New Siberian Islands

History

The first news about the existence of the New Siberian Islands was brought by a Cossack, Yakov Permyakov, in the beginning of the 18th century. In 1712, a Cossack unit led by M. Vagin reached the Great Lyakhovsky Island.

In 1809–10 Yakov Sannikov and Matvei Gedenschtrom went to the New Siberian Islands on a cartographic expedition. Sannikov reported the sighting of a "new land" north of Kotelny in 1811. This became the myth of Zemlya Sannikova or Sannikov Land. In 1886, Russian polar explorer and scientist Eduard Toll, during his first visit to the New Siberian Islands, thought that he had seen an unknown land north of Kotelny Island. He guessed that this was the so-called Zemlya Sannikova.

Toll paid a further visit to the island group in early 1892, accompanied by one Cossack and three natives. He traveled over the ice in sleds drawn by dogs and reached the south coast of Great Lyakhovsky Island.

In September 2014, the Russian Navy re-established a Soviet era naval base on Kotelny Island which had lain abandoned since 1993.

Geography

The New Siberian Islands proper, or Anzhu Islands (острова Анжу, Sakha: Анжу арыылара), covering a land area of about 29,000 km, consist of:

• Kotelny Island (о. Коте́льный) 11,700 km and
  • Faddeyevsky Island (о. Фадде́евский) 5,300 km. Bunge Land (земля́ Бу́нге) 6,200 km (occasionally submerged by sea) links Kotelny Island and Faddeyevsky Island. Very close to Bunge Land's northwestern coast lie two smaller islands:
    • Zheleznyakov Island (Ostrov Zheleznyakova), right off the NW cape and east of it, Matar Island (Ostrov Matar). Both islands have a length of about 5 km.
• Nanosnyy Island is a small island located due north off the northern bay formed by Kotelny and Bunge. It is C-shaped and only 4 km in length, but its geographical importance lies in the fact that it is the northernmost island of the New Siberian group.
• Novaya Sibir (о. Но́вая Сиби́рь) 6,200 km
• Belkovsky Island (о. Бельковский) 500 km

To the south and nearer to the Siberian mainland lie the Lyakhovskiye Islands (6,095 km):

• Great Lyakhovsky Island (о. Большо́й Ля́ховский) 4,600 km
• Little Lyakhovsky Island (о. Ма́лый Ля́ховский) 1,325 km
• Stolbovoy Island (о. Столбово́й) 170 km
• Semyonovsky Island (о. Семёновский) 0 km (now submerged)

The small De Long Islands (228 km) lie to the north-east of Novaya Sibir.

• Jeannette Island (о. Жанне́тты)
• Henrietta Island (о. Генрие́тты)
• Bennett Island (о. Бе́ннетта)
• Vilkitsky Island (о. Вильки́цкого)
• Zhokhov Island (о. Жо́хова)

The New Siberian Islands are low-lying. Their highest point is located on Bennett island, with an elevation of 426 m. They are part of the East Siberian Lowland, forming a geographical continuum with the continental plains further south.

The New Siberian Islands once formed major hills within the Great Arctic Plain that covered the northern part of Late Pleistocene "Beringia" between Siberia and Alaska during the Last Glacial Maximum (Late Weichselian Epoc). These islands represent the remains of about 1.6 million square kilometers of the formerly subaerial Great Arctic Plain that now lies submerged below parts of the Arctic Ocean, East Siberian Sea, and Laptev Sea. At this plain's greatest extent, sea level was 100–120 m below modern sea-level and the coastline lay 700 to 1000 kilometers north of its current position. This plain did not undergo extensive glaciation during the Late Pleistocene or the Last Glacial Maximum because it lay in the rain shadow of the Northern European ice sheet. During the frigid polar climate of the Last Glacial Maximum, 17,000 to 24,000 BC, small passive ice caps formed on the adjacent De Long Islands. Fragments of these ice caps remain on Jeannette, Henrietta, and Bennett Islands. Traces of former small slope and cirque glaciers in the form of buried ground ice deposits are preserved on Zhokhov Island. The sea submerged the Great Arctic Plain (except for the New Siberian and other isolated islands) within a relatively short time span of 7,000 years during the Early–Middle Holocene.Alekseev, M. N., 1997, Paleogeography and geochronology in the Russian eastern Arctic during the second half of the Quaternary. Quaternary International. vol. 41–42, pp. 11–15. M. A. Anisimov and V. E. Tumskoy, 2002, Environmental History of the Novosibirskie Islands for the last 12 ka. 32nd International Arctic Workshop, Program and Abstracts 2002. Institute of Arctic and Alpine Research, University of Colorado at Boulder, pp 23–25. L. Schirrmeister, H.-W. Hubberten, V. Rachold, and V.G. Grosse, 2005, Lost world: Late Quaternary environment of periglacial Arctic shelves and coastal lowlands in NE-Siberia. 2nd International Alfred Wegener Symposium Bremerhaven, October 30 – November 2, 2005.

Geology

As noted by Digby and numerous later publications, this archipelago consists of a mixture of folded and faulted sedimentary and igneous rocks ranging in age from Precambrian to Pliocene. The Lyakhovsky Islands consist of a folded and faulted assemblage of Precambrian metamorphic rocks; upper Paleozoic to Triassic sandstones and shales; Jurassic to lower Cretaceous turbidites; Cretaceous granites; and ophiolites. The Anzhu Islands consist of a highly faulted and folded assemblage of Ordovician to Devonian limestones, dolomites, sandstones, shales, volcanoclastic strata, and igneous rocks; upper Paleozoic to Triassic sandstones and shales; Jurassic to lower Cretaceous turbidites; and upper Cretaceous to Pliocene sandstones and shales. The De Long Islands consist of early Paleozoic, middle Paleozoic, Cretaceous, and Neogene sedimentary and igneous (mostly basalt) rocks. These sedimentary, metamorphic, and igneous rocks are mantled by loose Pleistocene and Holocene sediments that range in thickness from a fraction of a meter to about 35 m.

Digby who had never visited the New Siberian Islands and relied upon anecdotes of traders and travelers and local folklore for their descriptions of them, and other articles were written by explorers and ivory hunters untrained in either geology or other sciences. Such statements have been shown to be fictional in nature by detailed studies of the geology of the New Siberian Islands by professional geologists, paleontologists, and other scientists.

Ivory deposits

As noted by Baron Eduard V. Toll in his account of the New Siberian Islands, sizeable and economically significant accumulations of fossil ivory occur within them. The ivory, along with mammoth and other bones, are found in recent beaches, drainage areas, river terraces and river beds. The New Siberian Islands are unique in the burial and preservation of fossil ivory "in such a wonderful state of preservation that the tusks so found cannot be distinguished from the very best and purest ivory".

The abundant bones, even skeletons, of mammoth, rhinoceros, musk-ox, and other megafauna along with the mammoth ivory found in these islands are preserved by permafrost, in which they are encased. The permafrost periodically developed in Late Pleistocene loess, solifluction, pond, and stream sediments as they accumulated. The radiocarbon dating of bones, ivory, and plants, optically stimulated luminescence dating of enclosing sediments, and uranium-thorium dating of associated peats demonstrate that they accumulated over a period of some 200,000 years. Radiocarbon dates obtained from the collagen of 87 mammoth tusks and bones collected from Faddeevsky, Kotelniy, and New Siberia islands ranged from 9470±40 BP to greater than 50,000 BP (14C).

Important Bird Area

The entire archipelago has been designated an Important Bird Area (IBA) by BirdLife International because it supports breeding populations of many species of birds.

Climate

The climate is polar (Köppen ET) and severe. Snow cover is present for 9 months of the year.

• Average temperature in January: −28 to
• Temperature in July: At the coasts icy Arctic water keeps the temperatures relatively low. Average maximum temperatures here are from 8 to and average minimum temperatures from −3 to. In the interior of the islands the average maximum temperatures in July are 16 to and average minimum temperatures 3 to.
• Precipitation: up to 132 mm a year

Continuous permafrost rich in underground ice covers the archipelago. The surface of the islands is covered with Arctic tundra vegetation and numerous lakes.

The ocean surrounding the islands is covered with ice most of the year. During warm years, the ocean briefly opens for navigation July through October. During cold years, islands may remain ice-locked through the summer.

Polar night conditions are present November through February, and, conversely, the sun remains above the horizon continuously during summer months.

|Jan record high C = -7.2 |Feb record high C = -3.3 |Mar record high C = -4.8 |Apr record high C = 0.3 |May record high C = 6.2 |Jun record high C = 22.7 |Jul record high C = 25.1 |Aug record high C = 20.2 |Sep record high C = 11.8 |Oct record high C = 1.8 |Nov record high C = -2.5 |Dec record high C = -3.1 |year record high C = 25.1 |Jan record low C = -44.9 |Feb record low C = -49.9 |Mar record low C = -46.1 |Apr record low C = -46.2 |May record low C = -28.6 |Jun record low C = -14.9 |Jul record low C = -6.0 |Aug record low C = -9.2 |Sep record low C = -18.6 |Oct record low C = -40.2 |Nov record low C = -40.2 |Dec record low C = -45.0 |year record low C = -49.9 | access-date = 27 February 2016}} | access-date = 27 February 2016}}

Photo gallery

File:Kotelny-Insel 1 2014-08-24.jpg|Weatherstation on Kotelny Island (Anzhu Islands; 74° 38′ N, 139° 10′ E) File:Belkowski-Insel 1 2014-08-24.jpg|Belkovsky Island, Thilo Bay (Anzhu Islands; 75° 35′ 30″ N, 135° 38′ 44″ E) File:Belkowski-Insel 2 2014-08-24.jpg|Belkovsky Island (Anzhu Islands; 75° 35′ 30″ N, 135° 38′ 44″ E) File:Belkowski-Insel 3 2014-08-24.jpg|Belkovsky Island (Anzhu Islands; 75° 35′ 30″ N, 135° 38′ 44″ E) File:Strichowa-Insel 1 2014-08-24.jpg|Strizhov Island, a small rock island at southwest tip of Belkovsky Island (75° 18′ 40″ N, 135° 28′ 52″ E) File:Bennett-Insel 1 2014-08-25.jpg|Bennett Island (De Long Islands) between Cape Sophia and Cape Emmelin (76° 41′ 37″ N, 149° 20′ E) File:Bennett-Insel 2 2014-08-25.jpg|Bennett Island – M/S Hanseatic anchoring in the roads at the north coast File:Bennett-Insel 3 2014-08-25.jpg|Bennett Island, north coast – tundra landscape (76° 44′ 30″ N, 149° 21′ 19″ E) File:Bennett-Insel 4 2014-08-25.jpg|Bennett Island, north coast – tundra landscape File:Kigilyakh Peninsula of Bolshoy Lyakhovsky Island 2010-09-28.jpg|Bolshoy Lyakhovsky Island, view of the Kigilyakh Peninsula

References

• Locations

References

1. Markham, Albert Hastings ''Arctic Exploration'', 1895
2. Along the southern coast of this island he found well-preserved bones, ivory, peat, wood, and even a tree within {{convert. 40. m. ft
3. Schirrmeister, L., 2002, ''230Th/U Dating of Frozen Peat, Bol’shoy LyakhovskyIsland (Northern Siberia)''. Quaternary Research, vol. 57, pp. 253–258
4. "Russia dispatches naval force to reopen Arctic base". [[Daily Telegraph]].
5. Atle Staalesen. (September 17, 2013). "In remotest Russian Arctic, a new Navy base". Barents Observer.
6. Oleg Leonidovič Kryžanovskij, ''A Checklist of the Ground-beetles of Russia and Adjacent Lands.'' p. 16
7. Digby, B., 1926, ''The Mammoth and Mammoth-Hunting in North-East Siberia.'' D. Appleton and Company: New York, 224 pp.
8. V. K. Dorofeev, M. G. Blagoveshchensky, A. N. Smirnov, and V. I. Ushakov, 1999, ''New Siberian Islands. Geological structure and metallogeny''. VNIIOkeangeologia, St. Petersburg, Russia. 130 pp. (in Russian)
9. M. K. Kos'ko and G. V. Trufanov, 2002, [https://www.sciencedirect.com/science/article/pii/S0264817202000570 "Middle Cretaceous to Eopleistocene Sequences on the New Siberian Islands: an approach to interpret offshore seismic"]. ''[[Marine and Petroleum Geology]]''. vol. 19, no. 7, pp. 901–919.
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12. von Toll, Baron E., 1895, ''Wissenschaftliche Resultate der von der Kaiserlichen Akademie der Wissenschaften zur Erforschung des Janalandes und der Neusibirischen Inseln in den Jahren 1885 und 1886 ausgesandten Expedition.'' [''Scientific results of the expedition launched in the years 1885 and 1886 by the Imperial Academy of Sciences for the Investigation of Janaland and the New Siberian Islands'']. Abtheilung III: Die fossilen Eislager und ihre Beziehungen su den Mammuthleichen. Memoires de L'Academie imperials des Sciences de St. Petersbourg, VII Serie, Tome XLII, No. 13, Commissionnaires de l'Academie Impériale des sciences, St. Petersbourg, Russia.
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14. V. M. Makeyev, D. P. Ponomareva, V. V. Pitulko, G. M. Chernova and D. V. Solovyeva, 2003, [http://instaar.colorado.edu/aaar/journal_issues/abstract.php?id=2145 "Vegetation and Climate of the New Siberian Islands for the past 15,000 Years"]. ''Arctic, Antarctic, and Alpine Research'', vol. 35, no. 1, pp. 56–66.
15. A. M. Ivanova, V. Ushakov, G. A. Cherkashov, and A. N. Smirnov, 1999, "Placer Minerals of the Russian Arctic Shelf". ''Polarforschung''. vol. 69, pp. 163–167.
16. P. A. Nikolskiy, L.D. Sulerzhitsky, and V. V. Pitulko, 2010, "Last straw versus Blitzkrieg overkill: Climate-driven changes in the Arctic Siberian mammoth population and the Late Pleistocene extinction problem". ''Quaternary Science Reviews''. {{doi. 10.1016/j.quascirev.2010.10.017
17. . (2021). ["Novosibirski archipelago"](http://datazone.birdlife.org/site/factsheet/novosibirski-archipelago-iba-russia-(asian)). *BirdLife International*.