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Lake Bonney (77°43′S 162°22′E ) is a saline lake with permanent ice cover at the western end of Taylor Valley in the McMurdo Dry Valleys of Victoria Land, Antarctica.

Lake Bonney
Taylor Glacier at the lake
Lake Bonney
Location	Taylor Valley, Victoria Land, Antarctica
Coordinates	77°44′S 162°10′E
Type	saline, Endorheic
Primary inflows	Doran Stream/Priscu Stream, others
Primary outflows	none
Basin countries	(Antarctica)
Max. length	7 km (4.3 mi)
Max. width	0.9 km (0.56 mi)
Surface area	4.3 km2 (1.7 sq mi)
Average depth	15 m (49 ft)
Max. depth	40 m (130 ft)
Water volume	64,800,000 m3 (2.29×109 cu ft)
Surface elevation	57 m (187 ft)
Frozen	2.8 to 4.5 m (9.2 to 14.8 ft)
Settlements	Lake Bonney Hut

It is 7 kilometres (4.3 mi) long and up to 900 metres (3,000 ft) wide. A narrow channel only 50 metres (160 ft) wide (Lake Bonney at Narrows) separates the lake into East Lake Bonney (3.32 square kilometres [1.28 sq mi]) and West Lake Bonney (0.99 square kilometres [0.38 sq mi]).

To the north and south of the lake lie peaks that are over 1,500 metres (4,900 ft) above sea level, and the Taylor Glacier is positioned to the west of the lake. It is 130 feet (40 m) deep and is perpetually trapped under 12 to 15 feet (3.7 to 4.6 m) of ice.

It was first visited by the British Antarctic Expedition of 1901-1904. It was named by the Scott expedition of 1910-1913, for Thomas George Bonney, professor of geology at University College London, England from 1877 to 1901.

Lake Bonney is one of the main lakes studied by the National Science Foundations, McMurdo Long Term Ecological Research site.

Starting in 2007 NASA is funding an autonomous submersible robot called ENDURANCE to explore the water volume of the lake to study its shape and ecology. The robot is built by Stone Aerospace who also developed the DEPTHX submersible. The Endurance Project is led by Peter Doran with Bill Stone and John Priscu among the co-investigators. Scientists have discovered an ancient ecosystem beneath the Taylor Glacier, next to Lake Bonney. This ecosystem survives by transforming sulfur and iron compounds for growth.[1]

The work is seen as a stage in developing an autonomous submersible robot that could explore the ocean on Jupiter's moon Europa.

Tributaries

Lake Bonney is fed by a number of meltwater streams:[2]

• Bartlette Creek
• Bohner Stream
• Doran Stream (feeding Priscu Stream)
• Lawson Creek
• Lizotte Creek
• Lyons Creek
• Mason Creek
• Priscu Stream (the longest, 3.8 km)
• Red River
• Santa Fe Stream
• Sharp Creek
• Vincent Creek

See also

• Blood Falls, an outflow of the tip of the Taylor Glacier containing an iron oxide tainted plume of melting salty water flowing onto the ice-covered surface of Lake Bonney.
• Lake Washburn (Antarctica), a precursor lake

Further reading

• Johanna Laybourn-Parry, Jemma L. Wadham, Antarctic Lakes, P 120
• Peter T. Doran, W. Berry Lyons, Diane M. McKnight, editors Life in Antarctic Deserts and other Cold Dry Environments: Astrobiological Analogs, P 164
• Obryk, M. K., P. T. Doran, and J. C. Priscu (2014), The permanent ice cover of Lake Bonney, Antarctica: The influence of thickness and sediment distribution on photosynthetically available radiation and chlorophyll‐a distribution in the underlying water column, J. Geophys. Res. Biogeosci., 119, 1879–1891, doi: 10.1002/2014JG002672
• Chao Tang, Michael T. Madigan, and Brian Lanoil, Bacterial and Archaeal Diversity in Sediments of West Lake Bonney, McMurdo Dry Valleys, Antarctica, Appl Environ Microbiol. 2013 Feb; 79(3): 1034–1038. doi: 10.1128/AEM.02336-12
• H.A. DUGAN, M.K. OBRYK, P.T. DORAN, Lake ice ablation rates from permanently ice-covered Antarctic lakes, Journal of Glaciology, Vol. 59, No. 215, 2013 doi:10.3189/2013JoG12J080, P 491
• Gideon M. Henderson, Brenda L. Hall, Andrew Smith, Laura F. Robinson, Control on (²³⁴U/ ²³⁸U) in lake water: A study in the Dry Valleys of Antarctica, Chemical Geology 226 (2006) 298 – 308
• Tessa Pocock and Marc-André Lachance, Thomas Pröschold, John C. Priscu, Sam Sulgi Kim, Norman P. A. Huner, IDENTIFICATION OF A PSYCHROPHILIC GREEN ALGA FROM LAKE BONNEY ANTARCTICA: CHLAMYDOMONAS RAUDENSIS ETTL. (UWO 241) CHLOROPHYCEAE, J. Phycol. 40, 1138–1148 (2004), doi: 10.1111/j.1529-8817.2004.04060.x
• Ernest E. Angino Kenneth B. Armitage Jerry C. Tash, PHYSICOCHEMICAL LIMNOLOGY OF LAKE BONNEY, ANTARCTICA, doi: 10.4319/lo.1964.9.2.0207

References

• U.S. Geological Survey Geographic Names Information System: Lake Bonney (Antarctica) U.S. Geological Survey, Geographic Names Information System. Accessed January 2008
• Lachance; et al. (2004). "Identification of a Psychrophilic Green Alga from Lake Bonney Antarctica: Chlamydomonas Raudensis Ettl. (UWO 241) Chlorophyceae1" (PDF). J. Phycol. Phycological Society of America. 40 (6): 1138–48. doi:10.1111/j.1529-8817.2004.04060.x. S2CID 44209250. Archived from the original (PDF) on 2007-07-13. Retrieved 2008-01-02.
• Space Daily April 22, 2007. Accessed January 2008

External links

• Lake data
• Satellite map
• Lake Bonney panoramic picture

External image
Taylor Valley and saline Lake Bonney(One of the McMurdo Dry Valleys -a true polar desert with small 'alpine' glaciers. (Photo: © M.J. Hambrey)

На других языках

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[de] Bonneysee

Der Bonneysee ist ein Salzsee mit einer permanenten Eisdecke am westlichen Ende des Taylor Valley in Victorialand, Antarktis.

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- [en] Lake Bonney (Antarctica)

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[it] Lago Bonney

Il lago Bonney è un lago glaciale ipersalino situato nella parte occidentale della valle di Taylor, una delle tre valli principali dell'Area Antartica Specialmente Gestita delle valli secche McMurdo, un'area di circa 15000 km² situata nella regione centro occidentale della Dipendenza di Ross, nell'Antartide orientale.[1]

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[ru] Бонни (озеро, Антарктида)

Бонни (Бонней[1], англ. Lake Bonney) — бессточное подлёдное солёное озеро в Антарктиде, в западной оконечности долины Тейлор[en] под поверхностью Сухих долин Мак-Мердо[2] на Земле Виктории[1] к западу от пролива Мак-Мердо. Покрыто круглый год постоянной ледяной шапкой мощностью около 4 м и питается ледниковыми водами. Общая минерализация воды в озере вертикально распределена на три слоя. Температура воды в покрытом льдом озере Бонни составляет максимум 7,5 °C на глубине 13 м и минимум −2,5 °C на дне на глубине 32 м. Концентрация растворённой соли увеличивается с глубиной[3] — солёная вода оказывается около дна, пресная — у поверхности. Имеет необычно соленую консистенцию. Тип вод — хлор-кальциевый.

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