Antarktika maxsus muhofaza qilinadigan hudud - Antarctic Specially Protected Area
An Antarktika maxsus muhofaza qilinadigan hudud (ASPA) - materikdagi maydon Antarktida yoki yaqin atrofdagi orollarda, olimlar va bir nechta turli xil xalqaro tashkilotlar tomonidan himoyalangan. Himoyalangan hududlar 1961 yilda tashkil etilgan Antarktika shartnoma tizimi, bu 60 kenglikdan janubdagi barcha er va suvlarni boshqaradi va insoniyat rivojlanishidan himoya qiladi.[1] Har qanday ASPA saytiga kirish uchun ruxsatnoma talab qilinadi.[2] ASPA saytlari Avstraliya, Yangi Zelandiya, AQSh, Buyuk Britaniya, Chili, Frantsiya, Argentina, Polsha, Rossiya, Norvegiya, Yaponiya, Hindiston, Italiya va Koreya Respublikasi hukumatlari tomonidan himoyalangan. Hozirda 72 ta sayt mavjud.
ASPA saytlari ro'yxati
| Raqam | Ism | Tavsif | Qabul qilingan | Koordinatalar | Taxminiy maydon | Rasm |
|---|---|---|---|---|---|---|
| ASPA-101 | Teylor Rookery, Mac. Robertson Land | Maydon Teylor muzligining sharqiy qismida joylashgan shimoliy tosh ta'sirining butun qismidan iborat. Robertson Land. Unda imperator penguenlari koloniyasi mavjud bo'lib, ular ushbu turdagi ma'lum bo'lgan ikkita quruqlikdan kattaroq qismi bo'lib, ular butunlay quruqlikda joylashgan. Pishiriqlar pingvinlar populyatsiyasini uzoq vaqt davomida kuzatib borishgani uchun muhim (1954 yildan beri). | Rec IV-1 | 67 ° 26′00 ″ S 60 ° 50′00 ″ E / 67.4333 ° S 60.8333 ° E | 0,26 km2 (0,10 kvadrat milya) |  |
| ASPA-102 | Rookery orollari, Xolm-Bay, Mac. Robertson Land | Rookery orollari - Xolma ko'rfazining g'arbiy qismida joylashgan Masson va Macdagi Devid Ranges shimolida joylashgan kichik orollar va toshlar guruhi. Robertson Land va Avstraliyaning Mawson stantsiyasidan 10 km g'arbda. Ushbu hudud - bu Mawson mintaqasida yashovchi barcha oltita qush turlarining naslchilik koloniyalarining g'ayrioddiy birlashmasi bilan dengizdagi orolning yashash joyi; ulardan ikkitasi, janubiy gigant petrel va Cape petrel mintaqaning boshqa joylarida uchramaydi. | Rec IV-2 | 67 ° 36′36 ″ S 62 ° 32′06 ″ E / 67.61 ° S 62.535 ° E | 1,67 km2 (0,64 kvadrat milya) | |
| ASPA-103 | Arderi oroli va Odbert oroli, Budd sohili, Uilkes Land | Arderi oroli va Odbert oroli Vincennes ko'rfazining janubida, Sharqiy Antarktidaning Uilkes Land Budda sohilida joylashgan Shamol tegirmoni orollarining eng janubiy qismidir. Sayt petrelning bir nechta naslchilik turlarini qo'llab-quvvatlaydi va ularning yashash joylariga misol keltiradi. Antarktidaning sharqiy qismida to'rtta to'la dengiz petrelllari taqqoslashni o'rganish uchun etarli miqdordagi bir joyda ko'payadigan boshqa oson joy yo'q. Ushbu to'rt naslni bir joyda o'rganish Janubiy Okean ekotizimini tushunish va kuzatishda yuqori ekologik ahamiyatga ega. Bundan tashqari, ikkala orolda Uilsonning bo'ronli petrellari va Antarktika skualarining ko'payadigan populyatsiyalari mavjud; va Odbert oroli Adeli pingvinlarining ko'payadigan populyatsiyasini qo'llab-quvvatlaydi. | Rec IV-3 | 66 ° 23′06 ″ S 110 ° 29′50 ″ E / 66.385 ° S 110.4972 ° E | 2,44 km2 (0,94 kv mil) | |
| ASPA-104 | Sabrina oroli, Shimoliy Ross dengizi | Balleny orollari Pennell qirg'og'idan shimoliy Viktoriya eridan 325 km uzoqlikda joylashgan. ASPA tarkibiga dengiz sathidan baland bo'lgan Sabrina oroli, shu jumladan Monolit va Chinstrap orollari kiradi. Hudud ekologik va ilmiy ahamiyatga ega. Bu asosiy Antarktika qirg'oq oqimi ichida joylashgan yagona okean arxipelagi bo'lgan Balleni orollarining vakili namunasidir. Shunday qilib, ular dengiz qushlari va muhr turlari uchun muhim dam olish va etishtirish muhitini ta'minlaydi va turli xil turlarning sirkumpolyar tarqalishida muhim ahamiyatga ega. Izolyatsiya qilingan va qiyin ob-havo va muz sharoitlariga moyil bo'lgan Orollar odamlarning bezovtalanishini juda kam boshlagan. | Rec IV-4 | 66 ° 55′00 ″ S 163 ° 19′00 ″ E / 66.9167 ° S 163.3167 ° E | 1,5 km2 (0,58 kvadrat milya) | |
| ASPA-105 | Bofort oroli, McMurdo Sound, Ross dengizi | Maydon butun Bouortort orolini o'rtacha yuqori suv belgisidan yuqoriroqqa qamrab oladi va naslli imperator pingvinlari egallagan qo'shni tez muzni o'z ichiga oladi. Orolda muhim avifauna mavjud va u mintaqadagi naslchilikning eng muhim joylaridan biridir. U muzli yadroli moren skameykasida o'simliklarning muhim maydoniga ega, bu uning miqdori va sifati jihatidan alohida va McMurdo Sound mintaqasi uchun taniqli moxlarning eng keng va doimiy maydonidir. Shuningdek, u qizil qor yosunlari kuzatilgan eng janubiy joylardan birini anglatadi. | Rec IV-5 | 76 ° 59′00 ″ S 167 ° 00′00 ″ E / 76.9833 ° S 167.0 ° E | 14,16 km2 (5,47 kvadrat milya) |  |
| ASPA-106 | Cape Hallett, Shimoliy Viktoriya erlari, Ross dengizi | Cape Hallett shimoliy Viktoriya erining Moubray ko'rfazining janubiy uchida, Ross dengizining g'arbiy qismida joylashgan. Bu hudud Viktoriya Land va Ross dengizi kenglik gradyanining shimoliy uchida ma'lum bo'lgan eng keng va vakillik namunalari bo'lgan o'simlik jamoalari bilan turli xil yashash joylarini o'z ichiga oladi. Shuningdek, saytda janubiy qutbli skualar va katta Adélie pingvin koloniyasi ham uyalar. Insonlarning koloniyaga ta'siri tarixi ushbu saytni noyob va ekologik tizim buzilishidan keyin koloniyaga ta'sirini tiklash va tiklash bo'yicha ilmiy tadqiqotlar uchun ideal qiladi. Hudud mo'l-ko'l biologik resurslarning kombinatsiyasi bilan ajoyib estetik qadriyatlarga ega. Sobiq stantsiyadagi inson faoliyati tarixi ham tashrif buyuruvchilarni qiziqtiradi. | Rec IV-7 | 72 ° 19′00 ″ S 170 ° 16′00 ″ E / 72.3167 ° S 170.2667 ° E | 0,53 km2 (0,20 kvadrat milya) | |
| ASPA-107 | Imperator oroli, Dion orollari, Margerit ko'rfazi, Antarktika yarim oroli | Dion orollari, bir nechta orollar, toshlar va riflarni o'z ichiga olgan kichik arxipelag, Marguerite ko'rfazidagi Adelaida orolining janubi-g'arbiy qismidan 13,5 km janubda joylashgan. Sayt Antarktida yarim orolining g'arbiy qismida mavjud bo'lgan ma'lum bo'lgan imperator pingvinlarining yagona koloniyasini o'z ichiga oladi va ushbu koloniyaning boshqa turlardan ajratilishi uni juda katta ilmiy qiziqish uyg'otadi. Shuningdek, u eng shimoliy va ehtimol eng kichik imperator pingvin koloniyasidir va naslchilik quruqlikda sodir bo'ladigan ikkitadan biridir. Adeli pingvinlari va ko'k ko'zli shaglar ham bu erda ko'payadi. | Rec IV-8 | 67 ° 52′00 ″ S 68 ° 42′00 ″ Vt / 67.8667 ° S 68.7 ° Vt | 4.67 km2 (1,80 kvadrat milya) | |
| ASPA-108 | Yashil orol, Berthelot orollari, Antarktika yarim oroli | Yashil orol - Antarktika yarim orolining Grem qirg'og'idan taxminan 3 km uzoqlikda joylashgan Grandidier kanalidagi Berthelot orollari guruhining eng yirik qismidan 150 m shimolda joylashgan kichik orol. Mintaqadagi o'simliklar juda boy, mox çiminin yaxshi rivojlangan uzluksiz qirg'oqlari va Antarktika soch maysalarining kichik qismlari. Yashil orolidagi o'simliklar bir vaqtlar o'ylab ko'rganidek mintaqaviy jihatdan xilma-xil bo'lmasa-da, so'nggi yillarda u shimoliy orollarga Antarktika mo'yna muhrlari ta'sir qilganligi sababli mox banklariga katta zarar etkazishdan qutuldi. Katta ko'k ko'zli soqol koloniyasi, jigarrang skualar, janubiy qutbli skualar va duragaylar ham uchraydi. Ko'k ko'zli kormorantlar koloniyasi, ehtimol Antarktika yarim orolidagi eng yiriklardan biridir. | Rec IV-9 | 65 ° 19′00 ″ S 64 ° 09′00 ″ Vt / 65.3167 ° S 64.15 ° Vt | 0,17 km2 (0,066 kvadrat milya) | |
| ASPA-109 | Moe oroli, Janubiy Orkney orollari | Moe oroli, Janubiy Orkney orollari, Siny orolining janubi-g'arbiy qismidan 300 metr uzoqlikda joylashgan kichik tartibsiz shakldagi orol, uni Fyr kanali ajratib turadi. Unda dengiz Antarktika ekotizimining, shu jumladan mox maysazorining yirik qirg'oqlari va chinstrap pingvinlari koloniyalarining, Cape petrell va Antarktika prionlarining vakillik namunasi keltirilgan. Weddell muhrlari va mo'ynali muhrlar ham orolning plyajlarida olib boriladi. Moe oroli mo'ynali muhrlarning buzilishi sababli intensiv ilmiy izlanishlarga va past balandlikdagi er usti tizimidagi katta o'zgarishlarga duchor bo'lgan qo'shni Signy oroli bilan kelajakda taqqoslash uchun nazorat zonasi sifatida himoyalangan. Bundan tashqari, Moe orolida Antarktidada topilgan Chorisodontium-Polytrichum mox çiminin eng katta uzluksiz kengliklari mavjud. | Rec IV-13 | 60 ° 44′00 ″ S 45 ° 41′00 ″ Vt / 60.7333 ° S 45.6833 ° Vt | 1,2 km2 (0,46 kvadrat milya) | |
| ASPA-110 | Lynch oroli, Janubiy Orkney orollari | Lynch oroli - bu Janubiy Orkney orollaridagi Marshall ko'rfazining sharqiy qismida, Koronatsiya orolidan 200 m janubda va Siny orolidan 2,4 km shimolda joylashgan kichik orol. Ushbu hudud dengizning orollari va toshlarini hisobga olmaganda, suv oqimining past darajasidan yuqori bo'lgan butun orolni o'z ichiga oladi. Orol Antarktika Shartnomasi hududida ma'lum bo'lgan Antarktika tukli o'tlarining eng keng va zich stendlaridan birini qo'llab-quvvatlaydi; noyob tabiiy ekologik tizimning ajoyib namunasi. Moxlarning bir nechta turlari g'ayrioddiy unumdor bo'lib, tuproq tarkibida boy umurtqasizlar faunasi mavjud. Antarktika muhrlarining aksariyat turlari orol atrofida keng tarqalgan. Antarktika mo'ynali muhrlarining mahalliy zarariga qaramay, odamlarning tashrifi, ilmiy izlanishlari va tanlab olishlari natijasida cheklangan bezovtaliklari, mo'ynali muhr faoliyati natijasida sezilarli o'zgarishlarni boshdan kechirayotgan taqqoslanadigan ekotizimlarga qarshi o'lchov maydoni sifatida maydon potentsial ahamiyatga ega ekanligini anglatadi. | Rec IV-14 | 60 ° 39′10 ″ S 45 ° 36′25 ″ Vt / 60.6528 ° S 45.6069 ° Vt | 0,15 km2 (0,058 kvadrat milya) | |
| ASPA-111 | Janubiy Pauell oroli va qo'shni orollar, Janubiy Orkney orollari | Bu hududga butun Priell orolining janubiy cho'qqisi kengligidan janubda (375 m balandlikda) Fredriksen oroli, Mishelsen oroli, Kristoffersen oroli, Grey orol va noma'lum qo'shni orollar kiradi. Janubiy Pauell oroli va unga qo'shni orollar florani qo'llab-quvvatlaydi va Janubiy Orkney orollarining tabiiy ekologiyasining ko'plab qushlar va sutemizuvchilar faunasi vakillarini qo'llab-quvvatlaydi, ular mo'ynali muhrlarning uzoq vaqtdan beri rivojlanib kelayotgan koloniyasining mavjudligi bilan muhimroq ahamiyatga ega. | Rec IV-15 | 60 ° 42′00 ″ S 45 ° 01′00 ″ Vt / 60,7 ° S 45,0167 ° Vt | 23,56 km2 (9,10 kvadrat milya) | |
| ASPA-112 | Koppermin yarim oroli, Robert oroli, Janubiy Shetland orollari | Koppermin yarim oroli janubiy Shetland orollari arxipelagi o'rtasida, sharqda Nelson orolida va g'arbda Grinvich orolida joylashgan Robert orolining g'arbiy qismida joylashgan. Bu turli xil quruqlikdagi fauna va boy avifauna bilan birgalikda boy o'simliklarni qo'llab-quvvatlovchi biologik xilma-xil hudud. Antarktidadagi eng katta doimiy mox stendlaridan biriga ega. Chinstrap pingvinlari, janubiy gigant petrellar, Uilsonning bo'ronli petrellari, Antarktida ternlari, Dominikan gullalari, fil muhrlari, Ueddell muhrlari va mo'ynali muhrlar ham uchraydi. | Rec VI-10 | 62 ° 23′00 ″ S 59 ° 42′00 ″ Vt / 62.3833 ° S 59.7 ° Vt | 0,67 km2 (0,26 kvadrat milya) |  |
| ASPA-113 | Litchfild oroli, Artur Makoni, Anvers oroli, Palmer arxipelagi | Litchfild oroli Artur-Harbor, SW-Anvers orolida joylashgan. O'zining dengiz sohilidagi zonasi bilan birgalikda u dengiz va quruqlikdagi hayotning juda yuqori to'plamiga ega, oltita turdagi mahalliy parrandalar ko'payadigan joy sifatida qo'shni orollar orasida noyobdir va Antarktika yarim orolining tabiiy ekologik tizimining ajoyib namunasini taqdim etadi. Bundan tashqari, Litchfild oroli o'simliklarning boy o'simtalariga ega va Artur-Harbordagi orollarning er yuzidagi yashash joylarining eng xilma-xilligi va eng xilma-xilligiga ega. | Rec VIII-1 | 64 ° 46′00 ″ S 64 ° 06′00 ″ Vt / 64.7667 ° S 64.1 ° Vt | 0,36 km2 (0,14 kvadrat milya) | |
| ASPA-114 | Shimoliy Koronatsiya oroli, Janubiy Orkney orollari | Ushbu hudud shimoliy Koronatsiya orolining (Janubiy Orkney orollarining eng kattasi) g'arbiy qismida Kontseptsiya punkti va sharqida Foul nuqtasi orasidagi hududni o'z ichiga oladi. Sayt dengiz qirg'og'ining yirik koloniyalariga va likenlarga asoslangan jarliklarga ega bo'lgan qirg'oqlarning muzsiz hududlarini qamrab oladi. Brisben Heights platosiga ko'tarilgan doimiy muz Antarktika dengizining shimoliy chegarasi yaqinida toza muz muhitining ajoyib vakolatxonasini ta'minlaydi. Hududning o'zaro bog'liq quruqlik, muz va dengiz komponentlari dengiz Antarktida muhitiga xos bo'lgan qirg'oq, doimiy muz va sublittoral ekotizimlarning yaxlit namunasini o'z ichiga oladi. u mintaqaning asosiy potentsial qiymati ko'proq ta'sirlangan saytlar bilan taqqoslash tadqiqotlarida foydalanish uchun mos yozuvlar maydoni hisoblanadi. | Rec XIII-10 | 60 ° 33′00 ″ S 45 ° 35′00 ″ Vt / 60.55 ° S 45.5833 ° Vt | 91,76 km2 (35,43 kvadrat milya) | |
| ASPA-115 | Lagotellari oroli, Margerit ko'rfazi, Grem Land | Lagotellerie oroli Marguerite ko'rfazida, Fallières sohilida, Grem Landda, Adelaida orolidagi Rothera nuqtasining 46 km SE qismida, Porquois Pas orolidan 11 km janubda va Tog'li orolning janubiy uchidan 3,25 km g'arbda joylashgan. Orolda janubiy Antarktika yarim oroliga xos bo'lgan nisbatan xilma-xil o'simlik va hayvonot dunyosi mavjud. 10 m2 gacha bo'lgan stendlarni tashkil etadigan va Janubiy Shetland orollarining janubida ma'lum bo'lgan eng yirik stendlar qatoriga kiradigan faqat ikkita Antarktika gulli o'simliklarining ko'pligi diqqatga sazovordir, sayoz tuproq tuproq o'simlik va uning bilan bog'langan umurtqasizlar faunasi ostida rivojlangan. mikrobiyota, ehtimol, ushbu kenglikda noyobdir. Shuningdek, taxminan 1000 juft Adeli penguenlaridan iborat koloniya va ko'k ko'zli shaglarning eng janubiy koloniyalaridan biri mavjud. Orolda ko'plab jigarrang va janubiy qutbli skualar ham ko'payadi. | Rec XIII-11 | 67 ° 53′00 ″ S 67 ° 24′00 ″ Vt / 67.8833 ° S 67.4 ° Vt | 1,62 km2 (0,63 kvadrat milya) | |
| ASPA-116 | Yangi kollej vodiysi, Caughley Beach, Cape Bird, Ross oroli | Yangi kollej vodiysi Keyp Birdning janubida, Keyfi Qushning Shimoliy va O'rta roukeries deb nomlanuvchi Adélie penguen roukeries o'rtasida joylashgan Caughley Beach ustidagi muzsiz yamaqlar ustida joylashgan. Bu hudud janubiy Viktoriya Landidagi mox, suv o'tlari va likenlarning eng keng va hashamatli stendlari joylashgan joy; sayt ichidagi er usti ekotizimi uzoq muddatli tadqiqot mavzusidir. Kriptogamik o'simliklarning oyoq osti qilinishidan zararlanishiga moyilligi sababli, maydonning belgilanishi uning biotasini himoya qiladi. Cheklangan zona qo'riqlash qo'riqxonasi bo'lib, unga kirishning yanada qattiq shartlari mavjud | Rec XIII-12 | 77 ° 13′00 ″ S 166 ° 29′00 ″ E / 77.2167 ° S 166.4833 ° E | 0,34 km2 (0,13 kvadrat milya) | |
| ASPA-117 | Qushlar oroli, Margerit ko'rfazi, Antarktika yarim oroli | Qushlar oroli shimoliy g'arbiy Margerit ko'rfazida, Adelaida orolidan 400 m janubda, Antarktida yarim orolining g'arbiy qismida joylashgan. Bu joy juda ko'p ornitologik ahamiyatga ega va Antarktika yarim orolida o'zining mo'lligi va xilma-xilligi bilan ajralib turadi, olti xil dengiz qushi bir-biriga juda yaqin joyda ko'payadi. Bularga Adeli penguenlari, ko'k ko'zli kormorantlar, janubiy gigant petrellar, suv o'tlari martalalari, skuas va Uilson bo'ronli petrellari kiradi. Ushbu koloniyalarning bir nechtasi o'z mintaqalarining eng janubiy chegaralarida joylashgan va ularning umumiy mintaqaviy populyatsiyasiga muhim hissa qo'shganlar. | Rec XVI-4 | 67 ° 46′00 ″ S 68 ° 54′00 ″ Vt / 67.7667 ° S 68.9 ° Vt | 1,12 km2 (0,43 kvadrat milya) | |
| ASPA-118 | Sammit Melburn tog'i, Viktoriya Land | Melburn tog'i Ross dengizining g'arbiy qismida joylashgan Viktoriya Land shimolida. U Wood Bay va Terra Nova ko'rfazi o'rtasida, Kempbell muzligidan 10 km sharqda joylashgan. Bu hudud Antarktidadagi boshqa dengiz va balandlikdagi boshqa geotermik joylarga nisbatan yuqori bioxilma-xillikni namoyish etadi. Fumarollar tomonidan yaratilgan eng iliq erlar mox, jigar qurti va suv o'tlari yamoqlarini qo'llab-quvvatlaydi, shu bilan birga umurtqasizlar protozoyasining bir turi. Bunga Antarktika qit'asidagi mox Campylopus pyriformisning ma'lum bo'lgan yagona bargli namunasi va jigar qurti sefaloziella varianlarining noyob kontinental ko'rinishi kiradi. Erebus va Rittman tog'lari cho'qqilariga yaqin bo'lgan boshqa ma'lum bo'lgan baland balandlik bilan solishtiradigan bo'lsak, geotermik ta'sir ko'rsatadigan muzsiz hududlar. | Rec XIV-5 | 74 ° 21′S 164 ° 42′E / 74.35 ° S 164.7 ° E | 6,56 km2 (2,53 kvadrat milya) | |
| ASPA-119 | Devis vodiysi va Forlidas suv havzasi, Dufek massivi, Pensakola tog'lari | Devis vodiysi va Forlidas suv havzasi Transansarktik tog 'tizmasining bir qismi bo'lgan Pensakola tog'larining shimoliy-sharqiy Dyufek massivida joylashgan. Ushbu hudud Antarktidada ma'lum bo'lgan eng toza janubdagi suv havzalarini o'z ichiga oladi, ular toza va toza suv ekotizimlari va ularni yig'ish uchun noyob namunalar sifatida himoyalangan. Ular ushbu muhitlarning paydo bo'lishining eng yuqori chegaralariga yaqin biologik jamoalarni ilmiy o'rganish uchun noyob imkoniyatlarni yaratadilar. Hudud Antarktidadagi eng toza muzsiz vodiy tizimlaridan biri ekanligiga ishonishadi va shuning uchun Antarktika muz qatlamining iqlim o'zgarishiga ta'sirini tushunadigan tadqiqotlar uchun yo'nalish sifatida ajoyib imkoniyatlarga ega. | Rec XVI-9 | 82 ° 27′S 51 ° 21′W / 82,45 ° S 51,35 ° V | 56,81 km2 (21,93 kvadrat milya) | |
| ASPA-120 | Pointe-Geologie arxipelagi, Terre Adélie | Hudud to'rtta oroldan iborat: Jan Rostand, Le Mogen, Lamark va Klod Bernard; nunatak va Adeli qirg'og'ining qirg'oq mintaqasida joylashgan Cape Geology Archipelago qalbida joylashgan imperator pingvinlari uchun joy. Bu muhim biologik, geologik va estetik ahamiyatga ega bo'lgan mintaqadir. U o'simlik va hayvonot dunyosining xilma-xilligini o'z ichiga oladi va ilmiy tadqiqotlar uchun muhim yo'nalish hisoblanadi. Bu erda 1952 yildan beri qushlar koloniyalari, dengiz sutemizuvchilar va geologiya bo'yicha uzoq muddatli tadqiqot dasturlari o'tkazib kelinmoqda. 30 ga yaqin imperator pingvinlarini ko'paytirish joylari orasida bu doimiy stantsiya yonida joylashgan yagona narsa. | M 3 (1995) | 66 ° 40′00 ″ S 140 ° 02′00 ″ E / 66.6667 ° S 140.0333 ° E | 0,37 km2 (0,14 kvadrat milya) | |
| ASPA-121 | Keyp Royds, Ross oroli | Keyp Royds Ross orolining g'arbiy qismida, McMurdo Sound, muzsiz erning qirg'oq bo'yida joylashgan. Erebus tog'ining pastki g'arbiy yon bag'irlarida, taxminan 8 km kenglikda. Hudud quruqlik va dengiz komponentlarini o'z ichiga oladi. Hudud ma'lum bo'lgan janubda joylashgan Adeli pingvin koloniyasini qo'llab-quvvatlaydi. Ushbu sayt penguen populyatsiyasini tiklash va davom etayotgan ilmiy dasturlarni himoya qilish uchun maxsus himoya qilingan. Koloniya yuqori ilmiy va ekologik ahamiyatga ega bo'lib qolmoqda va shu sababli, ayniqsa, Keyp Roydsga yaqin stantsiyalar va sayyohlik guruhlaridan doimiy tashriflarini hisobga olgan holda, uzoq muddatli maxsus himoyani davom ettirdi. | Rec VIII-4 | 77 ° 33′20 ″ S 166 ° 09′56 ″ E / 77.5556 ° S 166.1656 ° E | 0,62 km2 (0,24 kvadrat milya) | |
| ASPA-122 | Kelish balandliklari, Hut-Point yarimoroli, Ross oroli | Arrival Heights - Ross orolining janubi-sharqida, Xut Point yarim orolining janubi-sharqiy uchi yaqinidagi past tepaliklarning kichik diapazoni. Hut Point yarim orolini tog 'yon bag'irlaridan janubga cho'zilgan kraterlar chizig'i hosil qiladi. Erebus. Hudud tabiiy va elektromagnit jihatdan sokin joy bo'lib, atmosferaning yuqori qatlamlarini o'rganish dasturlari bilan bog'liq ma'lumotlarni yozib olish uchun sezgir asboblarni o'rnatish uchun ideal sharoitlarni taklif etadi. Bundan tashqari, saytning asl geografik xususiyatlari, masalan uning balandligi va shu bilan keng ko'lamli ufq, vulqon krateri morfologiyasi va yaqin atrofdagi McMurdo Station (AQSh) (janubdan 1,5 km va Skott bazasi (NZ)) ning to'liq logistika yordamiga yaqinligi. ) 3 km janubi-sharqda), yuqori atmosferani o'rganish va chegara qatlami havosidan namuna olish ishlari uchun ushbu maydonni qimmatli qilishda davom eting. | Rec VIII-4 | 77 ° 49′00 ″ S 166 ° 39′00 ″ E / 77.8167 ° S 166.65 ° E | 0,73 km2 (0,28 kvadrat milya) | |
| ASPA-123 | Barvik va Balxem vodiylari, Janubiy Viktoriya erlari | Barvik vodiysi janubiy Viktoriya Landining Ross dengizi sohilidan 65 km uzoqlikda joylashgan. Hududga Barvik va Balxem vodiylari va ularning tegishli suv havzalari kiradi. Bu joy ekologik jihatdan noyob va o'ta qutbli cho'l ekotizimiga ega bo'lgan Viktoriya Lendining quruq vodiylaridan eng kam bezovtalangan va ifloslangan joylardan biridir. Sayt ilmiy tadqiqotlar muntazam olib boriladigan boshqa quruq vodiylarning taqqoslanadigan ekotizimlaridagi o'zgarishlarni o'lchash uchun mos yozuvlar bazasi sifatida muhim ahamiyatga ega. | Rec VIII-4 | 77 ° 20′00 ″ S 161 ° 00′00 ″ E / 77.3333 ° S 161.0 ° E | 418,14 km2 (161,44 kvadrat milya) | |
| ASPA-124 | Crozier burni, Ross oroli | Krozye burni Ross orolining sharqiy qismida joylashgan bo'lib, u erda muzsiz hudud Terror tog'ining pastki sharqiy yon bag'irlarini o'z ichiga oladi. Ushbu hudud Post Office Hill tepaligida joylashgan bo'lib, qo'shni Ross muzli tokchasini qamrab olgan bo'lib, muzlik tokchasidagi katta yoriqlarni har yili naslchilik imperatori pingvinlari egallagan tez muz bilan qoplaydi. Bu hudud boy qushlar va sutemizuvchilar faunasini, shuningdek mikrofauna va mikroflorani qo'llab-quvvatlaydi va ekotizim juda qiziqqan dengiz va quruqlik elementlarining sezilarli darajada aralashishiga bog'liq. Imperator va Adélie pingvin koloniyalarining populyatsiyasi dinamikasi va ijtimoiy xulq-atvorini uzoq muddatli tadqiq qilishda himoya qilish mumkin; shuningdek, skua populyatsiyalari va o'simliklar to'plamlari. | Rec IV-6 | 77 ° 30′30 ″ S 169 ° 21′30 ″ E / 77.5083 ° S 169.3583 ° E | 72,21 km2 (27,88 kv. Mil) | |
| ASPA-125 | Fildes yarim oroli, King George Island (25 de Mayo) | Fildes yarim oroli - qirol Jorj orolida (25-may, May) yozda qorsiz eng keng qirg'oq bo'yi, uning uzunligi 7 km atrofida. Bu Antarktidadagi eng katta paleontologik qiziqish uyg'otadigan joylardan biri, chunki bu turli xil organizmlarning toshqotgan qoldiqlari, shu jumladan umurtqali va umurtqasizlar ichnitlari hamda barglar va po'stlar, magistrallar, polen donalari taassurotlari bilan mo'l-ko'l flora. Kechdan boshlab paydo bo'lgan sport turlari Bo'r uchun Eosen davr. | Rec IV-12 | 62 ° 12′00 ″ S 58 ° 58′00 ″ Vt / 62,2 ° S 58,9667 ° Vt | 2,34 km2 (0,90 kvadrat milya) | |
| ASPA-126 | Byers yarim oroli, Livingston oroli, Janubiy Shetland orollari | Byers yarim oroli Livingston orolining g'arbiy qismida joylashgan. Yura va bo'r davrining cho'kindi va toshbo'ron qatlamlari yarim orolidagi uchta kichik muzsiz joylarni himoya qilish uchun mo'ljallangan bo'lib, Antarktida va boshqa janubiy qit'alar o'rtasidagi avvalgi aloqani o'rganish uchun juda katta ilmiy ahamiyatga ega. Hudud, shuningdek, biologik va arxeologik ahamiyati bilan mashhur, ayniqsa muhim biota bo'lgan qirg'oq va ichki ko'llar mavjud. Ichki ko'llar suv moxlarini o'z ichiga oladi va Antarktidadagi yagona mahalliy qanotli hasharotlar Parochlus steinenii tog'ining ko'payishi uchun xizmat qiladi. Yarim orol ham tarixiy qiziqish uyg'otadi, Antarktidadagi 19-asrning tarixiy joylarining eng katta kontsentratsiyasini o'z ichiga oladi, masalan, qochqinlar qoldiqlari, zamonaviy asarlar va o'n to'qqizinchi asr boshidagi ekspeditsiyalar muhrlangan kemalar. | Rec IV-10 | 62 ° 34′35 ″ S 61 ° 13′07 ″ V / 62.5764 ° S 61.2186 ° Vt | 90,56 km2 (34,97 kvadrat milya) | |
| ASPA-127 | Xasuell oroli | Maydon Xesvell orolini (arxipelagdagi eng katta orol), uning qirg'oq zonasini va Devis dengizidagi tez muzning qo'shni qismini o'z ichiga olgan ko'pburchak bilan belgilanadi. Bu joy Sharqiy Antarktidadagi deyarli barcha naslchilik qush turlari, shu jumladan beshta petrel, skuaning bitta turi va pingvin uchun noyob va nihoyatda muhim naslchilik joyidir. Hudud shuningdek pinnipedlarning beshta turini, shu jumladan Rossiyaning maxsus himoyalangan turlari bo'lgan muhrni qo'llab-quvvatlaydi. Doimiy Antarktika stantsiyasi atrofida bir nechta imperator pingvin koloniyalaridan biriga ega va bu turni va yashash muhitini o'rganish uchun afzalliklar beradi. | Rec VIII-4 | 66 ° 31′00 ″ S 93 ° 00′00 ″ E / 66.5167 ° S 93.0 ° E | 5,01 km2 (1,93 kvadrat milya) | |
| ASPA-128 | Admiralt ko'rfazining g'arbiy qirg'og'i, King George Island, Janubiy Shetland orollari | Ushbu hudud Antarktida qushlari va sutemizuvchilarning Arktovskiy stantsiyasiga (Polsha) yaqinida turistik kemalar tez-tez tashrif buyuradigan ajoyib to'plamini qo'llab-quvvatlaydi. Hududning muhim maqsadi 1976 yildan buyon saytda olib borilayotgan uzoq muddatli tadqiqot dasturlarini, ayniqsa naslchilik davrida, tasodifiy buzilishlardan himoya qilishdir. | Rec X-5 | 62 ° 11′00 ″ S 58 ° 27′00 ″ Vt / 62.1833 ° S 58.45 ° Vt | 18,04 km2 (6,97 kvadrat milya) | |
| ASPA-129 | Rothera Point, Adelaida oroli | Rothera Point Ryder ko'rfazida, Antarktika yarim orolining Adelaida orolining sharq tomonida, Rayt yarim orolining janubi-sharqiy burchagida joylashgan. Sayt biologik tadqiqot maydonchasi va nazorat zonasi bo'lib xizmat qiladi, unga qarshi Rothera tadqiqot stantsiyasi (Buyuk Britaniya) bilan bog'liq bo'lgan inson ta'sirining ta'sirini Antarktida yomg'ir ekotizimida kuzatish mumkin. Hududning o'zi tabiiy tabiatni muhofaza qilish qiymatiga ega emas. Saytda janubiy qutbli skuas va suv o'tlari uyalar. | Rec XIII-8 | 67 ° 34′00 ″ S 68 ° 06′00 ″ Vt / 67.5667 ° S 68.1 ° Vt | 0,04 km2 (0,015 kv mil) | |
| ASPA-130 | 'Tramvay tizmasi ', Erebus tog'i, Ross oroli | Maydon 200 m dan 200,8 m gacha bo'lgan kvadrat bo'lib, quyi Tramvay tizmasining iliq er maydonining ko'p qismini o'z ichiga oladi. Hudud deyarli teng o'lchamdagi ikki qismga bo'lingan, shimoliy yarmi taqiqlangan zonadir. Erebus tog'i fumarol faolligi va Antarktidada bog'langan o'simliklarning ma'lum bo'lgan uchta baland balandlikdagi maydonlaridan birini ta'minlaydi. Issiq zamin va uning o'simliklari botaniklar, fiziologlar va mikrobiologlar uchun qiziqish uyg'otadi va ekologik tadqiqotlar uchun yo'nalish bo'lib xizmat qiladi. Hudud sezilarli darajada gaz chiqindilariga ega va uning tuprog'i Erebus tog'ida eng yuqori sirt haroratiga ega, bu esa vulkanologlarni ham qiziqtiradi. Jamiyatlarning mintaqaviy o'ziga xosligi katta ilmiy qiziqish va ahamiyatga ega. | Rec XIII-8 | 77 ° 31′00 ″ S 167 ° 07′00 ″ E / 77.5167 ° S 167.1167 ° E | 0,04 km2 (0,015 kv mil) | |
| ASPA-131 | Kanada muzligi, Friksell ko'li, Teylor vodiysi, Viktoriya Land | Viloyat janubiy Viktoriya quruq quruq vodiysidagi Teylor vodiysida joylashgan. U pastki Kanadadagi muzlikning sharqiy tomonidagi muzliklarning aksariyat qismini o'z ichiga oladi va yozgi suv havzalari va mayda erigan suv oqimlari bilan Kanada muzligidan Frayksell ko'liga oqib tushadigan qiya muzsiz erni o'z ichiga oladi. U janubiy Viktoriya quruqlik vodiysidagi eng boy o'simlik o'simtalarini (suv o'tlari va moxlarni) o'z ichiga oladi va boshqa quruq vodiy ekotizimlari uchun mos yozuvlar maydoni sifatida qimmatlidir. Ushbu hududdagi tadqiqot faoliyatining kontsentratsiyasi odamlarning oyoq osti qilish, suv sifati va namuna olish borasidagi ta'sirini tartibga solishni talab qiladi. | Rec XIII-8 | 77 ° 37′00 ″ S 163 ° 03′00 ″ E / 77.6167 ° S 163.05 ° E | 1,51 km2 (0,58 kvadrat milya) | |
| ASPA-132 | Potter yarim oroli, King George Island, (Isla 25 de Mayo ), Janubiy Shetland orollari | Bu hudud Maksvell ko'rfazining sharqiy qirg'og'ida, qirol Jorj orolining janubi-g'arbiy qismida, Mirounga punktining janubiy uchi (Potter yarim orolining shimoli-g'arbiy qismida) va shimoliy-sharqiy chegarada "Spur 7" nomi bilan tanilgan joy o'rtasida joylashgan. Stranger Point. Bu erda muhim qushlar koloniyalari, dengiz sutemizuvchilarni ko'paytirish joylari va turli xil o'simlik turlari mavjud. U Argentinaning Jubani bazasiga yaqin. Fil muhrlari va qushlarining naslchilik ekologiyasi bo'yicha uzoq muddatli tadqiqot dasturlari (1982 yildan buyon ushbu hududda olib borilmoqda), ayniqsa, naslchilik davrlarida tasodifiy bezovtalik tufayli xavf tug'dirishi mumkin. | Rec XIII-8 | 62 ° 15′S 58 ° 39′W / 62,25 ° S 58,65 ° V | 2,17 km2 (0,84 kvadrat milya) | |
| ASPA-133 | Harmony Point, Nelson oroli, Janubiy Shetland orollari | Ushbu hudud Nelson orolining g'arbiy qirg'og'ida, shimoliy-sharqda qirol Jorj oroli va janubi-g'arbiy qismida Robert orolining o'rtasida joylashgan. U Harmony Point, Toe, qo'shni muz va atrofdagi dengiz zonasini o'z ichiga oladi. Bu Antarktidadagi penguenlarning eng yirik yakka koloniyalaridan biri, shu jumladan dengiz qushlarining o'n bitta turidan iborat yirik naslchilik koloniyalariga ega bo'lgan parranda turlariga boy hudud. O'simliklar qoplami keng va u mox, liken va gulli o'simlik turlarini o'z ichiga olgan boy florani o'z ichiga oladi. | Rec XIII-8 | 62 ° 18′00 ″ S 59 ° 11′00 ″ V / 62,3 ° S 59,1833 ° V | 30,69 km2 (11,85 kv. Mil) | |
| ASPA-134 | Cierva-Point va dengizdagi orollar, Danco Coast, Antarktika yarim oroli | Cierva nuqtasi Cierva Kovining janubiy qirg'og'ida, Xuz ko'rfazining shimolida, Danco va Palmer sohillari o'rtasida, Antarktika yarim orolining shimoliy-g'arbiy qismida joylashgan. Bu erda parranda populyatsiyasi, keng o'simlik va antarktika gulli ikkita o'simlik, bir nechta jigar qurtlari va umurtqasiz hayvonlar dunyosi mavjud. Hududning noyob topografiyasi o'simliklarning ko'pligi va xilma-xilligi bilan birga ko'plab mikrohayotiy uylarning shakllanishi uchun juda qulay sharoitlar yaratadi, bu esa o'z navbatida bioxilma-xillikning rivojlanishini qo'llab-quvvatlaydi va hududga ajoyib estetik ahamiyat beradi. | Rec XIII-8 | 64 ° 10′00 ″ S 61 ° 01′00 ″ Vt / 64.1667 ° S 61.0167 ° Vt | 59,03 km2 (22,79 kvadrat milya) | |
| ASPA-135 | Shimoliy-Sharqiy Beyli yarim oroli, Budd sohili, Uilkes Land | Mintaqa Sharqiy Antarktidaning Uilks Lendidagi Budil sohilidagi Shamol tegirmoni orollaridagi Beyli yarimorolida joylashgan. Saytda qarama-qarshi yashash joylari va suv havzalari, o'ta boy liken va mox jamoalari va jigar qurtining muhim stendi mavjud. Yaqin atrofdagi Keysi stantsiyasiga (Avstraliya) yaqinlik dala tadqiqotlari uchun moddiy-texnika muammolarini minimallashtiradi va shu bilan birga, ushbu hududdagi tadqiqotlarning buzilishi (shu jumladan, 1980-yillarning boshlaridan o'simliklarning turli xil birikmalariga oid tadqiqotlar) uchun potentsialni maksimal darajada oshiradi. Bu birinchi navbatda saytni muhofaza qilishni talab qilishi sababli. | Rec XIII-8 | 66 ° 17′00 ″ S 110 ° 33′00 ″ E / 66.2833 ° S 110.55 ° E | 0,28 km2 (0,11 kv mil) | |
| ASPA-136 | Klark yarim oroli, Budd sohili, Uilkes Land | Klark yarim oroli - Uilkes quruqligidagi Budd sohilidagi Vinsennes ko'rfazining sharqiy qismida Nyukom ko'rfazining shimoliy qismida joylashgan toshlar ta'sir qiladigan maydon, doimiy muz va qor maydonlari. Golotsen deglyatsiyasidan beri dengizda shamol tegirmoni orollari maydonining paydo bo'lishining o'ziga xos va ko'rinadigan vaqt ketma-ketligini ta'minlaydi. Hududdagi ilmiy tadqiqotlar o'simlik jamoalari va Adeli pingvin koloniyalarining uzoq muddatli populyatsiyasini o'rganishga qaratilgan. Ushbu o'simlik va hayvonot dunyosini muhofaza qilish, odamlarning bezovtalanish darajasi yuqori bo'lgan Keysi Stantsiyasiga yaqin bo'lgan o'xshash o'simlik jamoalari va pingvin koloniyalarini taqqoslash imkonini beradi. | Rec XIII-8 | 66 ° 15′S 110 ° 36′E / 66,25 ° S 110,6 ° E | 9,38 km2 (3,62 kv mil) | |
| ASPA-137 | Shimoliy-G'arbiy Oq orol, McMurdo Sound | McMurdo vulqon kompleksining bir qismi bo'lgan White Island, McMurdo Ice Shelf qirg'og'idan taxminan 20 km janubi-sharqda va Hut Point-dan 25 km janubi-sharqda, Rossdagi McMurdo Station (AQSh) va Scott Base (NZ) joylashgan. Orol. Ushbu makonda McMurdo Ice Shelf va Ross Ice Shelf tomonidan ilgari surilganligi sababli boshqa populyatsiyalardan jismonan ajratilgan Weddell muhrlarining odatiy bo'lmagan naslchilik populyatsiyasi mavjud. Bu Ueddell muhrlari muzli tokcha ostida oziqlanadigan juda kam joylardan biridir. Bu, shuningdek, janubdagi Weddell muhr populyatsiyalaridan biridir va yil davomida o'rganilgan. Populyatsiya 60 yilga yaqin deb hisoblangan boshqa muhrlar bilan o'zaro aloqada bo'lishdan jismoniy izolyatsiya qilinganligi sababli alohida ilmiy ahamiyatga ega. Ushbu guruhni genetik jihatdan alohida populyatsiya deb hisoblash mumkinligi bo'yicha tekshiruvlar olib borilmoqda. | Rec XIII-8 | 78 ° 07′00 ″ S 167 ° 11′00 ″ E / 78.1167 ° S 167.1833 ° E | 141,61 km2 (54,68 kvadrat milya) | |
| ASPA-138 | Linnaeus teras, Asgard tizmasi, Viktoriya Land | Linnaeus Terrace - bu Asgard tizmasining g'arbiy qismida, Oliver cho'qqisidan 1,5 km shimolda joylashgan, taxminan 1600 metr balandlikda, taxminan 1,5 km uzunlikdagi va 1 km kenglikdagi buzilgan mayoq qumtoshining dastgohi. Sayt Beacon qumtoshini mustamlaka qiladigan noyob kriptoendolitik jamoalar uchun eng boy joylardan biridir. Qumtoshlarda bir qator biologik va fizikaviy ob-havo shakllari, shuningdek qoldiqlarning izlari aks etadi va ko'plab shakllanishlar mo'rt bo'lib, ularni oyoq osti qilish va tanlab olish natijasida buzilish va vayronagarchiliklar mavjud. | Rec XIII-8 | 77 ° 35′00 ″ S 161 ° 05′00 ″ E / 77.5833 ° S 161.0833 ° E | 0,78 km2 (0,30 kvadrat milya) | |
| ASPA-139 | Biscoe Point, Anvers oroli, Palmer arxipelagi | Biscoe Point Anvers orolining janubiy qirg'og'iga yaqin joylashgan, Palmer arxipelagi deb nomlanadigan Antarktida yarim orolining g'arbiy qismida joylashgan kichik orolning g'arbiy qismida joylashgan. Saytda Antarktidaning ikkita mahalliy qon tomir o'simliklari, Antarktidadagi tukli o'tlar va Antarktida marvaridining katta, ammo uzluksiz stendi mavjud. Nisbatan yaxshi rivojlangan loy o'tning yopiq qirralari ostida uchraydi va tarkibiga boy biota kiradi, jumladan Belgika Antarktida apterous tizmasi. Antarktika mo'ynali muhrlari tomonidan u hali sezilarli darajada zarar ko'rmagan, shuning uchun bu hudud Antarktika mo'yna muhrining ushbu mintaqadagi o'simliklar va tuproqlarga ta'sirini baholash uchun potentsial nazorat joyidir. Shuningdek, u ornitologik tadqiqotlar uchun ham qimmatlidir. Hududda joylashgan Adélie va gentoo pingvin koloniyalarida uzoq muddatli tadqiqotlar olib borilmoqda, ular yaqin Palmer stantsiyasi va sayyohlik kemalarining aralashuvi bilan xavf ostida qolishi mumkin. | Rec XIII-8 | 64 ° 48′00 ″ S 63 ° 47′00 ″ Vt / 64,8 ° S 63,7833 ° Vt | 0,6 km2 (0,23 kvadrat milya) | |
| ASPA-140 | Ning qismlari Aldama orol, Janubiy Shetland orollari | Deception Island is an active volcano located in the South Shetland Islands The area comprises 11 sub-sites, lettered A to L (but excluding I), in a clockwise direction from the south-west of the Deception Island caldera, and referred to by the most prominent named geographical feature associated with each site. Due to major volcanic eruptions in 1967, 1969 and 1970, the island offers unique opportunities to study colonization processes in Antarctic environments. The flora of the island is unique in Antarctic terms, particularly where associated with these geothermal areas, but also because of the recently formed surfaces which provide known-age habitats for the study of colonization and other dynamic ecological processes by terrestrial organisms. | Rec XIII-8 | 62°57′00″S 60 ° 38′00 ″ Vt / 62.95°S 60.6333°W | 2,57 km2 (0,99 kv. Mil) | |
| ASPA-141 | Yukidori vodiysi, Langhovde, Lyutsov-Xolm ko'rfazi | Yukidori Valley is situated in the middle part of Langhovde, on the east coast of Lützow-Holm Bay, Continental Antarctica. The area is representative of the typical Antarctic fellfield ecosystem. Permanent quadrats for monitoring lichen and moss vegetation have been established in this typical continental ecosystem to investigate long-term environmental change. Considering the increasing pedestrian traffic from the nearby Syowa Station (Japan) the aim is to keep human impacts on the ecosystem to a minimum and protect scientific research. | Rec XIV-5 | 69°14′30″S 39°46′00″E / 69.2417°S 39.7667°E | 4,88 km2 (1,88 kvadrat milya) | |
| ASPA-142 | Svarthamaren | The area consists of the ice free areas of the Svarthmaren nunatak, as part of the Mühlig-Hoffmanfjella in Dronning Maud Land, and the nunatak’s surrounding rocks and boulders. It holds the largest known inland seabird colony in Antarctica, with snow petrel, south polar skua, and the largest proportion of the known world population of Antarctic petrel. The colony is an exceptional “natural research laboratory” providing for research on these seabirds, and their adaptation to breeding in the inland/interior of Antarctica. | Rec XIV-5 | 71°54′40″S 5°11′00″E / 71.9111°S 5.1833°E | 6,49 km2 (2.51 sq mi) |  |
| ASPA-143 | Dengiz tekisligi, Xachir yarimoroli, Vestfold tepaliklari, Malika Elizabeth Land | Marine Plain lies approximately 10km south-east of Davis Station in the Vestfold Hills. The area possesses unique vertebrate fossil fauna and is of exceptional ongoing scientific interest because of its relevance to the palaeocological and palaeoclimatic record of Antarctica. The area has been subject to several detailed geological, palaeontological, geomorphologic and glaciological studies. Burton Lake, a hypersaline lagoon in seasonal connection with the marine environment to the west of the site, represents a unique stage in the biological and physico-chemical evolution of a terrestrial water body from the marine environment. | Rec XIV-5 | 68°37′50″S 78 ° 07′55 ″ E / 68.6306°S 78.1319°E | 20,46 km2 (7,90 kvadrat milya) | |
| ASPA-144 | 'Chile Bay ' (Discovery Bay ), Grinvich oroli, Janubiy Shetland orollari | The area comprises two small areas of benthic habitat in Chile Bay. It has been the location of continuous benthic research since 1967, following the volcanic eruption on Deception island. Data being accumulated provides a baseline for long-term scientific investigations. | Rec XIV-5 | 62°29′06″S 59 ° 41′27 ″ V / 62.485°S 59.6908°W | 0,66 km2 (0,25 kvadrat milya) | |
| ASPA-145 | Port-Foster, Aldama orol, Janubiy Shetland orollari | The area comprises two sub-areas in Port Foster, Deception Island: benthic habitat A, with depths of between 50 and 150m; and benthic habitat B, between 100 and 150 m deep. The area is of exceptional ecological interest because of its active volcanic character. It also has a diversity of benthic fauna on two different kinds of sea bottom substrates. These two habitat areas are subject to long-term research on the ecological process of recolonisation after volcanic eruption, and it is necessary to reduce the risk of accidental interference which could jeopardize these studies. | Rec XIV-5 | 62°55′51″S 60°37′30″W / 62.9308°S 60.625°W | 2,24 km2 (0,86 kvadrat milya) |  |
| ASPA-146 | Janubiy ko'rfaz, Dumer oroli, Palmer arxipelagi | Doumer Island lies at the south-west entrance to the Neumayer Channel. It is separated from Wiencke Island by the Peltier Channel. South Bay lies on the south coast of Doumer Island. The site consists of a small area of coastal and subtidal benthos down to 45 m depth. It is the subject of a long-term study on marine ecology, focused on the study of the relationships between the marine organisms in the area. | Rec XIV-5 | 64 ° 52′00 ″ S 63 ° 35′00 ″ Vt / 64.8667°S 63.5833°W | 0,96 km2 (0,37 kv mil) | |
| ASPA-147 | Ablasyon vodiysi Va Ganymed Heights, Aleksandr oroli | Ablation Valley – Ganymede Heights is situated on the east side of Alexander Island, the largest island off the western coast of Palmer Land, Antarctic Peninsula. The site is one of the largest ice-free ablation areas in West Antarctica, making it an area of outstanding scientific interest. The site contains the only known area of unbroken exposure of rocks spanning the Jurassic – Cretaceous boundary in the Antarctic. There is also an exceptional and unique contiguous geomorphologic record of glacier and ice-shelf fluctuations extending over several thousand years, together with an outstanding assemblage of other geomorphologic features. Two perennially frozen freshwater lakes, which have the unusual property of contact with the saline waters of George VI Sound, are also a site for research activity. The area also has the greatest bryophyte diversity of any site at this latitude in Antarctica. | Rec XV-6 | 70°50′00″S 68°30′00″W / 70.8333°S 68.5°W | 109.02 km2 (42.09 sq mi) | |
| ASPA-148 | Flora tog'i, Umid Bay, Antarktika yarim oroli | Mount Flora is situated on the south-eastern flank of Hope Bay, on the Antarctic Peninsula. The area contains rich fossil flora, which was among the first fossil floras discovered in Antarctica. It has played a significant stratigraphic role in deducing the geological history of the Antarctic Peninsula. The area requires protection because of its long history as a geological research site, and its easy accessibility makes it vulnerable to souvenir collectors. | Rec XV-6 | 63°25′00″S 57°01′00″W / 63.4167°S 57.0167°W | 0,35 km2 (0,14 kvadrat milya) | |
| ASPA-149 | Shiref burni va San-Telmo oroli, Livingston oroli, Janubiy Shetland orollari | Cape Shirreff is situated on the northern coast of Livingston Island, between Barclay Bay and Hero Bay. The Antarctic fur seal and penguin breeding colonies and krill fisheries within the foraging range of these species make this a critical site for ecosystem monitoring. A survey of the South Shetland Islands and the Antarctic Peninsula identified Cape Shirreff – San Telmo Island as the most suitable site to monitor Antarctic fur seal colonies that could be affected by fisheries around the South Shetland Islands. The fur seal colony itself is the largest in the Antarctic Peninsula region, and has undergone monitoring since 1965, making it one of the longest continuous Antarctic fur seal monitoring programmes. | Rec IV-11 | 62°27′30″S 60°47′17″W / 62.4583°S 60.7881°W | 9,74 km2 (3,76 kvadrat milya) | |
| ASPA-150 | Ardli oroli, Maksvell ko'rfazi, King George Island (25 de Mayo) | The area comprises most of the island, and is linked to King George Island (25 de Mayo) by an isthmus that remains submerged at high tide. The eastern part of the isthmus, that remains dry during high tide, is included in the area as it is part of the island. The island was designated as a protected area on account of the diverse assemblage of bird species that breed on it, and in order to allow a study of their ecology and the factors that affect their populations. It also possesses a developed and outstanding flora, with several species of lichens, mosses and vascular plants. | Rec XVI-2 | 62 ° 13′00 ″ S 58°54′00″W / 62.2167°S 58.9°W | 1,22 km2 (0,47 kvadrat milya) | |
| ASPA-151 | Sherlar Rump, King George Island, Janubiy Shetland orollari | Lions Rump is located on the southern coast of King George Bay, King George Island. The area is representative of the terrestrial, limnological and littoral habitats of the maritime Antarctic. There is rich lichen flora, and two native flowering plants. Twelve species of birds, including colonies of Adélie, chinstrap and gentoo penguins, nest within the area. There are large numbers of elephant seals and fur seals on the beaches. The area has had minimal disturbance from human activity, except for occasional monitoring studies of the mammal and bird populations, geological and geomorphologic studies, and should be protected against damaging activities. | Rec XVI-2 | 62°08′00″S 58°07′00″W / 62.1333°S 58.1167°W | 1,32 km2 (0,51 kvadrat milya) |  |
| ASPA-152 | Western Bransfield Strait | This marine ASPA lies off the western and southern coasts of Low Island, South Shetland Islands. The shallow shelf south of Low Island is one of only two known sites in the vicinity of Palmer Station that are suitable for bottom trawling for fish and other benthic organisms. From an ecological standpoint, the Low Island site offers unique opportunities to study the composition, structure, and dynamics of several accessible marine communities. The Site, and in particular, its benthic fauna, is of exceptional scientific interest and requires long-term protection from potential harmful interference. | Rec XVI-3 | 63°23′00″S 62°21′00″W / 63.3833°S 62.35°W | 915.8 km2 (353.6 sq mi) | [doimiy o'lik havola ] |
| ASPA-153 | Sharqiy Dallmann ko'rfazi | This marine ASPA lies off the western and northern coasts of Brabant Island, Palmer Archipelago, situated 65 km west of the Antarctic Peninsula, between Brabant and Anvers Islands, with Bransfield Strait to the north and Gerlache Strait to the south. It is one of only two known sites near Palmer Station that are suitable for bottom trawling for fish and other benthic organisms. The Site and, in particular, its benthic fauna, are of exceptional scientific interest and require long-term protection from harmful interference. | Rec XVI-3 | 64 ° 10′00 ″ S 62°50′00″W / 64.1667°S 62.8333°W | 609.54 km2 (235.34 sq mi) | |
| ASPA-154 | Botanika ko'rfazi, Burun geologiyasi, Viktoriya Land | Cape Geology is situated in the south-western corner of Granite Harbour, southern Victoria Land, approximately 100 km north-west of Ross Island. The site is an extremely rich botanical refuge for such a high latitude location, with a lichen and moss species diversity and abundance that is unique for Southern Victoria Land. There are also abundant growths of algae, large populations of invertebrates and a colony of south polar skua. The area also contains a managed zone, which contains the remains of a rock shelter and associated artefacts of historical importance from the 1910-1913 British Antarctic Expedition. | M 3 (1997) | 77°00′30″S 162°34′00″E / 77.0083°S 162.5667°E | 2,14 km2 (0,83 kvadrat milya) | [doimiy o'lik havola ] |
| ASPA-155 | Keyp Evans, Ross oroli | Cape Evans is a small, triangular shaped, ice-free area in the south west of Ross Island, 10km to the south of Cape Royds and 22km to the north of Hut Point Peninsula on Ross Island. The site is one of the principal sites of the Heroic Age of Antarctic exploration; it contains historic structures and relics pertaining to this era. Some of the earliest advances in Antarctic science are associated with the R.F. Scott Terra Nova Expedition, and as such, the site has considerable historical, cultural and scientific significance. It was subsequently used as a base by the Ross Sea party of Sir Ernest Shackleton’s Imperial Trans-Antarctic Expedition of 1914-1917. The site includes Terra Nova hut and numerous artefacts that are distributed around the site. | M 2 (1997) | 77°38′00″S 166°24′00″E / 77.6333°S 166.4°E | 0,06 km2 (0,023 kvadrat milya) | [doimiy o'lik havola ] |
| ASPA-156 | Lyuis Bey, Erebus tog'i, Ross oroli | The area was the site of an Air New Zealand aircraft crash on 28 November 1979 into the northern slope of Mount Erebus. The designated area encompasses the crash zone and the surrounding glacial ice 2 km above and to either side of this position. All two hundred and fifty seven people on board the aircraft lost their lives in the tragedy. The site of the tragedy was originally designated a tomb to be "left in peace". The stainless steel cross memorial, approximately 3 km from the site, is not part of the ASPA, but is Historic Monument 73. The area is to be kept protected as a mark of respect, in remembrance of the victims of the tragedy and in order to protect the site’s emotional values. | M 2 (1997) | 77°25′29″S 167°28′30″E / 77.4247°S 167.475°E | 14,41 km2 (5,56 kvadrat milya) | |
| ASPA-157 | Orqa eshik ko'rfazi, Keyp Royds, Ross oroli | Cape Royds is an ice free area at the western extremity of Ross Island, approximately 40km to the south of Cape Bird and 35km to the north of Hut Point Peninsula on Ross Island. The area is one of the principal sites of the Heroic Age of Antarctic exploration and it contains historic structures and relics pertaining to this era. Some of the earliest advances in the study of earth sciences, meteorology, flora and fauna in Antarctica are associated with the 1907-1909 British Antarctic (Nimrod) Expedition which was based at this site. The hut was also used again by the Ross Sea Party of the Imperial Trans-Antarctic Expedition of 1914-1917. As such, the site has high historical, cultural and scientific significance. Numerous additional artifacts are distributed around the area. | M 1 (1998) | 77°33′10″S 166°10′06″E / 77.5528°S 166.1683°E | 0,04 km2 (0,015 kv mil) | |
| ASPA-158 | Hut Point, Ross Island | Hut Point is a small ice free area protruding south west from the Hut Point Peninsula and situated to the west of the United States McMurdo Station. The designated area consists solely of the structure of the hut which is situated near the south western extremity of Hut Point. The hut is one of the principal sites of the Heroic Age of Antarctic exploration, being built during the National Antarctic (Discovery) Expedition in 1901-1904, and used again by other expeditions in 1907-1909, 1910-1913, and 1914-1917. Consequently, the site contains historic structures and relics pertaining to this era, with some of the earliest advances in Antarctic science are associated with the Discovery Expedition. | M 1 (1998) | 77°50′50″S 166°38′00″E / 77.8472°S 166.6333°E | Yo'q | |
| ASPA-159 | Keyp Adare, Borchgrevink qirg'og'i | Cape Adare is a generally ice free, prominent volcanic headland, at the northern extremity of Victoria Land. The area is located to the south west of the Cape on the southern shore of Ridley Beach. The area is an important symbol of the Heroic Age of Antarctic exploration and, as such, has considerable historical and cultural significance. Some of the earliest advances in Antarctic science are associated with the two earliest expeditions based at this site. There are three main structures in the area. Two were built in February 1899 by the British Antarctic Expedition led by Borchgrevink (1898-1900), and used for the first winter spent on the Antarctic continent. In 1911 Scott's British Antarctic Expedition (1910-13) Northern Party wintered at the third hut, situated 30m to the north of Borchgrevink's hut and built in February 1911. There are also numerous associated historical relics located in the area. | M 1 (1998) | 71 ° 18′S 170°09′E / 71.3°S 170.15°E | 0,03 km2 (0,012 kvadrat milya) |  |
| ASPA-160 | Frazier orollari, Shamol tegirmoni orollari, Uilkes Land, Sharqiy Antarktida | The Frazier Islands are three islands located in the eastern part of Vincennes Bay, approximately 16km to the west-north-west of Casey Station (Australia). The islands are one of only four known breeding colonies of southern giant petrels around the coastline of continental Antarctica, and it is the only breeding site in nearly 3000 km of coastline between Davis Station (Australia) and Dumont d’Urville (France). The site has been visited infrequently, typically only for seabird observations, and provides a reference area for future comparative studies with other breeding populations of southern giant petrels. | M 2 (2003) | 66°14′00″S 110°10′00″E / 66.2333°S 110.1667°E | 0,6 km2 (0,23 kvadrat milya) | |
| ASPA-161 | Terra-Nova ko'rfazi, Ross dengizi | The area is situated in Terra Nova Bay, between the Campbell Glacier Tongue and Drygalski Ice Tongue, Victoria Land. The region contains an important littoral area for well-established and long-term scientific investigations, with a high diversity at both species and community levels. The sponge and anthozoan communities at Terra Nova Bay showing a unique structure. , and the region is particularly vulnerable to disturbance by pollution, over-sampling and alien introductions. Extensive marine ecological research has been carried out at Terra Nova Bay since 1986/1987, revealing a high diversity at both the species and community levels, with the sponge and anthozoan communities at Terra Nova Bay showing a unique structure. The area is vulnerable to disturbance by pollution, over-sampling and alien introductions, and requires protection against direct human impacts. | M 2 (2003) | 74°45′00″S 164°10′00″E / 74.75°S 164.1667°E | 29,46 km2 (11,37 kvadrat milya) | |
| ASPA-162 | Mawson kulbalari, Cape Denison, Hamdo'stlik ko'rfazi, Jorj V Land, Sharqiy Antarktida | Cape Denison is a 1.5km-wide peninsula projecting into the centre of Commonwealth Bay, a 60km-wide stretch of coast in George V Land, East Antarctica. At the seaward end of this valley is Boat Harbour, a 400m long indentation in the coast. Mawson’s Main Hut is located about 65m from the harbor. This ASPA covers four sites, each consisting of one hut and extending 5m from the perimeter of the hut. The area includes the Main Hut, the Transit Hut, the Absolute Magnetic Hut, and the Magnetograph House. The area is to protect the historical, archaeological, technical, social and aesthetic values of Mawson's Huts, which served as the base for the Australasian Antarctic Expedition of 1911-1914, organised and led by geologist Dr Douglas Mawson. It is an important symbol for the ‘Historic Era’ of Antarctic Exploration. | M 2 (2004) | 67°00′30″S 142°39′40″E / 67.0083°S 142.6611°E | Yo'q | |
| ASPA-163 | Dakshin Gangotri muzligi, Mod Landni uchirish | Dakshin Gangotri Glacier is a small tongue of polar continental ice sheet, overriding the Schirmacher Oasis of central Dronning Maud Land.The site contains a small tongue of polar continental ice sheet, The glacier was identified by the second Indian Antarctic Expedition in 1983, and since then its snout has been monitored continuously. With the availability of this vast amount of data for the past two decades, it has become a valuable site for observing the changes in the movement of the Antarctic ice sheet under the impact of global warming. The area has primary scientific importance for glaciologists and environmental scientists. | M 2 (2005) | 70°45′15″S 11 ° 38′30 ″ E / 70.7542°S 11.6417°E | 4.31 km2 (1,66 kvadrat milya) | |
| ASPA-164 | Skullin va Myurrey monolitlari, Mac Robertson Land | Scullin Monolith and Murray Monolith are situated on the coast of Mac. Robertson Land approximately 160km east of Mawson Station (Australia). The area holds the greatest concentration of breeding seabird colonies in East Antarctica, and is rich in species diversity. Including. It is also the second largest colony for at least 160,000 pairs of Antarctic petrels, from a minimum estimated global total of approximately half a million pairs. Adélie penguin colonies also occupy the lower slopes of both monoliths, extending almost to the foreshore. The area possesses outstanding aesthetic values in the geomorphology of the two Monoliths and the spectacular nature of the glaciers descending from the Continental plateau that flow around the Monoliths ending in calving glaciers. | M 2 (2005) | 67°48′07″S 66°43′06″E / 67.8019°S 66.7183°E | 10,23 km2 (3,95 kvadrat milya) | |
| ASPA-165 | Edmonson punkti, Yog'och ko'rfaz, Ross dengizi | Edmonson Point is a coastal ice-free area of 1.79 km2 situated at Wood Bay, 50km north of Terra Nova Bay, and at the foot of Mount Melbourne (2732m), 13km east of the summit, in Victoria Land. The terrestrial and freshwater ecosystem is one of the most outstanding in northern Victoria Land. An exceptional diversity of freshwater habitats is present, with numerous streams, lakes, ponds and seepage areas, exhibiting nutrient conditions ranging from eutrophic to oligotrophic. The nature and diversity of the terrestrial and freshwater habitats offer outstanding scientific opportunities, This area is considered one of the best sites in Antarctica for studies of algal ecology. The scientific value of Edmonson Point is also considered exceptional for studies on the impact of climate change on terrestrial ecosystems. | M 1 (2006) | 74°20′00″S 165°08′00″E / 74.3333°S 165.1333°E | 5,5 km2 (2,1 kvadrat milya) | |
| ASPA-166 | Port-Martin, Adélie Land | The area is centered on a point which corresponds to the marker known as the “Astrolabe pillar”, located on the left hand side of the “refuge shelter” at Port Martin, Terre-Adélie. The site contains the remains of the main building (destroyed by fire in 1952) and several annexes build by members of successive French Antarctic expeditions between 1948 and 1952. Since then, only limited visits of a few hours have occurred, and with its short duration of operation, the remains of Port-Martin base are a perfect illustration of a base in Antarctica in the immediate post-war period. For future archaeology, the site represents an optimal site to design methods and techniques adapted to extreme archaeological investigation conditions. It is considered not only as a historical bridge site, but also as an original archaeological field. | M 1 (2006) | 66°49′00″S 141°23′00″E / 66.8167°S 141.3833°E | 0,17 km2 (0.066 sq mi) | |
| ASPA-167 | Hawker oroli, Vestfold tepaliklari, Ingrid Kristensen qirg'og'i, Malika Elizabeth Land, Sharqiy Antarktida | Hawker Island is located approximately 300m offshore from the Vestfold Hills, which is a roughly triangular ice-free area of approximately 512 km2 of bedrock, glacial debris, lakes and ponds. The area supports the southernmost breeding colony of southern giant petrels on continental Antarctica, alongside of Adélie penguins and a limited number of flying birds. The breeding population of southern giant petrels at the island decreased following its discovery in 1963, and human disturbance has been implicated in the observed decreases at all four southern giant petrel breeding sites on continental Antarctica. As an ASPA it completes the effort to safeguard all known southern giant petrel breeding locations in East Antarctica. | M 1 (2006) | 68°35′00″S 77 ° 50′00 ″ E / 68.5833°S 77.8333°E | 2,17 km2 (0,84 kvadrat milya) | |
| ASPA-168 | Harding tog'i, Grove tog'lari, Sharqiy Antarktida | The Grove Mountains are located approximately 400km inland (south) of the Larsemann Hills in Princess Elizabeth Land, East Antarctica. The area includes the open blue-ice zone from the moraine on the west side of Mount Harding to the east side of the Zakharoff Ridge; as well as a number of nunataks, a detritus zone and a moraine within it. The primary reason for designation of the site is to protect the unique geomorphologic features of the area for scientific research on the evolutionary history of East Antarctic Ice Sheet (EAIS). The remains of the fluctuation of ice sheet surface preserved around Mount Harding will most probably provide the precious direct evidences for reconstructing the EAIS behaviour. The site contains glacial erosion and wind-erosion physiognomies which are rare in nature and extremely vulnerable, such as the ice-core pyramid and the ventifact. These glacial-geological features have not only important scientific values, but also have rare wildness and aesthetic values. | M 2 (2008) | 72°54′00″S 75°02′30″E / 72.9°S 75.0417°E | 102.78 km2 (39,68 kv. Mil) | |
| ASPA-169 | Amanda Bay, Ingrid Kristensen qirg'og'i, Malika Elizabeth Land, Sharqiy Antarktida | Amanda Bay is located on the Ingrid Christensen Coast of Princess Elizabeth Land, East Antarctica. The area was designated to protect the breeding colony of several thousand pairs of emperor penguins annually resident in the south-west corner of Amanda Bay, while providing for continued collection of valuable long-term research and monitoring data and comparative studies with colonies elsewhere in East Antarctica. The accessibility of Amanda Bay is advantageous for research purposes, but also creates the potential for human disturbance of the birds. | M 3 (2008) | 69°15′00″S 76°49′59″E / 69.25°S 76.8331°E | 17,15 km2 (6,62 kvadrat mil) | |
| ASPA-170 | Marion Nunataks, Sharkot oroli, Antarktika yarim oroli | Charcot Island is roughly circular in shape, approximately 50km across and is separated from north-west Alexander Island by Wilkins Sound and Wilkins Ice shelf. It is ice-covered with the exception of Marion Nunataks, which form a 12 km chain of rock outcrops that overlook the mid-north coast of Charcot Island. The area was designated to protect its outstanding environmental values and to facilitate ongoing and planned scientific research. The nunataks have several unique characteristics including two lichens species that have not been recorded elsewhere in Antarctica, mosses that are rarely found at such southerly latitudes and, perhaps most significantly off all, a complete lack of predatory arthropods and Collembola which are common at all other equivalent sites within the biogeographical zone. | M 4 (2008) | 69 ° 45′S 75 ° 15′W / 69.75°S 75.25°W | 179.55 km2 (69.32 sq mi) | |
| ASPA-171 | Narebski Point, Barton yarim oroli, King George Island | Narebski Point is located on the southeast coast of Barton Peninsula, King George Island. The area is rich in flora and fauna, of which the abundance of some species is exceptional. The cover of mosses and lichens is very extensive. There are large numbers of chinstrap and gentoo penguins and the breeding areas of seven other birds including the nests of the southern giant petrel. The high diversity in relief and coastal forms, due to the presence of different geologies and a prominent system of fractures, in addition to an extensive and varied vegetation cover, provides unusual scenic diversity in the Antarctic environment. | M 13 (2009) | 62°14′03″S 58°46′05″W / 62.2342°S 58.7681°W | 0,89 km2 (0,34 kvadrat milya) | |
| ASPA-172 | Pastroq Teylor muzligi va Qon tushishi, Teylor vodiysi, McMurdo quruq vodiylari, Viktoriya Land | Blood Falls is an iron-rich saline discharge located at the terminus of the Taylor Glacier, Taylor Valley, McMurdo Dry Valleys. The source of the discharge is believed to be a subglacial marine salt deposit and brine reservoir located beneath the ablation zone of the Taylor Glacier, estimated to be located between one to six kilometres above Blood Falls. The primary reasons for designation of the area are its unique physical properties, and the unusual microbial ecology and geochemistry. The area is an important site for exobiological studies and provides a unique opportunity to sample the subglacial environment without direct contact. The influence of Blood Falls on adjacent Lake Bonney is also of significant scientific interest. Furthermore, the ablation zone of the Taylor Glacier is an important site for paleoclimatic and glaciological research. The lower Taylor Glacier subglacial brine reservoir and Blood Falls are globally unique and a site of outstanding scientific importance. | M 9 (2012) | 77°50′13″S 161°40′14″E / 77.8369°S 161.6706°E | 436 km2 (168 kvadrat milya) | |
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- ^ "Arxivlangan nusxa". Arxivlandi asl nusxasi 2009-06-29. Olingan 2010-02-06.CS1 maint: nom sifatida arxivlangan nusxa (havola)
- ^ "Arxivlangan nusxa". Arxivlandi asl nusxasi 2009-06-29. Olingan 2010-02-06.CS1 maint: nom sifatida arxivlangan nusxa (havola)
Tashqi havolalar
- Official List of ASPA sites
- ats.aq: The Official Guide to the Preparation of Management Plans for Antarctic Specially Protected Areas
- Government of Japan - efforts to protect Antarctica in Japan
- US State Department - Proposed Re-numbering of Antarctic Specially Protected Areas
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