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Sergey Zimov

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Sergey Aphanasievich Zimov
S.A. Zimov overlooking the Siberian landscape
BornJuly 1955
Alma materFar East State University, Vladivostok, Russia
Known forThe Northeast Science Station, Pleistocene Park, global carbon and methane cycles, Pleistocene ecosystem reconstruction
AwardsWolf Vishniac Award (1991)
Scientific career
InstitutionsNortheast Science Station, Cherskii, RU

Sergey Aphanasievich Zimov (Russian: Сергей Афанасьевич Зимов) is a Russian scientist. He is a geophysicist who specialises in arctic and subarctic ecology. He is the Director of Northeast Scientific Station (a research institute of the Russian Academy of Sciences), a senior research fellow of the Pacific Institute for Geography (an institute within the Far East Division of the Russian Academy of Sciences (FED RAS)), and one of the founders of Pleistocene Park (a 160 km2 wildlife preserve and a research substation of the Northeast Scientific Station). He is best known for his work in advocating the theory that human overhunting of large herbivores during the Pleistocene caused Siberia's grassland-steppe ecosystem to disappear and for raising awareness as to the important roles permafrost and thermokarst lakes play in the global carbon cycle.

According to a colleague, Sergey Zimov is the most cited Russian earth scientist.[1]

Life and work

Sergei Zimov is a Russian scientist who resides in Cherskii, Sakha Republic, Russia. He studied and received his degree in geophysics from Far East State University, located in Vladivostok, Russia.[2]

Zimov founded the Northeast Science Station near Cherskii in 1977.[3] Twelve years later, in 1988, he initiated the Pleistocene Park project.[3] In 1991, Sergei Zimov was awarded the Wolf Vishniac Award at the tenth International Symposium On Environmental Biogeochemistry (ISEB).[4]

Professional highlights and accomplishments

Northeast Science Station

Overview of the Northeast Science Station, Cherskii, Russia
View from the Northeast Science Station
Main article: Northeast Science Station

Coordinates: 69 degrees 30 minutes North latitude, 161 degrees 30 minutes East longitude[5]

Sergei Zimov is the director of the Northeast Science Station.[6] Located near Cherskii, Russia on the mouth of the Kolyma River, 150 kilometers south of the Arctic Ocean, the station serves as a year-round base for international Arctic research.[6] Its focus lies on carbon cycles, methane fluxes, paleoclimate, and the changing ecosystem.[7] Founded in 1977,[3] the Northeast Science Station boasts three laboratories, a network of field sites, tools for data analysis and communication, transportation, accommodation for visiting researchers,[6] and a year round staff of six.[8] A barge floating on the Kolyma River serves as a traveling dormitory and laboratory.[8]

Permafrost and methane

In collaboration with Dr. Terry Chapin and Dr. Katey Walter-Anthony, Sergei Zimov has published a series a collection of scientific papers exposing the importance of permafrost and high-latitude carbon dioxide and methane emissions in the global carbon cycle. These papers identified methane ebullition from thermokarst lakes to be a significant source of atmospheric methane, a potent greenhouse gas.[9]

Permafrost is a large global carbon reservoir which has remained frozen throughout much of the Holocene.[10] Due to recent climate change, the permafrost is beginning to thaw, releasing stored carbon and forming thermokarst lakes.[9][10] When the thawed permafrost enters the thermokarst lakes, its carbon is converted into carbon dioxide and methane and released into the atmosphere.[11][12][13] Methane is a potent greenhouse gas and the methane emissions from thermokarst lakes have the potential to initiate a positive feedback cycle in which increased atmospheric methane concentrations lead to amplified global climate change, which in turn leads to more permafrost thaw and more methane and carbon dioxide emissions.[12][13]

Pleistocene Park

Main article: Pleistocene Park
Restored grasslands in Pleistocene Park

Zimov initiated the Pleistocene Park project in 1988 in Northeast Siberia near the Northeast Science Station in Cherskii, Republic of Sakha, Russia.[3] Pleistocene Park seeks to test the hypotheses that large herbivores maintained the Pleistocene tundra steppe and that overhunting by humans caused both the animals and Pleistocene ecosystem to vanish.[2]

The grassland-steppe ecosystem which dominated Siberia during the Pleistocene disappeared 10,000 years ago and was replaced by mossy and forested tundra.[2] Concurrently, many of the large herbivores who roamed Siberia during the Pleistocene, including mammoths, woolly rhinoceroses, bison, horses, musk oxen, elk, saiga, and yaks, vanished from the region.[2] Today, reindeer and moose are the only surviving large herbivores to roam Siberia.[2] Zimov and colleagues believe that humans, with their constantly improving technology, overhunted the large herbivores and led to their extinction and extirpation. Without herbivores grazing and trampling over the land, mosses, shrubs, and trees were able to take over and replace the grassland ecosystem.[2]

At Pleistocene Park, Zimov is attempting to recreate the Pleistocene grasslands to demonstrate that the grasslands would have persisted into the Holocene if humans did not overhunt the herds of Pleistocene herbivores which roamed and maintained the ecosystem. He has demonstrated that grasses take over the landscape 1–2 years after mosses are anthropogenically removed.[2] According to Zimov, re-introducing large herbivores to Siberia would initiate a positive feedback loop promoting the reestablishment of grassland ecosystems: "The animals, their hooves, they disturb the moss and let grasses grow instead. The soil dries out, the animals deposit their fertilizer, the grass grows more, and more animals can graze."[14]

Current efforts in the park include reintroducing surviving Pleistocene megafauna into the fenced enclosure until they reach densities to change the vegetation and soil to a steppe grassland ecosystem.[2] Pleistocene Park currently covers an area of 160 square kilometers[14] and contains less than 100 large mammals[14] representing six major herbivore species (horses, moose, reindeer, muskox, elk, and bison).[3] Zimov's goal for Pleistocene Park is to increase the number of large herbivores to 20 per square kilometer then begin reintroducing predators, including wolves, bears, and Siberian tigers.[14]

In 2007 a 35-meter high flux tower was erected in the park which constantly monitors the levels of methane, carbon dioxide, water vapor and energy (temperature) in the park's atmosphere. The data among others contributes to the Global Monitoring Division of NOAA's Earth System Research Lab.[15]

Selected publications

  • Walter, K. M.; Edwards, M. E.; Grosse, G.; Zimov, S. A.; Chapin, F. S. (2007-10-26). "Thermokarst Lakes as a Source of Atmospheric CH4 During the Last Deglaciation". Science. 318 (5850): 633–636. doi:10.1126/science.1142924. ISSN 0036-8075. PMID 17962561.
This paper estimates that 33-87% of high-latitude increases in atmospheric methane originate from thermokarst lakes. It is suggested that sediments which have been frozen since the Pleistocene, called yedoma, will have high methane-releasing potential as they thaw due to climate change.
This paper quantifies methane emissions from thermokarst lakes in North Siberia. Most of the methane is sourced to thawing permafrost from the lake margins.
This essay outlines the concept behind Pleistocene Park, Sergei Zimov's research site in which he seeks to demonstrate that human overhunting of Pleistocene megafauna led to the disappearance of the Pleistocene's grassland-steppe ecosystem.
This paper suggests that increasing high-latitude ecological disturbances such as fires and grazing contribute to the long-term increase in atmospheric carbon dioxide.
This paper contends that permafrost represents a significant global carbon sink. As climate change causes permafrost to thaw, the stored carbon will be released and amplify global climate change.
This paper identifies Pleistocene-aged soils, referred to as yedoma, as being a major carbon source for methane emissions from thermokarst lakes in North Siberia.

Person

Projects

References

  1. ^ Dr. Igor Petrovich Semiletov (IARC resume), Head of the Laboratory of Geochemistry in the Polar Regions at the Pacific Oceanological Institute in Vladivostok and representative of the FED RAS at the University of Alaska Fairbanks, in an interview in 2011. See Елизавета Понарина (Elizabeta Ponarina), "Парниковое дыхание Арктики. Деградация подводной мерзлоты Восточно-Сибирского шельфа как причина возможных будущих быстрых климатических изменений." 30 December 2011, retrieved from the archives of the Russian Academy of Sciences. Retrieved 2 November 2016.
  2. ^ a b c d e f g h Sergey A. Zimov: "Pleistocene Park: Return of the Mammoth's Ecosystem." Science, 6 May 2005, vol. 308, no. 5723, pp. 796–798.
  3. ^ a b c d e "Pleistocene Park and the North-East Scientific Station," homepage of the official website, without date. Retrieved 2 November 2016.
  4. ^ William S. Reeburgh: "Meeting report." Report on the Tenth International Symposium on Environmental Biogeochemistry (ISEB-10). In: Geomicrobiology Journal 28 January 1992, vol. 10, no. 1, pp. 73–74. (Full text at eScholarship, UC.) Retrieved 3 November 2016.
  5. ^ Earth Exploration Toolbook: "Case Study: Something is Rotten in Chersky." Without date. Retrieved 2 November 3016.
  6. ^ a b c F. Stuart ‘Terry’ Chapin III: "Northeast Science Station. Cherskii, Russia." terrychapin.org, 12 November 2006. Retrieved 2 November 2016.
  7. ^ International Arctic Systems for Observing the Atmosphere (IASOA): "Cherskii, Russia. Observatory." Without date. Retrieved 2 November 2016.
  8. ^ a b Polar Field Services: "Tag Archives: Northeast Science Station." 2010–2012. Retrieved 2 November 2016.
  9. ^ a b University of Alaska Fairbanks: "Methane Bubbling From Arctic Lakes, Now And At End Of Last Ice Age." ScienceDaily, 26 October 2007. Retrieved 2 November 2016.
  10. ^ a b Sergey A. Zimov, Edward A. G. Schuur, F. Stuart Chapin III: "Climate Change Permafrost and the Global Carbon Budget." Science, 16 June 2006, vol. 312, no. 5780, pp. 1612–1613. (Full text at Heat is Online, ResearchGate.) Retrieved 2 November 2016.
  11. ^ K. M. Walter, M. E. Edwards, G. Grosse, S. A. Zimov, F. S. Chapin III: "Thermokarst Lakes as a Source of Atmospheric CH4 During the Last Deglaciation." Science, 26 October 2007, vol. 318, no. 5850, pp. 633–636. (Full text at ResearchGate.) Retrieved 2 November 2016.
  12. ^ a b K. M. Walter, S. A. Zimov, J. P. Chanton, D. Verbyla and F. S. Chapin III: "Methane bubbling from Siberian thaw lakes as a positive feedback to climate warming." Nature, vol. 443, no. 7107, 7 September 2006, pp. 71–75. (Full text at ResearchGate.)
  13. ^ a b S. A. Zimov, Y. V. Voropaev, I. P. Semiletov, S. P. Davidov, S. F. Prosiannikov, F. S. Chapin III, M. C. Chapin, S. Trumbore, S. Tyler: "North Siberian Lakes: A Methane Source Fueled by Pleistocene Carbon." In: Science, 8 August 1997, vol. 277, no. 5327, pp. 800–802. (Full text at ResearchGate.) Retrieved 2 November 2016.
  14. ^ a b c d Adam Fowler: "Siberian Window on the Ice Age." BBC News, 2 July 2007. Retrieved 2 November 2016.
  15. ^ International Arctic Systems for Observing the Atmosphere (IASOA): "Pleistocene Park." Without date. Retrieved 2 November 2016.
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