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The Drygalski Ice Tongue or Drygalski Barrier or Drygalski Glacier Tongue is a glacier in Antarctica, on the Scott Coast, in the northern McMurdo Sound of Antarctica's Ross Dependency, 240 kilometres (150 mi) north of Ross Island. The Drygalski Ice Tongue is stable by the standards of Antarctica's icefloes, and stretches 70 kilometres (43 mi) out to sea from the David Glacier, reaching the sea from a valley in the Prince Albert Mountains of Victoria Land. The Drygalski Ice Tongue ranges from 14 to 24 kilometres wide.
Pine Island Glacier (PIG) is a large ice stream, and the fastest melting glacier in Antarctica, responsible for about 25% of Antarctica's ice loss. The glacier ice streams flow west-northwest along the south side of the Hudson Mountains into Pine Island Bay, Amundsen Sea, Antarctica. It was mapped by the United States Geological Survey (USGS) from surveys and United States Navy (USN) air photos, 1960–66, and named by the Advisory Committee on Antarctic Names (US-ACAN) in association with Pine Island Bay.
Devosia glacialis is a psychrophilic Gram-negative, aerobic, motile bacteria from the genus of Devosia with a polar flagella which was isolated from a glacier in the Hohe Tauern in Austria.
Devosia psychrophila is a psychrophilic, aerobic, Gram-negative, rod-shaped bacteria from the genus of Devosia which was isolated from the Pitztaler Jöchl glacier in the Oetztaler Alps in Tyrol in Austria.
Massilia yuzhufengensis is a Gram-negative, rod-shaped, aerobic and motile bacterium from the genus Massilia with a polar flagella which has been isolated from the Yuzhufeng Glacier from the Tibetan Plateau in China.
Sphingomonas psychrolutea is a Gram-negative, rod-shaped, aerobic and psychrotolerant bacteria from the genus of Sphingomonas which has been isolated from the Midui glacier in Tibet in China.
Anseongella is a genus from the family of Sphingobacteriaceae.
Arcticibacter eurypsychrophilus is a Gram-negative and rod-shaped bacterium from the genus of Arcticibacter which has been isolated from the ice core of the Muji Glacier.
Arcticibacter svalbardensis is a Gram-negative, rod-shaped and non-motile bacterium from the genus of Arcticibacter which has been isolated from surface soil from Ny-Ålesund on Svalbard.
Chelatococcus reniformis is a Gram-negative and non-motile bacterium from the genus of Chelatococcus which has been isolated from the Muztagh Glacier on the Tibetan Plateau in China.
Hymenobacter glacieicola is a Gram-negative, rod-shaped and non-motile bacterium from the genus of Hymenobacter which has been isolated from glacier ice from the Muztagh Glacier from the Tibetan Plateau in China.
Arthrobacter ruber is a Gram-positive bacterium from the genus of Arthrobacter has been isolated from ice from the Midui glacier from Tibet in China.
Aurantiacibacter arachoides is a Gram-negative and rod-shaped bacteria from the genus Aurantiacibacter which has been isolated from the ice core of the East Rongbuk Glacier from the Tibetan Plateau.
Hymenobacter frigidus is a Gram-negative, psychrophilic and rod-shaped bacterium from the genus of Hymenobacter which has been isolated from the ice core of the Muztagh Glacier from the Tibetan Plateau.
Aureimonas glaciei is a Gram-negative, aerobic, short rod-shaped and motile bacteria from the genus of Aurantimonas which has been isolated from the Muztagh Glacier in China.
Cryobacterium flavum is a Gram-positive and rod-shaped bacterium from the genus of Cryobacterium which has been isolated from glacier ice from Xinjiang in China.
Cryobacterium levicorallinum is a psychrophilic and Gram-positive bacterium from the genus of Cryobacterium which has been isolated from glacier ice from Xinjiang in China.
Cryobacterium luteum is a Gram-positive and rod-shaped bacterium from the genus of Cryobacterium which has been isolated from glacier ice from a glacier from the Xinjiang Uyghur Autonomous Region in China.
Mycetocola miduiensis is a Gram-positive, aerobic, psychrotolerant and non-spore-forming bacterium from the genus of Mycetocola which has been isolated from soil from the Midui glacier from the Tibet Province.
The Quelccaya Ice Cap is the second largest glaciated area in the tropics, after Coropuna. Located in the Cordillera Oriental section of the Andes mountains in Peru, the cap covers an area of 42.8 square kilometres (16.5 sq mi) with ice up to 200 metres (660 ft) thick. It is surrounded by tall ice cliffs and a number of outlet glaciers, the largest of which is known as Qori Kalis Glacier; lakes, moraines, peat bogs and wetlands are also present. There is a rich flora and fauna, including birds that nest on the ice cap. Quelccaya is an important source of water, eventually melting and flowing into the Inambari and Vilcanota Rivers.
References
- 1 2 Parte, A.C. "Arcticibacter". LPSN .
- 1 2 "Arcticibacter pallidicorallinus". www.uniprot.org.
- ↑ Liu, Q.; Kim, S.-g.; Liu, H.-c.; Xin, Y.-h.; Zhou, Y.-g. (7 April 2014). "Arcticibacter pallidicorallinus sp. nov. isolated from glacier ice". International Journal of Systematic and Evolutionary Microbiology. 64 (Pt 7): 2229–2232. doi: 10.1099/ijs.0.061754-0 . PMID 24711590.