bosh suyagini va boshqasini tayinlamagan bo'lsa Kamarasaurus- bosh suyagiga o'xshash Brontosaurus, ilgari haqiqiy bosh suyagi tan olingan bo'lar edi Brontosaurus va Apatosaurus ga o'xshashroq edi Diplodokus.[29] Keyinchalik Makintosh Felch karerasi bosh suyagini taxminiy ravishda tegishli deb tan oldi Braxiosaurusva uni Amerika paleontologlari e'tiboriga havola etdi Kennet Carpenter va Virjiniya Tidvell, ularni ta'riflashga undashganda. Bosh suyagini olib kelishdi Denver tabiiy tarix muzeyi, bu erda ular uni yana tayyorladilar va bosh suyaklari bilan alohida suyaklar gipslari asosida qayta tikladilar Giraffatitan va Kamarasaurus yo'qolgan suyaklar uchun shablon sifatida harakat qilish.[27][30][4]

1998 yilda Carpenter va Tidwell Felch karerining bosh suyagini tasvirlab berishdi va uni rasmiy ravishda tayinladilar Braxiosaurus sp. (noaniq turlar bo'yicha), chunki uning turga mansubligini aniqlash mumkin emas B. altitoraks o'zi (chunki ikkita namuna o'rtasida bir-birining ustiga chiqadigan material yo'q). Ular bosh suyagining topshirig'iga asoslanishdi Braxiosaurus bilan o'xshashligi bo'yicha B. brancai, keyinchalik sifatida tanilgan Giraffatitan.[27][30] 2019 yilda amerikalik paleontologlar Maykl D. D'emik va Metyu T. Karrano Felch karerining bosh suyagini yaxshilab tayyorlab, qayta tayyorlashdan so'ng uni qayta tekshirib ko'rishdi. KT-skanerdan o'tkazildi (suyaklarning oldingi holatlarini ko'rsatuvchi tarixiy rasmlar bilan maslahatlashayotganda) va shunday xulosaga keldi: a to'rtburchak suyagi Carpenter va Tidwell tomonidan bosh suyagining bir qismi deb hisoblangan tish tishi unga tegishli emas edi. Kvadrat skuamoz bilan ifodalash uchun juda katta, boshqa suyaklardan farqli ravishda saqlanib qoladi va bir necha metr narida topilgan. Tish jag'ning tishlariga o'xshamaydi (KT ma'lumotlari aniqlanganidek), kattaroq va shuning uchun Kamarasaurus sp. (ushbu jinsga tegishli bo'lgan boshqa tishlar karerdan ma'lum). Shuningdek, ular bosh suyagini tayinlashni eng sodda deb hisoblashdi B. altitoraks Morrison Formation-da boshqa brakiyosurid taksonlari haqida hech qanday ma'lumot yo'qligi sababli (va bu va boshqa mumkin bo'lgan elementlarni filogenetik tahlil holatini o'zgartirmadi B. altitoraks).[31]

Skapulakorakoid BYU 9462 imkon qadar ko'rilgan Braxiosaurus suyak; u dastlab tayinlangan edi Ultrasauros (endi a kichik sinonim ning Supersaurus), Qadimgi hayot muzeyi

Korakoidli elka pichog'i Quruq Mesa karer, Kolorado, bu markazdagi namunalardan biridir Supersaurus /Ultrasauros 1980 va 1990-yillarning soni. 1985 yilda, Jeyms A. Jensen tasvirlangan disartikulyatsiyalangan sauropod qoldiqlaridan juda katta bo'lganlarga tegishli taksonlar jumladan, yangi avlod Supersaurus va Ultrasaurus,[32] ikkinchisi qayta nomlandi Ultrasauros ko'p o'tmay, chunki boshqa sauropod ismni allaqachon olgan edi.[33] Keyinchalik tadqiqotlar shuni ko'rsatdiki, "ultrasavr" materiali asosan tegishli bo'lgan Supersaurus, ammo elkama pichog'i yo'q edi. Ning holotipi bo'lgani uchun Ultrasauros, dorsal vertebra, aslida olingan namunalardan biri edi Supersaurus, ism Ultrasauros ning sinonimidir Supersaurus. Yelka pichog'i, namuna BYU 9462 (ilgari BYU 5001), 1996 yilda a Braxiosaurus sp. (noaniq turlar bo'yicha) Brayan Kurtis va uning hamkasblari tomonidan; 2009 yilda Maykl P. Teylor unga murojaat qilish mumkin emas degan xulosaga keldi B. altitoraks.[4][23] Quruq Mesaning "ultrasavri" o'ylanganchalik katta bo'lmagan; yelkaning korakoid suyagining o'lchamlari hayvon Riggzning asl nusxasidan kichikroq ekanligini ko'rsatadi Braxiosaurus.[4]

Potter Creek-dan oldingi suyak (humerus), USNM 21903

1987 yilda Jensen tomonidan bir nechta qo'shimcha namunalar qisqacha tavsiflangan.[22] Ushbu topilmalardan biri, humerus USNM 21903, taxminan, topilgan. 1943 yil Vivian va Deniel Jons uran izlovchilari tomonidan Kolorado g'arbiy qismidagi Potter-Krik karerida va xayr-ehson qilishdi. Smitson instituti. Dastlab, bu humerus to'planmagan, kam saqlanib qolgan qisman skeletning bir qismi edi.[22][4][34] 2009 yilda Teylorga ko'ra, bunga aniq murojaat qilish mumkin emas Braxiosaurus 2.13 metr (6 fut) katta hajmiga qaramay 11 34 ichida). Jensenning o'zi 1971 va 1975 yillarda Potter-Krik maydonida ishlagan, BYU 4744 ning disartikulyar namunasini qazib olgan, uning tarkibida o'rta dorsal vertebra, to'liq bo'lmagan chap iliyum, chap radius va o'ng metakarpal mavjud. 2009 yilda Teylorning so'zlariga ko'ra, ushbu namunaga ishonchli murojaat qilish mumkin B. altitoraks, uning namunasi bilan bir-biriga mos keladigan darajada. Jensen, shuningdek, yaqinda topilgan namunani eslatib o'tdi Jensen, Yuta 2,75 metr (9 fut) qovurg'ani o'z ichiga oladi 14 uzunlikda, bo'yin old umurtqasi, skapula qismi va korakoid, garchi u ta'rif bermagan bo'lsa.[22][4] 2001 yilda Kurtis va Stadtman Quruq Mesa kareridan ikkita bo'g'inli dorsal umurtqani (BYU 13023 namunasi) tayinladilar. Braxiosaurus.[24] Teylor, 2009 yilda, bu vertebralarnikiga qaraganda ancha qisqaroq ekanligini ta'kidlagan B. altitoraks holotip, garchi boshqacha bo'lsa ham.[4]

2012 yilda Xose Karballido va uning hamkasblari uzunligi taxminan 2 metr (6 fut 7 dyuym) bo'lgan kichik o'spirinning postkranial deyarli to'liq skeletlari haqida xabar berishdi. "Toni" laqabli va SMA 0009 deb kataloglangan ushbu namuna Morrison Formation of the Bighorn havzasi Vayoming shtatining shimoliy qismida. Dastlab a ga tegishli deb o'ylagan bo'lsa ham diplodotsid, keyinchalik brakiosaurid sifatida qayta talqin qilingan, ehtimol unga tegishli B. altitoraks.[35] 2018 yilda hozirgacha topilgan eng katta sauropod oyoqlari haqida xabar berildi Qora tepaliklar ning Weston County, Vayoming. Femur suyagi saqlanib qolmagan, ammo taqqoslashlarga qaraganda bu uningnikidan 2% ko'proq bo'lgan B. altitoraks holotip. Ehtimol, tegishli bo'lishi mumkin Braxiosaurus, mualliflar ehtiyotkorlik bilan uni noaniq brakiosaurid deb tasnifladilar.[36]

Ilgari tayinlangan turlar

Brachiosaurus brancai va Brachiosaurus fraasi

Skeletlari topildi Giraffatitan, avval B. brancai, Tabiiy tarix muzeyi, Berlin

1909-1912 yillarda keng ko'lamli paleontologik ekspeditsiyalar Germaniya Sharqiy Afrika ning katta miqdorini qazib oldi brakiosaurid dan material Tendaguru shakllanishi. 1914 yilda nemis paleontologi Verner Yanensch ushbu qoldiqlar orasidagi farqlar va umumiyliklarni sanab o'tdi B. altitoraks, xulosa qilib, ularni naslga murojaat qilish mumkin Braxiosaurus. Ushbu materialdan Janensch ikkita turni nomladi: Brachiosaurus brancai kattaroq va to'liq takson uchun va Brachiosaurus fraasi kichikroq va kam ma'lum bo'lgan turlar uchun.[37] 1929 yilda yana uchta nashrda,[38] 1950[39] va 1961 yil,[40] Janensch ushbu turlarni batafsilroq taqqoslab, ular orasida o'n uchta umumiy belgilarni sanab o'tdi Brachiosaurus brancai (u hozir qo'shishni o'ylagan B. fraasi) va B. altitoraks.[4] Teylor, 2009 yilda ushbu belgilarning atigi to'rttasini haqiqiy deb hisoblagan; oltitasi Brachiosauridae'dan ko'ra ko'proq inklyuziv guruhlarga tegishli, qolganlarini baholash qiyin yoki ularga mos bo'lmagan materiallarga murojaat qilish Braxiosaurus.[4]

Ko'p materiallar haqida gap bor edi B. brancai Berlindagi fur Naturkunde muzeyi kollektsiyalarida, ba'zilari esa yo'q qilingan Ikkinchi jahon urushi. Boshqa materiallar Germaniya bo'ylab boshqa muassasalarga o'tkazildi, ularning ba'zilari ham yo'q qilindi. Tomonidan qo'shimcha materiallar to'plangan Britaniya tabiiy tarixi muzeyi Tendaguru ekspeditsiyasi, shu jumladan F.W.H. tomonidan to'plangan deyarli to'liq skelet (BMNH R5937). Migeod 1930 yilda. Ushbu namunaga endi ishoniladi yangi turni anglatadi, tavsifini kutmoqda.[41][4]

Janensch o'zining tavsifiga asoslanib B. brancai Tendagurudan "Skelet S" (skelet S) da,[37] ammo keyinchalik u ikkita qisman shaxsni o'z ichiga olganligini angladi: S I va S II.[38] U dastlab ularni a deb belgilamadi sintip seriyali, ammo 1935 yilda S I (hozirgi MB.R.2180) ni yaratdi lektotip. 2009 yilda Teylor ushbu harakatni bilmagan holda, ma'ruza turi sifatida kattaroq va to'liqroq S II (MB.R.2181) ni taklif qildi.[4] Bunga boshqa suyaklar qatori bir nechta orqa umurtqalar, chap skapula, ikkala korakoid, ikkalasi ham kiradi sternals (ko'krak suyaklari), ikkala humeri, ikkala ulna va radius (pastki qo'l suyaklari), o'ng qo'l, qisman chap qo'l, ikkalasi pablar (son suyagi) va o'ng femur, tibia va fibula (suyak suyaklari). Keyinchalik 2011 yilda Teylor Yanensch 1935 yilda S I skeletini lektotip sifatida tayinlaganini tushundi.[42][43]

Ikkala suyaklarni o'z ichiga olgan diagramma Braxiosaurus va Giraffatitan, tomonidan Uilyam Diller Metyu, 1915

1988 yilda, Gregori S. Pol skeletining yangi rekonstruktsiyasini nashr etdi B. brancai, u va orasidagi mutanosiblikdagi farqlarni ta'kidlash B. altitoraks. Ular orasida magistral umurtqalarining turlicha bo'lishini ajratib ko'rsatish kerak edi: ular Afrika materiallarida uzunligi bo'yicha bir xil, ammo har xil B. altitoraks. Pavlus ikkala turning ham oyoq-qo'llari va kamar elementlari juda o'xshashligiga ishongan va shuning uchun ularni jinsda emas, balki faqat subgenus darajasi, kabi Braxiosaurus (Brachiosaurus) altitoraks va Brachiosaurus (Giraffatitan) brancai.[44] Giraffatitan 1991 yilda Jorj Olshevskiy tomonidan umurtqaning o'zgarishini nazarda tutgan holda to'liq nasl darajasiga ko'tarilgan.[33] 1991 yildan 2009 yilgacha ism Giraffatitan boshqa tadqiqotchilar tomonidan deyarli butunlay e'tiborsiz qoldirilgan.[4]

Teylor tomonidan 2009 yilda barcha materiallar, shu jumladan oyoq-qo'llar va kamar suyaklari bo'yicha batafsil tadqiqotlar o'rtasida bir-biridan farqlar borligi aniqlandi. B. altitoraks va ikkala turdan ma'lum bo'lgan barcha elementlarda Tendaguru moddasi. Teylor yigirma oltita aniq osteologik (suyakka asoslangan) belgilarni topdi, bu ularning orasidagi farq katta Diplodokus va Barosaurus va shuning uchun afrikalik materiallar haqiqatan ham o'z turiga joylashtirilishi kerak, deb ta'kidladilar.Giraffatitan- kabi Giraffatitan brancai.[4] Ikki nasl o'rtasidagi muhim qarama-qarshilik ularning umumiy tana shakli, bilan Braxiosaurus 23% uzunroq umurtqa pog'onali seriyali va 20 dan 25% gacha, shuningdek uzunroq dumga ega.[4] Bo'linishni 2010 yilda Daniel Chure rad etdi,[45] ammo 2012 yildan boshlab ko'plab tadqiqotlar ushbu nomni tan olishdi Giraffatitan.[46]

Brachiosaurus atalaiensis

O'rta kaudal umurtqalari Lusotitan, avval "B." atalaiensis

1947 yilda Portugaliyadagi Atalayada brakiyosurid qoldiqlari qatlamlardan topilgan Titoniy. Albert-Feliks de Lapparent va Georges Zbyszewski ularni tur deb atashdi Brachiosaurus atalaiensis 1957 yilda.[47] Uning yo'nalishi Braxiosaurus ning 2004 yilgi nashrida shubha qilingan Dinozavrlar Pol Upchurch, Barret va Piter Dodson uni hali noma'lum brachiosaurid turiga kiritgan.[48] 2004 yilgi kitob nashr etilishidan sal oldin bu tur o'z turiga joylashtirilgan edi Lusotitan tomonidan Migel Telles Antunes va Oktavi Mateus 2003 yilda.[49] De Lapparent va Zbiszevski bir qator qoldiqlarni tasvirlab berishgan, ammo a belgisini ko'rsatmaganlar turdagi namunalar. Antunes va Mateus qisman postkranial skeletni tanladilar (MIGM 4978, 4798, 4801-4810, 4938, 4944, 4950, 4952, 4958, 4964-4966, 4981-4982, 4985, 8807, 8793-87934) lektotip sifatida; ushbu namunada yigirma sakkizta umurtqalar, chevronlar, qovurg'alar, mumkin bo'lgan elkama pichog'i, humeri, bilak suyaklari, qisman chap tos suyagi, pastki oyoq suyaklari va o'ng to'piqning bir qismi. Pastki nerv umurtqalari, humerusning taniqli deltopektoral tepasi (qo'lning yuqori suyagidagi mushak biriktiruvchi joy), cho'zilgan humerus (juda uzun va ingichka) va iliyumning uzun o'qi yuqoriga qarab burilganligini ko'rsatadi. Lusotitan brakiosaurid,[49] buni ba'zi keyingi tadqiqotlar, masalan, 2013 yilda tahlil qilish bilan tasdiqladi.[46]

Brachiosaurus nougaredi

Ning saqlanib qolgan qismlari ko'rsatilgan diagramma "B." nougaredi sakrum ko'k

1958 yilda frantsuz neft geologi F.Nuugerde sharqda parchalangan brakiosaurid qoldiqlarini topgani haqida xabar berdi Jazoir, ichida Sahara cho'llari.[50] Shular asosida Albert-Feliks de Lapparent turlarni tavsiflab, ularga nom bergan Brachiosaurus nougaredi 1960 yilda. U kashfiyot joyini Kech yura Taouratine seriyasi. U toshlarni qisman bu yoshga, chunki taxmin qilingan mavjudligi sababli tayinlagan Braxiosaurus.[51] So'nggi sharh uni "Kontinental interkaler ga tegishli deb hisoblanadi Albian kech yoshi Erta bo'r, sezilarli darajada yoshroq.[48]

Parijga ko'chirilgan material sakrumdan iborat bo'lib, cho'l yuzasida buzilib ketgan va chap metakarpallarning bir qismi va falanjlar. Kashfiyot joyidan topilgan, ammo to'planmagan, chap bilakning qisman suyaklari, bilak suyaklari, o'ng suyak suyagi va undan olingan bo'laklar. metatarsallar.[51]

"B." nougaredi 2004 yilda aniq, noma'lum brachiosaurid turini ifodalaydi,[48] ammo Filipp D. Mannion va uning hamkasblari tomonidan 2013 yilda o'tkazilgan tahlil natijalariga ko'ra qoldiqlar bir nechta turlarga tegishli bo'lishi mumkin, chunki ular bir-biridan uzoqroq joyda to'plangan.[46] Metakarpalar ba'zi noaniqlarga tegishli degan xulosaga kelishdi titanosauriform. Sakrum 2013 yilda yo'qolganligi haqida xabar berilgan edi. U tahlil qilinmagan va vaqtincha noaniq sauropod vakili deb topilgan, shu vaqtgacha uni kollektsiyalar to'plamiga ko'chirish mumkin edi. Naturelle musiqiy milliy muzeyi. Besh sakraldan atigi to'rttasi umurtqalar saqlanib qolgan. Umumiy asl uzunligi 1960 yilda 1,9 metr (4 fut 3 dyuym) ga teng, 0,91 metr (3 fut 0 dyuym) ga nisbatan B. altitoraks.[51] Bu uni boshqa har qanday sauropod sakrumidan kattaroq qiladi, bundan tashqari Argentinosaurus va Apatosaurus.[46]

Tavsif

Odamga nisbatan o'lcham

Hajmi

Eng taxminlar Brachiosaurus altithorax"s hajmi bog'liq bo'lgan narsalarga asoslangan brakiosaurid Giraffatitan (ilgari nomi bilan tanilgan B. brancai) ga qaraganda ancha to'liq materiallardan ma'lum Braxiosaurus. Ikki tur - bu eng katta brakiosauridlar, ularning nisbatan keng qoldiqlari topilgan. Shimoliy Amerika uchun yana bir noaniqlik elementi mavjud Braxiosaurus chunki turi (va eng to'liq) namuna a ni ifodalaydi kichik yoshdagi, qo'llanilmagan ko'rsatilgandek tikuv o'rtasida korakoid, suyagi elkama-kamar ning bir qismini tashkil etadi elka qo'shilishi, va skapula (elka pichog'i).[4] Bir necha yillar davomida B. altitoraks 35,0 metr (38,6 qisqa tonna) tonnaga baholandi,[44] 28,3 metrik tonna (31,2 qisqa tonna),[52] 43,9 metr (48,4 qisqa tonna),[26] 28,7 metr (31,6 qisqa tonna),[4] 56,3 metr (62,1 qisqa tonna),[53] va 58 metrik tonna (64 qisqa tonna).[54] Uzunligi Braxiosaurus 20-21 metrga baholangan (66-69 fut)[44] va 18 metr (59 fut),[55][52] va uning balandligi 9,4 metr (30 34 ft)[55] va 12-13 metr (39-43 fut).[44][56]

Oyoq suyaklari eng to'liq bo'lsa-da Giraffatitan skelet (MB.R.2181) hajmi jihatidan juda o'xshash edi Braxiosaurus turi namunasi, avvalgisiga qaraganda biroz engilroq edi Braxiosaurus uning mutanosib farqlarini hisobga olgan holda namuna. Ikkala avlod uchun taxminlarni o'z ichiga olgan tadqiqotlarda, Giraffatitan 31,5 metr (34,7 qisqa tonna),[44] 23,3 metr (25,7 qisqa tonna),[4] va 34,0 metrik tonna (37,5 qisqa tonna).[53][42] Asosiy kabi Braxiosaurus namuna, Giraffatitan MB.R.2181 namunasi, ehtimol, jinsning maksimal hajmini aks ettirmaydi fibula (namuna HM XV2) MB 2181 yilga nisbatan 13% uzunroq.[4]

Umumiy qurilish

Hayotni tiklash gipotetik nazalni ko'rsatish bezak

Barcha sauropod dinozavrlari singari, Braxiosaurus to'rt boshli kichkina bosh suyagi, uzun bo'yin va katta magistral bilan baland bo'yliellipsoid ko'ndalang kesim, uzun, mushak dumi va ingichka, ustunli oyoq-qo'llar.[48] Katta havo yostig'i o'pka tizimiga ulangan bo'yin va magistral mavjud edi, bostirib kirdi umurtqalar va qovurg'alar suyak rezorbsiyasi, tananing umumiy zichligini sezilarli darajada kamaytiradi.[57][58] Bo'yin saqlanib qolmaydi holotip namunasi, ammo sauropod me'yorlari bo'yicha ham juda yaqin bo'lgan Giraffatitan, o'n uch cho'zilgan iborat bachadon bo'yni (bo'yin) vertebra.[59] Bo'yin engil S-egri chiziq bilan ushlab turilgan, pastki va yuqori qismlari egilib, to'g'ri o'rta qismi.[60] Braxiosaurus ehtimol baham ko'rgan Giraffatitan juda cho'zilgan bo'yin qovurg'alari, bo'yinning pastki qismida yugurib, oldingi bir nechta umurtqalarni qoplagan. Ushbu suyak tayoqchalari uchlarida bo'yin muskullariga biriktirilgan bo'lib, bu mushaklarning ishlashiga imkon yaratgan distal bo'yinning ayrim qismlari magistralga yaqinroq bo'lib, distal bo'yin qismlarini engillashtiradi.[60][61]

Braxiosaurus va Giraffatitan ehtimol, uchinchi va beshinchi o'rtasida kichik yelka kamari bo'lgan dorsal (orqa) vertebra, bu erda yon tomonga va yuqoriga yo'naltirilgan vertebral jarayonlar bo'yin muskullarini biriktirish uchun qo'shimcha sirtni ta'minlaydigan uzunroq edi.[62] Qovurg'a suyagi boshqa sauropodlarga nisbatan chuqur edi.[1] Garchi humerus (yuqori qo'l suyagi) va suyak suyagi (son suyagi) uzunligi bo'yicha taxminan teng edi, butun old oyoq orqa oyoqdan uzunroq bo'lar edi, chunki cho'zilgan bilakdan va metakarpus boshqa brakiyosauridlar.[4] Buning natijasida moyil magistral yelkaning son qismidan ancha balandroq va bo'yin magistraldan tik burchak ostida chiqib ketishiga olib keldi. Umumiy tuzilishi Braxiosaurus o'xshaydi a Jirafa boshqa tirik hayvonlarga qaraganda ko'proq.[44] Aksincha, boshqa sauropodlarning aksariyati orqa oyoqqa qaraganda qisqaroq old oyoqqa ega edilar; old qism ayniqsa zamondoshda qisqa diplodokoidlar.[63]

Braxiosaurus bir-biri bilan chambarchas bog'liq bo'lgan tana nisbati bilan ajralib turardi Giraffatitan. Magistral taxminan 25-30% uzunroq edi, natijada umurtqa pog'onasidan uzun umurtqa pog'onasi paydo bo'ldi. Faqat bitta to'liq kaudal (quyruq) vertebra kashf etilgan, ammo uning katta balandligi dumnikidan kattaroq ekanligini ko'rsatadi Giraffatitan. Ushbu vertebra uchun juda katta maydon mavjud edi ligament kengaytirilganligi sababli biriktirma asab orqa miya, quyruq ham uzunroq bo'lganligini ko'rsatmoqda Giraffatitan, ehtimol 20-25% gacha.[4] 1988 yilda paleontolog Gregori S.Pol bo'yinbog'ini taklif qildi Braxiosaurus undan qisqa edi Giraffatitan, ammo 2009 yilda paleontolog Mayk P. Teylor bachadon bo'yni umurtqalariga tegishli bo'lishi mumkinligini ta'kidladi Braxiosaurus bir xil nisbatlarga ega edi.[4][44] Aksincha Giraffatitan va boshqa sauropodlar, vertikal yo'naltirilgan old oyoqlari, qo'llari Braxiosaurus korakoidlarning bo'g'im yuzalarining yon tomon yo'nalishi ko'rsatilgandek, yelka bo'g'imlarida biroz taranglashgan ko'rinadi.[4] Humus suyaklariga qaraganda kamroq ingichka edi Giraffatitan, femur esa shunga o'xshash nisbatlarga ega edi. Bu oldingi pog'onalarni ko'rsatishi mumkin Braxiosaurus tana vaznining odatdagidan ko'proq qismini qo'llab-quvvatladi Giraffatitan.[4]

Postkranial skelet

Vertebral holotip skeletining anatomiyasi. Yuqoridan: orqa (A) va o'ng tomondan (B) ko'rinishdagi oltinchi dorsal vertebra. Pastki: orqa (C) va yon tomondan (D) ikkinchi kaudal vertebra.

Magistral yoki gavdaning umurtqa pog'onasi to'liq noma'lum bo'lsa-da, orqa tomoni Braxiosaurus ehtimol o'n ikki dumg'aza umurtqasidan iborat; bu noma'lum brakiosaurid namunasida saqlanib qolgan to'liq dumg'aza umurtqa pog'onasidan kelib chiqishi mumkin, BMNH R5937.[64] Dorsal ustunning old qismidagi umurtqalar biroz yuqoriroq, ammo orqa qismnikiga qaraganda ancha uzunroq edi. Bu farqli o'laroq Giraffatitan, bu erda oldingi qismdagi umurtqalar ancha balandroq, ammo biroz uzunroq edi. Vertebra (vertebra tanalari), umurtqaning pastki qismi, ko'proq uzunroq va tasavvurlar shaklida taxminan dumaloq edi, shu bilan birga Giraffatitan uzunroqdan kengroq edi. The foramina (kichik teshiklar) sentrning yon tomonlarida havo xaltachalarining kirib kelishiga imkon bergan, kattaroq Giraffatitan. Diafofizlar (katta proektsiyalar asab kamari umurtqalar) gorizontal edi, ularniki Giraffatitan yuqoriga moyil edi. Ularning oxirida bu proektsiyalar qovurg'alar bilan ifodalangan; bo'g'im yuzasi oldingi kabi aniq uchburchak emas edi Giraffatitan. Yon tomondan, yuqoriga qarab loyihalash asab tizmalari vertikal holda turar va tepada ikki baravar kengroq edi; ular Giraffatitan orqaga burildi va ularning tagida kengaymadi. Old yoki orqa tomondan ko'rilganda, asab orqa miya tepalari tomon kengaygan.[4]

Yilda Braxiosaurus, bu kengayish asta-sekin ro'y berdi, natijada belkurakka o'xshash shakl paydo bo'ldi Giraffatitan kengayish to'satdan va faqat eng yuqori qismida sodir bo'ldi. Ikkala old va orqa tomonlarida ham, orqa miya katta, uchburchak va qo'pol yuzalarga ega edi Giraffatitan yarim doira shaklida va ancha kichik bo'lgan. Turli xil vertebral jarayonlar suyakning ingichka choyshablari yoki tizmalari bilan bog'langan bo'lib, ular deyiladi laminalar. Braxiosaurus mavjud bo'lgan postspinal laminalar etishmadi Giraffatitan, asab orqa miya orqa tomonida yugurib. Nerv umurtqalaridan diapofizlarga qadar cho'zilgan spinodiapophyseal laminae, asab nayzalari va nervlar o'rtasida cho'zilgan spinopostzigapofizal laminalar bilan to'qnashdi. qo'shma jarayonlar umurtqaning orqa qismida va shuning uchun asab umurtqalarining o'rta balandligida tugaydi. Yilda Giraffatitan, ikkala laminalar birlashtirilmagan va spinodiapophyseal laminae asab orqa miya tepasiga etib borgan. Braxiosaurus dan yana ajralib turadi Giraffatitan dorsal vertebra laminalarida so'nggi jinsga xos bo'lgan uchta tafsilot etishmasligidadir.[4]

Sakrum, ilium va .ning anatomiyasi korakoid. Yuqoridan: Sakrum pastda (A) va o'ng tomonda (B). Pastki tomon: o'ng tomonda ilium yon tomonda (C) va chap korakoid yon ko'rinishda (D).

Havo xaltachalari nafaqat umurtqalarni, balki qovurg'alarni ham bosib olgan. Yilda Braxiosaurus, havo yostig'i qovurg'a vallari old tomonidagi kichik teshik orqali bostirib kirgan Giraffatitan Tuberkulyumning old va orqa tomonlarida teshiklar, suyak proektsiyasi vertebra diapofizlari bilan ifodalangan. Pol, 1988 yilda, ning qovurg'alari Braxiosaurus dan uzunroq edi Giraffatitan, bu 2009 yilda Teylor tomonidan so'roq qilingan.[4] Dorsal vertebra ustunining orqasida, sakrum beshta kosuyaklangan sakral vertebra.[11] Xuddi shunday Giraffatitan, sakrum mutanosib ravishda keng bo'lib, juda qisqa nerv umurtqalari bilan ajralib turardi. Sakral materialning yomon saqlanishi Giraffatitan ikkala nasl o'rtasidagi batafsil taqqoslashni istisno qiladi. Quyruqdan faqat ikkinchi kaudal vertebra yaxshi saqlanib qolgan.[4]

Xuddi shunday Giraffatitan, bu vertebra biroz amfikoloz (ikkala uchida konkav), yon tomonlarida teshiklari bo'lmagan va to'rtburchaklar va orqaga burilgan qisqa nerv umurtqasi bo'lgan. Ning ikkinchi kaudal vertebrasidan farqli o'laroq Giraffatitan, bu Braxiosaurus mutanosib baland bo'yli asab kamari bor edi, bu esa umurtqani 30% atrofida balandroq qildi. Markazdan farqli o'laroq, uning yon tomonlarida tushkunlik yo'q edi Giraffatitan. Old yoki orqa tomondan nerv umurtqasi uchiga qarab eng kam kengligidan taxminan uch baravar kengaygan, ammo hech qanday kengayish ko'rinmaydi Giraffatitan. Nerv o'murtalari, shuningdek, taxminan 30 ° ga orqaga burildi, bu esa ko'proq Giraffatitan (20 °). Kaudal qovurg'alar lateral ravishda proektsiyalangan va oldingi kabi orqaga burilmagan Giraffatitan. Umurtqaning orqa qismidagi artikulyar jarayonlarning bo'g'im tomonlari pastga, pastga qarab yo'naltirilgan Giraffatitan yon tomonlarga ko'proq qaragan. Artikulyar jarayonlardan tashqari, gipofen-gipantrum artikulyatsiyasi umurtqa pog'onasini yanada qattiqroq qilib, vertebra o'rtasida qo'shimcha artikulyatsiya hosil qildi; yilda Braxiosaurus, gifosfen nisbatan ancha aniqroq bo'lgan Giraffatitan.[4]

Femur (chapda) va holotipning humerusi

Korakoid yarim doira shaklida va kengroqdan balandroq bo'lgan. Dan farqlari Giraffatitan skapula bilan tikilgan tikuvni o'z ichiga olgan yon ko'rinishdagi shakli bilan bog'liq. Bundan tashqari, elka bo'g'imining bir qismini tashkil etuvchi bo'g'im yuzasi qalinroq va yon tomonga yo'naltirilgan Giraffatitan and other sauropods, possibly indicating a more sprawled forelimb. The humerus, as preserved, measures 204 centimeters (80 12 in) in length, though part of its lower end was lost to erosion; its original length is estimated at 216 centimeters (85 in). This bone was more slender in Braxiosaurus than in most other sauropods, measuring only 28.5 centimeters (11 14 in) in width at its narrowest part. It was, however, more robust than that of Giraffatitan, being around 10% broader at the upper and lower ends. At its upper end, it featured a low bulge visible in side view, which is absent in Giraffatitan.[4]

Distinguishing features can also be found in the ilium of the pelvis. Yilda Braxiosaurus, the ischiadic peduncle, a downward projecting extension connecting to the iskiyum, reaches farther downward than in Giraffatitan. While the latter genus had a sharp notch between the ischiadic peduncle and the back portion of the ilium, this notch is more rounded in Braxiosaurus. On the upper surface of the hind part of the ilium, Braxiosaurus had a pronounced tubercle that is absent in other sauropods. Of the hindlimb, the femur was very similar to that of Giraffatitan although slightly more robust, and measured 203 centimeters (80 in) long.[1] Xuddi shunday Giraffatitan, it was strongly elliptical in cross-section, being more than twice as wide in front or back view than in side view.[4] The fourth trochanter, a prominent bulge on the back side of the femoral shaft, was more prominent and located further downward. This bulge served as anchor point for the most important locomotory muscle, the caudofemoralis, which was situated in the tail and pulled the upper thigh backward when contracted. At the lower end of the femur, the pair of kondiller did not extend backward as strongly as in Giraffatitan; the two condyles were similar in width in Braxiosaurus but unequal in Giraffatitan.[4]

Boshsuyagi

Reconstruction of the Felch Quarry Braxiosaurus bosh suyagi, Denver tabiat va fan muzeyi

As reconstructed by Carpenter and Tidwell, the assigned Felch Quarry skull was about 81 centimeters (32 in) long from the oksipital kondil at the back of the skull to the front of the premaxillae (the front bones of the upper jaw), making it the largest sauropod skull from the Morrison shakllanishi.[27] D'Emic and Carrano instead estimated the skull to have been 70 centimeters (27 12 in) long, and if proportionally similar to that of Giraffatitan, about 55 centimeters (21 12 in) tall, and 35 centimeters (14 in) wide.[31] Overall, the skull was tall as in Giraffatitan, with a snout that was long (about 36% of the skull length according to Carpenter and Tidwell) in front of the nasal bar between the nostrils – typical of brachiosaurids. The snout was somewhat blunt when seen from above (as in Giraffatitan), and since it was set at an angle relative to the rest of the skull, gave the impression of pointing downward.[27][31]

The dorsal and lateral temporal fenestrae (openings at the upper rear and sides of the skull) were large, perhaps due to the force imparted there by the massive jaw adductor musculature. The frontal bones on top of the skull were short and wide (similar to Giraffatitan), fused and connected by a suture to the parietal suyaklar, which were also fused together. The surface of the parietals between the dorsal fenestrae was wider than that of Giraffatitan, but narrower than that of Kamarasaurus. The skull differed from that of Giraffatitan in its U-shaped (instead of W-shaped) suture between frontal and nasal bones, a shape which appears more pronounced by the frontal bones extending forward over the orbitalar (ko'z teshiklari). O'xshash Giraffatitan, the neck of the occipital condyle was very long.[27][31]

Diagram of the Felch Quarry skull, with known material in white

The premaxilla appears to have been longer than that of Kamarasaurus, sloping more gradually toward the nasal bar, which created the very long snout. Braxiosaurus had a long and deep maxilla (the main bone of the upper jaw), which was thick along the margin where the alveolalar (tooth sockets) were placed, thinning upward. The tishlararo plitalar of the maxilla were thin, fused, porous, and triangular. There were triangular ozuqaviy foramina between the plates, each containing the tip of an erupting tooth. The narial fossa (depression) in front of the bony nostril was long, relatively shallow, and less developed than that of Giraffatitan. It contained a subnarial fenestra, which was much larger than those of Giraffatitan va Kamarasaurus. The dentaries (the bones of the lower jaws that contained the teeth) were robust, though less than in Kamarasaurus. The upper margin of the dentary was arched in profile, but not as much as in Kamarasaurus. The interdental plates of the dentary were somewhat oval, with diamond shaped openings between them. The dentary had a Meckelian yiv that was open until below the ninth alveolus, continuing thereafter as a shallow trough.[27][31]

Each maxilla had space for about 14 or 15 teeth, whereas Giraffatitan had 11 and Kamarasaurus 8 to 10. The maxillae contained almashtirish tishlari that had rugose emal, o'xshash Kamarasaurus, but lacked the small denticles (serrations) along the edges. Since the maxilla was wider than that of Kamarasaurus, Braxiosaurus would have had larger teeth. The replacement teeth in the premaxilla had crinkled enamel, and the most complete of these teeth did not have denticles. It was somewhat spatulate (spoon-shaped), and had a longitudinal ridge. Each dentary had space for about 14 teeth. The maxillary tooth rows of Braxiosaurus va Giraffatitan ended well in front of the antorbital fenestra (the opening in front of the orbit), whereas they ended just in front of and below the fenestra in Kamarasaurus va Shunosaurus.[27][31]

Tasnifi

Replica skeleton outside the FMNH

Riggs, in his preliminary 1903 description of the not yet fully prepared holotype specimen, considered Braxiosaurus to be an obvious member of the Sauropoda. To determine the validity of the genus, he compared it to the previously named genera Kamarasaurus, Apatosaurus, Atlantosaurus va Amfikoelialar, whose validity he questioned given the lack of overlapping fossil material. Because of the uncertain relationships of these genera, little could be said about the relationships of Braxiosaurus o'zi.[1] In 1904, Riggs described the holotype material of Braxiosaurus in more detail, especially the vertebrae. He admitted that he originally had assumed a close affinity with Kamarasaurus, but now decided that Braxiosaurus bilan chambarchas bog'liq bo'lgan Haplocanthosaurus. Both genera shared a single line of neural spines on the back and had wide hips. Riggs considered the differences from other taxa significant enough to name a separate family, Brachiosauridae, of which Braxiosaurus bo'ladi namesake genus. According to Riggs, Haplocanthosaurus was the more primitive genus of the family while Braxiosaurus was a specialized form.[11]

Ta'riflashda Brachiosaurus brancai va B. fraasi in 1914, Janensch observed that the unique elongation of the humerus was shared by all three Braxiosaurus species as well as the British Pelorosaurus. He also noted this feature in Cetiosaurus, where it was not as strongly pronounced as in Braxiosaurus va Pelorosaurus.[37] Janensch concluded that the four genera must have been closely related to each other, and in 1929 assigned them to a subfamily Brachiosaurinae within the family Bothrosauropodidae.[38]

During the twentieth century, several sauropods were assigned to Brachiosauridae, including Astrodon, Bothriospondylus, Pelorosaurus, Pleurocoelus va Ultrasauros.[65] These assignments were often based on broad similarities rather than unambiguous sinapomorfiyalar, shared new traits, and most of these genera are currently regarded as shubhali.[66][48] In 1969, in a study by R.F. Kingham, B. altitoraks, "B." brancai and "B." atalaiensis, along with many species now assigned to other genera, were placed in the genus Astrodon, yaratish Astrodon altithorax.[67] Kingham's views of brachiosaurid taxonomy have not been accepted by many other authors.[68] Since the 1990s, computer-based kladistik analyses allow for postulating detailed hypotheses on the relationships between species, by calculating those daraxtlar that require the fewest evolutionary changes and thus are the most likely to be correct. Such cladistic analyses have cast doubt on the validity of the Brachiosauridae. In 1993, Leonardo Salgado suggested that they were an unnatural group into which all kinds of unrelated sauropods had been combined.[69] In 1997, he published an analysis in which species traditionally considered brachiosaurids were subsequent offshoots of the stem of a larger grouping, the Titanosauriformes, and not a separate branch of their own. This study also pointed out that B. altitoraks va B. brancai did not have any synapomorphies, so that there was no evidence to assume they were particularly closely related.[70]

Fifth dorsal vertebra in front of the pelvis of the holotype, compared to the same region of a human vertebral column

Many cladistic analyses have since suggested that at least some genera can be assigned to the Brachiosauridae, and that this group is a basal branch within the Titanosauriformes.[71] The exact status of each potential brachiosaurid varies from study to study. For example, a 2010 study by Chure and colleagues recognized Abidozavr as a brachiosaurid together with Braxiosaurus, which in this study included B. brancai.[45] In 2009, Taylor noted multiple anatomical differences between the two Braxiosaurus species, and consequently moved B. brancai into its own genus, Giraffatitan. In contrast to earlier studies, Taylor treated both genera as distinct units in a cladistic analysis, finding them to be opa-singillar guruhlari. Another 2010 analysis focusing on possible Asian brachiosaurid material found a clade including Abidozavr, Braxiosaurus, Sidarozavr, Giraffatitanva Paluxysaurus, lekin emas Qiaowanlong, the putative Asian brachiosaurid.[71] Several subsequent analyses have found Braxiosaurus va Giraffatitan not to be sister groups, but instead located at different positions on the evolutionary tree. A 2012 study by D'Emic placed Giraffatitan in a more basal position, in an earlier branch, than Braxiosaurus,[68] while a 2013 study by Philip Mannion and colleagues had it the other way around.[46]

The kladogramma of the Brachiosauridae below follows that published by Michael D. D'Emic in 2012:[68]

Brachiosauridae  

Evropasaurus

Giraffatitan

Braxiosaurus

Abidozavr

Sidarozavr

Venenozavr

Cladistic analyses also allow scientists to determine which new traits the members of a group have in common, their synapomorphies. According to the 2009 study by Taylor, B. altitoraks shares with other brachiosaurids the classic trait of having an upper arm bone that is at least nearly as long as the femur (ratio of humerus length to femur length of at least 0.9). Another shared character is the very flattened femur shaft, its transverse width being at least 1.85 times the width measured from front to rear.[4]

Paleobiologiya

Hayotni tiklash

Odatlar

It was believed throughout the nineteenth and early twentieth centuries that sauropods like Braxiosaurus were too massive to support their own weight on dry land, and instead lived partly submerged in water.[72] Riggs, affirming observations by Jon Bell Xetcher, was the first to defend in length that most sauropods were fully terrestrial animals in his 1904 account on Braxiosaurus, pointing out that their hollow vertebrae have no analogue in living aquatic or semiaquatic animals, and their long limbs and compact feet indicate specialization for terrestrial locomotion. Braxiosaurus would have been better adapted than other sauropods to a fully terrestrial lifestyle through its slender limbs, high chest, wide hips, high ilia and short tail. In its dorsal vertebrae the zygapophyses were very reduced while the hyposphene-hypanthrum complex was extremely developed, resulting in a stiff torso incapable of bending sideways. The body was only fit for quadrupedal movement on land.[11] Though Riggs' ideas were gradually forgotten during the first half of the twentieth century, the notion of sauropods as terrestrial animals has gained support since the 1950s, and is now universally accepted among paleontologists.[73][72] In 1990 the paleontologist Stephen Czerkas stated that Braxiosaurus could have entered water occasionally to cool off (thermoregulate ).[74]

Neck posture

Assigned neck vertebra BYU 12866, BYU Paleontologiya muzeyi

Ongoing debate revolves around the neck posture of brachiosaurids, with estimates ranging from near-vertical to horizontal orientations.[75] The idea of near-vertical postures in sauropods in general was popular until 1999, when Stevens and Parrish argued that the sauropod neck was not flexible enough to be held in an upright, S-curved pose, and instead was held horizontally.[76][62] Reflecting this research, various newspapers ran stories criticizing the Field Museum Braxiosaurus mount for having an upward curving neck. Museum paleontologists Olivier Rieppel and Christopher Brochu defended the posture in 1999, noting the long forelimbs and upward sloping backbone. They also stated that the most developed neural spines for muscle attachment being positioned in the region of the shoulder girdle would have permitted the neck to be raised in a giraffe-like posture. Furthermore, such a pose would have required less energy than lowering its neck, and the inter-vertebral discs would not have been able to counter the pressure caused by a lowered head for extended periods of time (though lowering its neck to drink must have been possible).[77] Some recent studies also advocated a more upward directed neck. Christian and Dzemski (2007) estimated that the middle part of the neck in Giraffatitan was inclined by 60–70 degrees; a horizontal posture could be maintained only for short periods of time.[60]

With their heads held high above the heart, brachiosaurids would have had stressed cardiovascular systems. It is estimated that the heart of Braxiosaurus would have to pump double the blood pressure of a giraffe to reach the brain, and possibly weighed 400 kg (880 lb).[78] The distance between head and heart would have been reduced by the S-curvature of the neck by more than 2 meters (6 12 ft) in comparison to a totally vertical posture. The neck may also have been lowered during locomotion by 20 degrees.[60] In studying the inner ear of Giraffatitan, Gunga & Kirsch (2001) concluded that brachiosaurids would have moved their necks in lateral directions more often than in dorsal-ventral directions while feeding.[60][79]

Feeding and diet

Replica skeleton showing the neck pointing upward, at O'Hare xalqaro aeroporti (formerly housed in the Field Museum)

Braxiosaurus is thought to have been a high brauzer, feeding on foliage well above the ground. Even if it did not hold its neck near vertical, and instead had a less inclined neck, its head height may still have been over 9 meters (30 ft) above the ground.[26][55] It probably fed mostly on foliage above 5 meters (16 ft). This does not preclude the possibility that it also fed lower at times, between 3 to 5 meters (9.8 to 16.4 ft) up.[55] Its diet likely consisted of ginkgos, conifers, tree ferns, and large cycads, with intake estimated at 200 to 400 kilograms (440 to 880 lb) of plant matter daily in a 2007 study.[55] Brachiosaurid feeding involved simple up-and-down jaw motion.[80] As in other sauropods, animals would have swallowed plant matter without further oral processing, and relied on orqa ichak fermentatsiyasi for food processing.[75] As the teeth were not spoon-shaped as with earlier sauropods but of the compressed cone-chisel type, a precision-shear bite was employed.[81] Such teeth are optimized for non-selective nipping,[82] and the relatively broad jaws could crop large amounts of plant material.[81] Even if a Braxiosaurus of forty tonnes would have needed half a tonne of fodder, its dietary needs could have been met by a normal cropping action of the head. If it fed sixteen hours per day, biting off between a tenth and two-thirds of a kilogram, taking between one and six bites per minute, its daily food intake would have equaled roughly 1.5% of its body mass, comparable to the requirement of a modern elephant.[83]

Sifatida Braxiosaurus u bilan bo'lishdi yashash joyi, the Morrison, with many other sauropod species, its specialization for feeding at greater heights would have been part of a system of niche partitioning, the various taxa thus avoiding direct competition with each other. A typical food tree might have resembled Sequoiadendron. The fact that such tall conifers were relatively rare in the Morrison might explain why Braxiosaurus was much less common in its ekotizim than the related Giraffatitan, which seems to have been one of the most abundant sauropods in the Tendaguru.[84] Braxiosaurus, with its shorter arms and lower shoulders, was not as well-adapted to high-browsing as Giraffatitan.[85]

Taklif qilingan Braxiosaurus could rear on its hind legs to feed, using its tail for extra ground support.[44] A detailed physical modelling-based analysis of sauropod rearing capabilities by Heinrich Mallison showed that while many sauropods could rear, the unusual body shape and limb length ratio of brachiosaurids made them exceptionally ill-suited for rearing. The forward position of its center of mass would have led to problems with stability, and required unreasonably large forces in the hips to obtain an upright posture. Braxiosaurus would also have gained only 33% more feeding height, compared to other sauropods, for which rearing may have tripled the feeding height.[86] A bipedal stance might have been adopted by Braxiosaurus in exceptional situations, like male dominance fights.[87]

The downward mobility of the neck of Braxiosaurus would have allowed it to reach open water at the level of its feet, while standing upright. Modern giraffes spread their forelimbs to lower the mouth in a relatively horizontal position, to more easily gulp down the water. Bu ehtimoldan yiroq emas Braxiosaurus could have attained a stable posture this way, forcing the animal to plunge the snout almost vertically into the surface of a lake or stream. This would have submerged its fleshy nostrils if they were located at the tip of the snout as Witmer hypothesized. Hallett and Wedel therefore in 2016 rejected his interpretation and suggested that they were in fact placed at the top of the head, above the bony nostrils, as traditionally thought. The nostrils might have evolved their retracted position to allow the animal to breathe while drinking.[88]

Nostril function

The fleshy external nostril would have been placed at the front of the nasal fossa, here demarcated by a dashed line

The bony nasal openings of neozauropodlar kabi Braxiosaurus were large and placed on the top of their skulls. Traditionally, the fleshy nostrils of sauropods were thought to have been placed likewise on top of the head, roughly at the rear of the bony nostril opening, because these animals were erroneously thought to have been amphibious, using their large nasal openings as snorkels when submerged. Amerikalik paleontolog Lawrence M. Witmer rejected this reconstruction in 2001, pointing out that all living umurtqali hayvonlar land animals have their external fleshy nostrils placed at the front of the bony nostril. The fleshy nostrils of such sauropods would have been placed in an even more forward position, at the front of the narial fossa, the depression which extended far in front of the bony nostril toward the snout tip.[89]

Czerkas speculated on the function of the peculiar brachiosaurid nose, and pointed out that there was no conclusive way to determine where the nostrils where located, unless a head with skin impressions was found. He suggested that the expanded nasal opening would have made room for tissue related to the animal's ability to smell, which would have helped smell proper vegetation. He also noted that in modern reptiles, the presence of bulbous, enlarged, and uplifted nasal bones can be correlated with fleshy horns and knobby protuberances, and that Braxiosaurus and other sauropods with large noses could have had bezak nasal crests.[74]

It has been proposed that sauropods, including Braxiosaurus, may have had probozlar (trunks) based on the position of the bony narial orifice, to increase their upward reach. Fabien Knoll and colleagues disputed this for Diplodokus va Kamarasaurus in 2006, finding that the opening for the yuz nervi in the braincase was small. The facial nerve was thus not enlarged as in elephants, where it is involved in operating the sophisticated musculature of the proboscis. However, Knoll and colleagues also noted that the facial nerve for Giraffatitan was larger, and could therefore not discard the possibility of a proboscis in this genus.[90]

Metabolizm

Boshqa sauropodlar singari, Braxiosaurus was probably homeothermic (maintaining a stable internal temperature) and endotermik (controlling body temperature through internal means) at least while growing, meaning that it could actively control its body temperature ("warm-blooded "), producing the necessary heat through a high basic metabolic rate of its cells.[75] Russel (1989) used Braxiosaurus as an example of a dinosaur for which endothermy is unlikely, because of the combination of great size (leading to overheating) and great kaloriya needs to fuel endothermy.[91] Sander (2010) found that these calculations were based on incorrect body mass estimates and faulty assumptions on the available cooling surfaces, as the presence of large air sacs was unknown at the time of the study. These inaccuracies resulted in the overestimation of heat production and the underestimation of heat loss.[75] The large nasal arch has been postulated as an adaptation for cooling the brain, as a surface for bug'lanish cooling of the blood.[91]

Air sacs

Dorsal vertebrae of the holotype; the openings at their lower sides are pleurocoels, bu orqali air sacs invaded the bone and connected with air cells inside

The respiration system of sauropods, like that of birds, made use of air sacs. There was not a bidirectional airflow as with mammals, in which the lungs function as körükler, first inhaling and then exhaling air. Instead the air was sucked from the traxeya into an abdominal air sac in the belly which then pumped it forward through the parabranchi, air loops, of the stiff lung. Valves prevented the air from flowing backward when the abdominal air sac filled itself again; at the same time a cervical air sac at the neck base sucked out the spent air from the lung. Both air sacs contracted simultaneously to pump the used air out of the trachea. This procedure guaranteed a unidirectional airflow, the air always moving in a single forward direction in the lung itself. This significantly improved the kislorod intake and the release of karbonat angidrid. Not only was dead air removed quickly but also the blood flow in the lung was counterdirectional in relation to the airflow, leading to a far more effective gaz almashinuvi.[92]

In sauropods, the air sacs did not simply function as an aid for respiration; by means of air channels they were connected to much of the skeleton. These branches, the diverticula, via pneumatic openings invaded many bones and strongly hollowed them out. It is not entirely clear what the evolutionary benefit of this phenomenon was but in any case it considerably lightened the skeleton. They might also have removed excess heat to aid thermoregulation.[92]

In 2016, Mark Hallett and Mathew Wedel for the first time reconstructed the entire air sac system of a sauropod, using B. altitoraks as an example of how such a structure might have been formed. In their reconstruction a large abdominal air sac was located between the pelvis and the outer lung side. As with birds, three smaller sacs assisted the pumping process from the underside of the breast cavity: at the rear the posterior thoracic air sac, in the middle the anterior thoracic air sac and in front the clavicular air sac, in that order gradually diminishing in size. The cervical air sac was positioned under the shoulder blade, on top of the front lung. The air sacs were via tubes connected with the vertebrae. Diverticula filled the various fossae and pleurocoels that formed depressions in the vertebral bone walls. These were again connected with inflexible air cells inside the bones.[92]

O'sish

Voyaga etmagan B. sp. specimen SMA 0009 (the skull is reconstructed following the initial diplodokoid identification), Sauriermuseum Aathal

The ontogenez ning Braxiosaurus has been reconstructed by Carballido and colleagues in 2012 based on SMA 0009, a postcranial skeleton of a young juvenile with an estimated total body length of just 2 meters (6.6 ft). This skeleton shares some unique traits with the B. altitoraks holotype, indicating it is referable to this species. These commonalities include an elevation on the rear blade of the ilium; the lack of a postspinal lamina; vertical neural spines on the back; an ilium with a subtle notch between the appendage for the ischium and the rear blade; and the lack of a side bulge on the upper thighbone. There are also differences; these might indicate that the juvenile is not a B. altitoraks individual after all, but belongs to a new species. Alternatively, they might be explained as juvenile traits that would have changed when the animal matured.[93]

Such ontogenetic changes are especially to be expected in the proportions of an organism. The middle neck vertebrae of SMA 0009 are remarkably short for a sauropod, being just 1.8 times longer than high, compared with a ratio of 4.5 in Giraffatitan. This suggests that the necks of brachiosaurids became proportionally much longer while their backs, to the contrary, experienced relative negative growth. The humerus of SMA 0009 is relatively robust: it is more slender than that of most basal titanosauriforms but thicker than the upper arm bone of B. altitoraks. This suggests that it was already lengthening in an early juvenile stage and became even more slender during growth. This is in contrast to diplodocoids and basal macronarians, whose slender humeri are not due to such allometrik o'sish. Braxiosaurus also appears to have experienced an elongation of the metacarpals, which in juveniles were shorter compared to the length of the radius; SMA 0009 had a ratio of just 0.33, the lowest known in the entire Neosauropoda.[93]

Another plausible ontogenetic change is the increased pnevmatizatsiya of the vertebrae. During growth, the diverticula of the air sacs invaded the bones and hollowed them out. SMA 0009 already has pleurocoels, pneumatic excavations, at the sides of its neck vertebrae. These are divided by a ridge but are otherwise still very simple in structure, compared with the extremely complex ridge systems typically shown by adult derived sauropods. Its dorsal vertebrae still completely lack these.[93]

Two traits are not so obviously linked to ontogeny. The neural spines of the rear dorsal vertebrae and the front sacral vertebrae are extremely compressed transversely, being eight times longer from front to rear than wide from side to side. The spinodiapophyseal lamina or "SPOL", the ridge normally running from each side of the neural spine toward each diapophysis, the transverse process bearing the contact facet for the upper rib head, is totally lacking. Both traits could be avtomomorfiyalar, unique derived characters proving that SMA 0009 represents a distinct species, but there are indications that these traits are growth-related as well. Of the basal sauropod Tazoudasaurus a young juvenile is known that also lacks the spinodiapophyseal lamina, whereas the adult form has an incipient ridge. Furthermore, a very young juvenile of Evropasaurus had a weak SPOL but it is well developed in mature individuals. These two cases represent the only finds in which the condition can be checked; they suggest that the SPOL developed during growth. As this very ridge widens the neural spine, its transverse compression is not an independent trait and the development of the SPOL plausibly precedes the thickening of the neural spine with more mature animals.[93]

Sauropods were likely able to sexually reproduce before they attained their maximum individual size. The maturation rate differed between species. Its bone structure indicates that Braxiosaurus was able to reproduce when it reached 40% of its maximal size.[94]

Paleoekologiya

Map showing locations of brakiosaurid dan qoladi Morrison shakllanishi (gray); 5 (middle left) is the B. altitoraks tipdagi joy

Braxiosaurus is known only from the Morrison Formation of western North America (following the reassignment of the African species).[4] The Morrison Formation is interpreted as a yarimarid environment with distinct ho'l va quruq fasllar,[95][96] va tekis toshqinlar.[95] Several other sauropod genera were present in the Morrison Formation, with differing body proportions and feeding adaptations.[26][97] Ular orasida edi Apatosaurus, Barosaurus, Kamarasaurus, Diplodokus, Haplocanthosaurusva Supersaurus.[26][98] Braxiosaurus was one of the less abundant Morrison Formation sauropods. In a 2003 survey of over 200 fossil localities, John Foster reported 12 specimens of the genus, comparable to Barosaurus (13) va Haplocanthosaurus (12), but far fewer than Apatosaurus (112), Kamarasaurus (179), and Diplodokus (98).[26] Braxiosaurus fossils are found only in the lower-middle part of the expansive Morrison Formation (stratigraphic zones 2–4), dated to about 154–153 million years ago,[99] unlike many other types of sauropod which have been found throughout the formation.[26] If the large foot reported from Wyoming (the northernmost occurrence of a brachiosaurid in North America) did belong to Braxiosaurus, the genus would have covered a wide range of latitudes. Brachiosaurids could process tough vegetation with their broad-crowned teeth, and might therefore have covered a wider range of vegetational zones than for example diplodocids. Camarasaurids, which were similar in tooth morphology to brachiosaurids, were also widespread and are known to have migrated seasonally, so this might have also been true for brachiosaurids.[36]

Other dinosaurs known from the Morrison Formation include the predatory tropodlar Koparion, Stokesosaurus, Ornitholestes, Ceratosaurus, Allosaurus va Torvosaurus, as well as the herbivorous ornithischians Camptosaurus, Dryosaurus, Otnieliya, Gargoyleosaurus va Stegosaurus.[100] Allosaurus accounted for 70 to 75% of theropod specimens and was at the top trofik daraja of the Morrison oziq-ovqat tarmog'i.[101] Ceratosaurus might have specialized in attacking large sauropods, including smaller individuals of Braxiosaurus.[84] Other vertebrates that shared this paleoenvironment included ray-finned fishes, qurbaqalar, salamanderlar, toshbaqalar kabi Dorsetokelis, sfenodontlar, kaltakesaklar, terrestrial and aquatic crocodylomorphans kabi Hoplosuchus va bir nechta turlari pterosaur kabi Harpaktognatus va Mesadaktil. Chig'anoqlari ikkilamchi va suvda shilliq qurtlar ham keng tarqalgan. The flora of the period has been revealed by fossils of yashil suv o'tlari, qo'ziqorinlar, moxlar, ot quyruqlari, tsikllar, ginkgoes, and several families of ignabargli daraxtlar. Vegetation varied from river-lining forests in otherwise treeless settings (gallery forests ) bilan daraxt ferns va ferns, to fern savannalar with occasional trees such as the Araukariya -like conifer Brakifillum.[102]

Madaniy ahamiyati

Child with the Potter Creek humerus, 1959

Riggs in the first instance tried to limit public awareness of the find. When reading a lecture to the inhabitants of Grand Junction, illustrated by lantern slides, on 27 July 1901, he explained the general evolution of dinosaurs and the exploration methods of museum field crews but did not mention that he had just found a spectacular specimen.[103] He feared that teams of other institutions might soon learn of the discovery and take away the best of the remaining fossils. A week later, his host Bradbury published an article in the local Grand Junction yangiliklari announcing the find of one of the largest dinosaurs ever. On 14 August, The New York Times brought the story.[104] At the time sauropod dinosaurs appealed to the public because of their great size, often exaggerated by sensationalist newspapers.[105] Riggs in his publications played into this by emphasizing the enormous magnitude of Braxiosaurus.[106]

Braxiosaurus has been called one of the most iconic dinosaurs, but most popular depictions are based on the African species B. brancai which has since been moved to its own genus, Giraffatitan.[4] A asosiy kamar asteroid, 1991 yil GX7, nomi berilgan 9954 Brachiosaurus in honor of the genus in 1991.[107][108] Braxiosaurus was featured in the 1993 movie Yura parki, as the first computer generated dinosaur shown.[109] These effects were considered ground-breaking at the time, and the awe of the movie's characters upon seeing the dinosaur for the first time was mirrored by audiences.[110][111] The movements of the movie's Braxiosaurus were based on the gait of a giraffe combined with the mass of an elephant. A scene later in the movie used an animatronik head and neck, for when a Braxiosaurus interacts with human characters.[109] The digital model of Braxiosaurus ichida ishlatilgan Yura parki later became the starting point for the ronto models in the 1997 special edition of the film Yulduzli urushlar IV-qism: Yangi umid.[112]

Adabiyotlar

  1. ^ a b v d e f g h men j k l Riggs, E.S. (1903). "Brachiosaurus altithorax, the largest known dinosaur". Amerika Ilmiy jurnali. 4. 15 (88): 299–306. Bibcode:1903AmJS...15..299R. doi:10.2475/ajs.s4-15.88.299.
  2. ^ a b Glut, D.F. (1997). "Braxiosaurus". Dinozavrlar: Entsiklopediya. McFarland & Company. pp.213 –221. ISBN  978-0-89950-917-4.
  3. ^ a b Tyorner, CE .; Peterson, F. (1999). "Biostratigraphy of dinosaurs in the Upper Jurassic Morrison Formation of the Western Interior, USA". Gillete-da Devid D. (tahrir). Yuta shtatidagi umurtqali hayvonlar paleontologiyasi. Turli nashrlar 99-1. Salt Lake City, Utah: Utah Geological Survey. pp. 77–114. ISBN  978-1-55791-634-1.
  4. ^ a b v d e f g h men j k l m n o p q r s t siz v w x y z aa ab ak reklama ae af ag ah ai aj ak al am an ao Taylor, M.P. (2009). "Qayta baholash Brachiosaurus altithorax Riggs 1903 (Dinosauria, Sauropoda) and its generic separation from Giraffatitan brancai (Janensh 1914)" (PDF). Umurtqali hayvonlar paleontologiyasi jurnali. 29 (3): 787–806. doi:10.1671/039.029.0309. S2CID  15220647.
  5. ^ Brinkman 2010 yil, p. 106.
  6. ^ Brinkman 2010 yil, p. 105.
  7. ^ Brinkman 2010 yil, p. 108.
  8. ^ a b Chenoweth, W.L. (1987). "Riggz tepaligi va Dinozavr tepaligi joylari, Mesa okrugi, Kolorado". Averettda Valter R. (tahrir). Paleontologiya va dinozavr uchburchagi geologiyasi. Grand Junction, Kolorado: G'arbiy Kolorado muzeyi. 97-100 betlar. LCCN  93247073. OCLC  680488874.
  9. ^ Brinkman 2010 yil, p. 111.
  10. ^ Lohman, S.V. (1965). Kolorado shtatidagi Grand Junction hududining geologiyasi va artezian suv ta'minoti. Professional hujjat 451. Reston, Virjiniya: AQSh Geologiya xizmati. 1-149 betlar.
  11. ^ a b v d e f g h Riggs, E.S. (1904). "Opisthocoelian dinozavrlarning tuzilishi va munosabatlari. II qism. Brachiosauridae". Geologik seriyalar (Kolumbiya dala muzeyi). 2 (6): 229–247.
  12. ^ Brinkman 2010 yil, p. 117.
  13. ^ Brinkman 2010 yil, p. 118.
  14. ^ Brinkman 2010 yil, p. 119.
  15. ^ a b v d Riggs, E.S. (1901). "Taniqli eng katta dinozavr". Ilm-fan. 13 (327): 549–550. Bibcode:1901Sci .... 13..549R. doi:10.1126 / science.13.327.549-a. PMID  17801098.
  16. ^ Liddell, XG; Skott, R. "karapushka". Yunoncha-inglizcha leksika. Perseus raqamli kutubxonasi. Olingan 2018-04-06.
  17. ^ Brinkman 2010 yil, p. 243.
  18. ^ Tschopp, E .; Mateus, O.V .; Benson, RBJ (2015). "Diplodocidae (Dinosauria, Sauropoda) ning namunaviy darajadagi filogenetik tahlili va taksonomik qayta ko'rib chiqilishi". PeerJ. 3: e857. doi:10.7717 / peerj.857. PMC  4393826. PMID  25870766.
  19. ^ "Ajablanadigan sayohatchilarni kuting" (Matbuot xabari). Dala muzeyi. 1999-11-26. Arxivlandi asl nusxasi 2000-03-02 da. Olingan 2009-08-27.
  20. ^ "Tanlangan tarixiy fotosuratlardan sarlavhalar (sarlavha raqami GN89396_52c)" (PDF). Dala muzeyi foto arxivlari. Arxivlandi asl nusxasi (PDF) 2009-03-18. Olingan 2009-08-27.
  21. ^ "Oldengate ko'prigi". Arxivlandi asl nusxasi 2019-03-07 da. Olingan 2019-03-06.
  22. ^ a b v d e Jensen, J.A. (1987). "Yuta va Kolorado shtatining so'nggi yurasidan olingan yangi brakiozavr materiali". Buyuk havza tabiatshunos. 47 (4): 592–608.
  23. ^ a b Kurtis, B .; Stadtman, K .; Curtice, L. (1996). "Qayta baholash Ultrasauros macintoshi (Jensen, 1985) ". Moralesda M. (tahrir). Kontinental yura davri: Kontinental yura simpoziumi operatsiyalari. 60. Shimoliy Arizona byulletenining muzeyi. 87-95 betlar.
  24. ^ a b Kurtis, B .; Stadtman, K. (2001). "Vafot etgan Dystylosaurus edwini va qayta ko'rib chiqilishi Supersaurus vivianae". Makkordda, RD; Boaz, D. (tahrir). G'arbiy umurtqali paleontologlar assotsiatsiyasi va janubi-g'arbiy paleontologik simpozium - 2001 yil ishi. 8. Mesa janubi-g'arbiy muzeyi xabarnomasi. 33-40 betlar.
  25. ^ Bonnan, M.F .; Wedel, MJ (2004). "Birinchi marta Braxiosaurus (Dinozavriya, Sauropoda) Oklaxomaning yuqori yura morrison shakllanishidan " (PDF). PaleoBios. 24 (2): 12–21.
  26. ^ a b v d e f g Foster, JR (2003). Morrison Formation (Yuqori Yura) umurtqali hayvonot dunyosining paleoekologik tahlili, Rokki-Tog'li mintaqa, AQSh. Nyu-Meksiko Tabiat Tarixi va Ilmiy Muzeyi 23. Albukerke, Nyu-Meksiko: Nyu-Meksiko Tabiat tarixi va fan muzeyi.
  27. ^ a b v d e f g h Duradgor, K .; Tidwell, V. (1998). "A ning dastlabki tavsifi Braxiosaurus bosh suyagi, Felch kareridan 1, Garden Park, Kolorado ". Zamonaviy geologiya. 23 (1–4): 69–84.
  28. ^ Marsh, O.C. (1891). "Qayta tiklash Triceratops" (PDF). Amerika Ilmiy jurnali. 41 (244): 339–342. Bibcode:1891AmJS ... 41..339M. doi:10.2475 / ajs.s3-41.244.339. S2CID  130653625.
  29. ^ a b Makintosh, J.S .; Berman, DS (1975). "Sauropod dinozavrining tanglay va pastki jag'iga tavsif Diplodokus (Reptilia: Saurischia) ning bosh suyagi tabiatiga oid izohlari bilan Apatosaurus". Paleontologiya jurnali. 49 (1): 187–199. JSTOR  1303324.
  30. ^ a b Tidwell, V. (1996). "Yura davridagi ezilgan dinozavrlarning bosh suyaklarini namoyish qilish uchun tiklash". Moralesda M. (tahrir). Kontinental yura davri: Kontinental yura simpoziumi operatsiyalari. 60. Shimoliy Arizona byulletenining muzeyi.
  31. ^ a b v d e f D'emik, M. D .; Carrano, M. T. (2019). "Yuqori Yura Morrison Formatsiyasidan brakiosaurid sauropod dinozavr materialining qayta tavsifi, AQSh, Kolorado". Anatomik yozuv. 303 (4): 732–758. doi:10.1002 / ar.24198. PMID  31254331. S2CID  195765189.
  32. ^ Jensen, J.A. (1985). "Kolorado Yuqori Yura davridan uchta yangi sauropod dinozavrlari". Buyuk havza tabiatshunos. 45 (4): 697–709. doi:10.5962 / bhl. qism.4439.
  33. ^ a b Olshevskiy, G. (1991). "Archosauria Cope parainfraclass-ning qayta ko'rib chiqilishi, 1869, rivojlangan Crocodylia bundan mustasno" (PDF). Mezozoy davri. 2: 1–196. Arxivlandi asl nusxasi (PDF) 2018-08-19. Olingan 2018-04-14.
  34. ^ Olshevskiy, G.; Olshevskiy, A .; Ford, T. (1988). "So'nggi Yura Shimoliy Amerika brakiyosauridlari". Arxosauriya artikulyatsiyasi. 1 (2): 9–11.
  35. ^ Karballido, J.L .; Marpmann, J.S .; Shvarts-Uings, D. Pabst, B. (2012). "Morrison shakllanishidan voyaga etmagan sauropod namunasi to'g'risida yangi ma'lumotlar va uning tizimli pozitsiyasini qayta baholash" (PDF). Paleontologiya. 55 (2): 567–582. doi:10.1111 / j.1475-4983.2012.01139.x.
  36. ^ a b Maltalik, Entoni; Tsxop, Emanuil; Xolverda, Femke; Burnham, Devid (2018). "Haqiqiy Bigfoot: AQShning Vayoming shtatidan kelgan peslar - bu hozirgi kungacha bildirilgan eng yirik sauropod pesidir va brakiosauridlarning yuqori yura morrison shakllanishida eng shimoliy qismida uchraydi".. PeerJ. 6: e5250. doi:10.7717 / peerj.5250. PMC  6063209. PMID  30065867.
  37. ^ a b v Janensch, V. (1914). "Ubersicht über der Wirbeltierfauna der Tendaguru-Schichten nebst einer kurzen Charakterisierung der neu aufgefuhrten Arten von Sauropoden" [Tendaguru qatlamlari umurtqali hayvonot dunyosiga umumiy nuqtai va yangi ro'yxatga olingan sauropodlar turlarining qisqacha tavsifi] (PDF). Archiv für Biontologie (nemis tilida). 3: 81–110.
  38. ^ a b v Janensch, V. (1929). "Material und Formengehalt der Sauropoden in der Ausbeute der Tendaguru-Expedition" [Tendaguru ekspeditsiyasining sauropod rentabelligi materiallari va qoliplari]. Paleontografiya (nemis tilida). 2 (Qo'shimcha 7): 1-34.
  39. ^ Janensch, V. (1950). "Die Wirbelsäule von Brachiosaurus brancai" [Umurtqa pog'onasi Brachiosaurus brancai] (PDF). Paleontografiya (nemis tilida). 3 (Qo'shimcha 7): 27-93.
  40. ^ Janensch, V. (1961). "Die Gliedmaßen und Gliedmaßengürtel der Sauropoden der Tendaguru-Schichten" [Tendaguru qatlamlari sauropodlarining oyoq-qo'llari va tos kamarlari]. Paleontografiya (nemis tilida). 3 (Qo'shimcha 7): 177-235.
  41. ^ Mayer, G. (2003). Afrikalik dinozavrlar topildi: Tendaguru ekspeditsiyalari. Bloomington, IN: Indiana University Press. ISBN  978-0-253-34214-0.
  42. ^ a b Teylor, M.P. (2011). "Tuzatish: qayta baholash Brachiosaurus altithorax Riggs 1903 (Dinosauria, Sauropoda) va uning Giraffatitan brancai-dan umumiy ajralishi (Janensch 1914)"". Umurtqali hayvonlar paleontologiyasi jurnali. 31 (3): 727. doi:10.1080/02724634.2011.557115. S2CID  198127824.
  43. ^ Janensch, V. (1936). "Die Schädel der Sauropoden Braxiosaurus, Barosaurus und Dikraozavr aus den Tendaguru-Schichten Deutsch-Ostafrikas " [Sauropodlarning bosh suyaklari Braxiosaurus, Barosaurus va Dikraozavr Germaniyaning Sharqiy Afrikasining Tendaguru qatlamlaridan] (PDF). Paleontografiya (nemis tilida). 2: 147–298.
  44. ^ a b v d e f g h Pol, G.S. (1988). "Morrison va Tendaguru brakiozauri gigantlari yangi subgenus tavsifi bilan, Giraffatitanva dunyodagi eng katta dinozavrlarni taqqoslash ". (PDF). Hunteriya. 2 (3).
  45. ^ a b Chure, D .; Britt, B .; Uitlok, J. A .; Uilson, J. A. (2010). "Amerika bo'ridan birinchi to'liq sauropod dinozavr bosh suyagi va sauropod tish protezining evolyutsiyasi". Naturwissenschaften. 97 (4): 379–391. Bibcode:2010NW ..... 97..379C. doi:10.1007 / s00114-010-0650-6. PMC  2841758. PMID  20179896.
  46. ^ a b v d e Mannion, P. D .; Qilingan Pol; Barns, Rozi N.; Mateus, Oktavio (2013). "So'nggi yura davridagi portugaliyalik sauropod dinozavrining osteologiyasi Lusotitan atalaiensis (Makronariya) va bazal titanosauriformalarning evolyutsion tarixi " (PDF). Linnean Jamiyatining Zoologik jurnali. 168: 98–206. doi:10.1111 / zoj.12029.
  47. ^ de Lapparent, A.F.; Zbyszewski, G. (1957). "Les dinosauriens du Portugal" (PDF). Mémoire Service Géologique Portugaliya. 2: 1–63.
  48. ^ a b v d e Upchurch, P .; Barret, PM; Dodson, P. (2004). "Sauropoda". Vayshampelda, D.B.; Dodson, P.; Osmolska, H. (tahrir). Dinozavralar, ikkinchi nashr. Kaliforniya shtatidagi Press universiteti, Berkli. pp.259 –322. ISBN  978-0-520-24209-8.
  49. ^ a b Antunes, M. T .; Mateus, O. (2003). "Portugaliyaning dinozavrlari". Comptes Rendus Palevol. 2 (1): 77–95. doi:10.1016 / S1631-0683 (03) 00003-4.
  50. ^ Lapparent, A.F. de; Klarak, P .; Nougarède, F. (1958). "Nouvelles découvertes de Vertébrés dans les séries continentales au Nord d'Edjelch (markaziy Sahara)". Comptes Rendus Hebdomadaires des Séances de l'Académie des Sciences de Parij. 247: 2399–2402.
  51. ^ a b v de Lapparent, A. F. (1960). Matrani tarjima qilgan Karrano. "Les dinosauriens du" continental intercalaire "du Sahara markaziy"" [Markaziy Sahroning "kontinental interkalerasi" dinozavrlari] (PDF). Mémoires de la Société Géologic de France, Nouvelle Séries 88A (frantsuz tilida). 39 (1–6): 1–57.
  52. ^ a b Seebacher, F. (2001-03-26). "Dinozavrlarning massa-massa aloqalarini allometrik hisoblashning yangi usuli". Umurtqali hayvonlar paleontologiyasi jurnali. 21 (1): 51–60. CiteSeerX  10.1.1.462.255. doi:10.1671 / 0272-4634 (2001) 021 [0051: ANMTCA] 2.0.CO; 2. ISSN  0272-4634.
  53. ^ a b Benson, R. B. J .; Campione, N.S.E .; Karrano, M.T .; Mannion, P. D .; Sallivan, C .; Upchurch, P .; Evans, D.C. (2014). "Dinozavrlar tanasining massa evolyutsiyasi darajasi parrandalar nasl-nasabida 170 million yillik barqaror ekologik yangilikni ko'rsatadi". PLOS biologiyasi. 12 (5): e1001853. doi:10.1371 / journal.pbio.1001853. PMC  4011683. PMID  24802911.
  54. ^ Benson, R. B. J .; Xant, G.; Karrano, M.T .; Campione, N .; Mannion, P. (2018). "Cope qoidasi va dinozavrlar tanasi kattaligi evolyutsiyasining landshafti". Paleontologiya. 61 (1): 13–48. doi:10.1111 / pala.12329.
  55. ^ a b v d e Foster, J. (2007). "Brachiosaurus altithorax". Yura G'arbiy: Morrison shakllanishi dinozavrlari va ularning dunyosi. Indianapolis: Indiana universiteti matbuoti. 205–208 betlar. ISBN  978-0253348708.
  56. ^ Klayn, Nikol; Remes, Kristian; Gee, Kerol T.; Sander, P. Martin (2011). "Ilova: Turli xil bazal sauropodomorflar va sauropodlar uchun nashr etilgan tana ommaviy ma'lumotlarini to'plash". Sauropod dinozavrlari biologiyasi. Indiana universiteti matbuoti. 317-320 betlar. ISBN  978-0-253-35508-9.
  57. ^ Wedel, MJ (2003). "Vertebral pnevmatik, havo yostig'i va sauropod dinozavrlar fiziologiyasi". Paleobiologiya. 29 (2): 243–255. doi:10.1666 / 0094-8373 (2003) 029 <0243: vpasat> 2.0.co; 2.
  58. ^ Wedel, MJ (2003). "Sauropod dinozavrlarida umurtqali pnevmatik kasallik evolyutsiyasi". Umurtqali hayvonlar paleontologiyasi jurnali. 23 (2): 344–357. doi:10.1671 / 0272-4634 (2003) 023 [0344: teovpi] 2.0.co; 2.
  59. ^ Teylor, M.P.; Wedel, MJ (2013). "Nega sauropodlarning bo'yni uzun, nega jirafalarning bo'yni kalta edi". PeerJ. 1 (36): –36. arXiv:1209.5439. Bibcode:2012arXiv1209.5439T. doi:10.7717 / peerj.36. PMC  3628838. PMID  23638372.
  60. ^ a b v d e Kristian, A .; Dzemski, G. (2007). "Servikal skelet holatini tiklash Brachiosaurus brancai Janensch, 1914 yil bo'yin bo'ylab intervertebral stressni tahlil qilish va turli xil yondashuvlar natijalari bilan taqqoslash orqali ". Fosil yozuvlari. 10 (1): 38–49. doi:10.1002 / mmng.200600017.
  61. ^ Klayn, N .; Kristian, A .; Sander, P.M. (2012). "Gistologiya shuni ko'rsatadiki, sauropod dinozavrlaridagi bo'yinning cho'zilgan qovurg'alari suyaklashgan tendonlardir". Biologiya xatlari. 8 (6): 1032–1035. doi:10.1098 / rsbl.2012.0778. PMC  3497149. PMID  23034173.
  62. ^ a b Woodruff, D.C. (2016). "Diplodotsidli sauropodlardagi nuxal ligament rekonstruksiyasi bo'yinning gorizontal ovqatlanish holatini qo'llab-quvvatlaydi". Tarixiy biologiya. 29 (3): 308–319. doi:10.1080/08912963.2016.1158257. S2CID  87437457.
  63. ^ Karrano, Metyu T. (2005). "Sauropodning harakatlanishi evolyutsiyasi". Kristina Kori Rojersda; Jeffri Uilson (tahrir). Sauropodlar: evolyutsiya va paleobiologiya. Oklend, Kaliforniya: Kaliforniya universiteti matbuoti. 229–251 betlar. doi:10.1525 / california / 9780520246232.003.0009. ISBN  9780520246232. S2CID  38974370.
  64. ^ Migeod, F.W.H. (1931). "Britaniya muzeyi Sharqiy Afrika ekspeditsiyasi: 1930 yilda qilingan ishlar hisoboti". Tabiiy tarix jurnali. 3: 87–103.
  65. ^ Makintosh, Jon; X. Osmolska (1990). "Sauropoda". Devid B. Vayshampelda; Piter Dodson; Xalszka Osmolska (tahr.) Dinozavrlar (1 nashr). Berkli: Kaliforniya universiteti matbuoti. p. 376. ISBN  978-0-520-06726-4.
  66. ^ Wedel, Metyu J.; Cifelli, R. L.; Sanders, R .. K. (2000). "Sauropod dinozavrining osteologiyasi, paleobiologiyasi va aloqalari Sauroposeidon". Acta Palaeontologica Polonica. 45: 343–388.
  67. ^ Kingham, R.F. (1962). "Sauropod dinozavrini o'rganish Astrodon Leydi "deb nomlangan. Vashington Junior Fanlar akademiyasi materiallari. 1: 38–44.
  68. ^ a b v D'Emic, M. D. (2012). "Titanozauriform sauropod dinozavrlarning dastlabki evolyutsiyasi" (PDF). Linnean Jamiyatining Zoologik jurnali. 166 (3): 624–671. doi:10.1111 / j.1096-3642.2012.00853.x.
  69. ^ Leonardo Salgado, 1993, "Izohlar Chubutisaurus insignis del Corro (Saurischia, Sauropoda) ", Ameghiniana 30(3): 265–270
  70. ^ Salgado, L., R. A. Coria va J. O. Calvo. 1997. "Titanozaurid sauropodlarning evolyutsiyasi. I: postkranial dalillarga asoslangan filogenetik tahlil". Ameghiniana 34: 3-32
  71. ^ a b Ksepka, D. T .; Norell, M. A. (2010). "Osiyo Brachiosauridae uchun yolg'on dalillar: yangi material Erketu ellisoni va bazal Titanosauriformesning filogenetik bahosi " (PDF). Amerika muzeyi Novitates. 3700: 1–27. doi:10.1206/3700.2. S2CID  86254470.
  72. ^ a b Xenderson, D. M. (2004). "Maslahatchilar: sauropod dinozavrlari pnevmatikligi, suzish qobiliyati va suvda ishlatiladigan odatlar". London Qirollik jamiyati materiallari B. 271 (Qo'shimcha 4) (Qo'shimcha 4): S180-S183. doi:10.1098 / rsbl.2003.0136. PMC  1810024. PMID  15252977.
  73. ^ Jensen, J. A. (1985). "Kolorado Yuqori Yura davridan uchta yangi sauropod dinozavrlari". Buyuk havza tabiatshunos. 45 (4): 697–709. doi:10.5962 / bhl. qism.4439.
  74. ^ a b Czerkas, S. J .; Czerkas, S. A. (1990). Dinozavrlar: global ko'rinish. Limpsfild: Ejderlar dunyosi. pp.134 –135. ISBN  978-0-7924-5606-3.
  75. ^ a b v d Sander, PM; Kristian, A .; Klauss, M .; Fechner, R .; Gee, CT .; Griebeler, E.-M .; Gunga, H.-C .; Xummel, J .; Mallison, X.; Perri, S.F .; Preushoft, X.; Rauhut, O.W.M .; Remes, K .; Tutken, T .; Qanotlar, O .; Vitzel, U. (2010). "Sauropod dinozavrlari biologiyasi: gigantizm evolyutsiyasi". Biologiya sharhlari. 86 (1): 117–155. doi:10.1111 / j.1469-185X.2010.00137.x. PMC  3045712. PMID  21251189.
  76. ^ Stivens, K. A .; Parrish, M. J. (1999). "Ikki yura sauropod dinozavrlarining bo'yin holati va ovqatlanish odatlari". Ilm-fan. 284 (5415): 798–800. Bibcode:1999Sci ... 284..798S. doi:10.1126 / science.284.5415.798. PMID  10221910.
  77. ^ Rieppel, O .; Brochu (1999). "Paleontologlar dinozavrlarni himoya qilishmoqda" (PDF). Dalada. 70: 8.
  78. ^ Fastovskiy, D. E .; Vayshampel, D. B. (2016). Dinozavrlar: qisqacha tabiiy tarix. Kembrij universiteti matbuoti. p. 206. ISBN  978-1107135376.
  79. ^ Gunga, H.-C .; Kirsch, K. (2001). "Von Hochleistungsherzen und wackeligen Hälsen" [Yuqori mahsuldorlik yuraklari va qaltiroq bo'yinlari]. Forschung (nemis tilida). 2–3: 4–9.
  80. ^ Barret, Pol M.; Upchurch, Pol (2005). "Vaqt o'tishi bilan Sauropodomorf xilma-xilligi". Kori Rojersda Kristina A.; Uilson, Jeffri A. (tahrir). Sauropodlar: evolyutsiya va paleobiologiya. Berkli, Kaliforniya: Kaliforniya universiteti. pp.125 –156. ISBN  978-0520246232.
  81. ^ a b Hallett va Wedel 2016 yil, p. 150.
  82. ^ Hallett va Wedel 2016 yil, p. 139.
  83. ^ Hallett va Wedel 2016, p. 90.
  84. ^ a b Hallett va Wedel 2016 yil, p. 233.
  85. ^ Hallett va Wedel 2016 yil, p. 239.
  86. ^ Mallison, H. (2011). "Rearing Gigantlar - sauropod ikki oyoqli va tripodal pozalarini kinetik-dinamik modellashtirish." Klein, N., Remes, K., Gee, C. va Sander M. (tahrir): Sauropod dinozavrlari biologiyasi: gigantlar hayotini tushunish. O'tmish hayoti (seriya tahriri Farlow, J.). Bloomington, IN: Indiana University Press.
  87. ^ Hallett va Wedel 2016 yil, p. 173.
  88. ^ Hallett va Wedel 2016 yil, p. 98.
  89. ^ Witmer, L. M. (2001). "Dinozavrlar va boshqa umurtqali hayvonlardagi burun teshigi holati va uning burun faoliyati uchun ahamiyati". Ilm-fan. 293 (5531): 850–853. CiteSeerX  10.1.1.629.1744. doi:10.1126 / science.1062681. PMID  11486085. S2CID  7328047.
  90. ^ Knoll, F.; Galton, P. M.; Lopez-Antuanzas, R. (2006). "Sauropod dinozavridagi probozga qarshi paleoneurologik dalillar Diplodokus". Geobios. 39 (2): 215–221. doi:10.1016 / j.geobios.2004.11.005.
  91. ^ a b Rassel, D. A. (1989). Vaqtdagi Odisseya: Shimoliy Amerikaning dinozavrlari. Minocqua, Viskonsin: NorthWord Press. p. 78. ISBN  978-1-55971-038-1.
  92. ^ a b v Hallett va Wedel 2016 yil, p. 100-101.
  93. ^ a b v d Karballido, J. L .; Marpmann, J. S .; Shvarts-Uings, D. Pabst, B. (2012). "Morrison shakllanishidan voyaga etmagan sauropod namunasi to'g'risida yangi ma'lumotlar va uning tizimli pozitsiyasini qayta baholash" (PDF). Paleontologiya. 55 (3): 567–582. doi:10.1111 / j.1475-4983.2012.01139.x.
  94. ^ Hallett va Wedel 2016 yil, p. 159.
  95. ^ a b Rassel, D. A. (1989). Vaqtdagi Odisseya: Shimoliy Amerikaning dinozavrlari. Minocqua, Viskonsin: NorthWord Press. 64-70 betlar. ISBN  978-1-55971-038-1.
  96. ^ Engelmann, G.F .; Chure, D.J .; Fiorillo, A.R. (2004). "Quruq iqlimning yuqori yura morrison shakllanishi faunasining paleoekologiyasiga ta'siri". Cho'kindi geologiya. 167 (3–4): 297–308. Bibcode:2004 yilSedG..167..297E. doi:10.1016 / j.sedgeo.2004.01.008.
  97. ^ Foster, J. (2007). "Ilova." Yura G'arbiy: Morrison shakllanishi dinozavrlari va ularning dunyosi. Indiana universiteti matbuoti. 327–329 betlar.
  98. ^ Chure, D.J .; Litvin, R .; Hasiotis, S.T .; Evanoff, E .; Duradgor, K. (2006). "Morrison shakllanishi faunasi va florasi: 2006 yil". Fosterda JR .; Lukas, S.G (tahr.) Paleontologiya va yuqori yura morrison shakllanishi geologiyasi. Nyu-Meksiko Tabiat Tarixi va Ilmiy Muzeyi Axborotnomasi, 36. Albukerke, Nyu-Meksiko: Nyu-Meksiko Tabiat tarixi va fan muzeyi. 233–248 betlar.
  99. ^ Turner, CE va Peterson, F., (1999). "G'arbiy ichki makonning yuqori yura morrison shakllanishidagi dinozavrlarning biostratigrafiyasi, AQSh". Pp. 77–114 yillarda Gillette, D.D. (tahr.), Yuta shtatidagi umurtqali hayvonlar paleontologiyasi. Utah Geological Survey turli xil nashr 99-1.
  100. ^ Chure, Daniel J.; Litvin, Ron; Hasiotis, Stiven T.; Evanoff, Emmet; Duradgor, K. (2006). "Morrison shakllanishi faunasi va florasi: 2006 yil". Fosterda Jon R.; Lukas, Spenser G. (tahr.). Paleontologiya va yuqori yura morrison shakllanishi geologiyasi. Nyu-Meksiko Tabiat Tarixi va Ilmiy Muzeyi Axborotnomasi, 36. Albukerke, Nyu-Meksiko: Nyu-Meksiko Tabiat tarixi va fan muzeyi. 233–248 betlar.
  101. ^ Foster, Jon R. (2003). Morrison shakllanishidagi umurtqali hayvonot dunyosining paleoekologik tahlili (Yuqori Yura davri), Rokki tog 'mintaqasi, AQSh. Nyu-Meksiko Tabiat Tarixi va Ilmiy Muzeyi Axborotnomasi, 23. Albukerke, Nyu-Meksiko: Nyu-Meksiko Tabiat tarixi va fan muzeyi. p. 29.
  102. ^ Duradgor, K. (2006). "Kattaning eng kattasi: mega-souropodni tanqidiy qayta baholash Amphicoelias fragillimus". Fosterda Jon R.; Lukas, Spenser G. (tahrir). Paleontologiya va yuqori yura morrison shakllanishi geologiyasi. Nyu-Meksiko Tabiat Tarixi va Ilmiy Muzeyi Axborotnomasi, 36. Albukerke, Nyu-Meksiko: Nyu-Meksiko Tabiat tarixi va fan muzeyi. 131-138-betlar.
  103. ^ Brinkman 2010 yil, p. 114.
  104. ^ Brinkman 2010 yil, p. 115.
  105. ^ Brinkman 2010 yil, p. 248.
  106. ^ Brinkman 2010 yil, p. 249.
  107. ^ "JPL kichik tanadagi ma'lumotlar bazasi brauzeri: 9954 Brachiosaurus (1991 GX7)". NASA. Olingan 2007-04-28.
  108. ^ Uilyams, G. "Kichik sayyora nomlari: alifbo ro'yxati". Smitson astrofizika rasadxonasi. Olingan 2007-02-10.
  109. ^ a b Shay, D .; Dunkan, J. (1993). Yura parkini yaratish. Nyu-York: Boxtree Ltd. 99-bet, 133-135. ISBN  978-1-85283-774-7.
  110. ^ Xuls, A. (2013). "Yura parki davri: CGI dinozavrlari filmni qanday qilib abadiy o'zgartirgan". Atlantika. Atlantika. Olingan 20 iyul 2018.
  111. ^ Britton, P. (1993). "WOW omil". Ommabop fan: 86–91.
  112. ^ "Ronto". Ma'lumotlar bazasi. Star Wars.com. Arxivlandi asl nusxasi 2008 yil 3 oktyabrda. Olingan 2009-01-13.

Bibliografiya

  • Brinkman, P. D. (2010), Yura dinozavrlarining ikkinchi shoshilishi: yigirmanchi asr boshida Amerikadagi muzeylar va paleontologiya, Chikago va London: Chikago universiteti Press, ISBN  978-0226074726
  • Xallett, M.; Wedel, M. (2016), Sauropod dinozavrlari: Gigantlar davridagi hayot, Baltimor: Jons Xopkins universiteti matbuoti, ISBN  978-1421420288

Tashqi havolalar