NATURAL ENVIRONMENT DYNAMICS AND MORPHOLITHOGENESIS IN SHALLOWS OF THE EAST SIBERIAN ARCTIC SHELF

2021 ◽  
Vol 25 (3) ◽  
pp. 3-21
Author(s):  
A.V. Gavrilov ◽  
E.I. Pizhankova
2018 ◽  
Vol 15 (15) ◽  
pp. 4777-4779
Author(s):  
Katy J. Sparrow ◽  
John D. Kessler

Abstract. In this comment, we outline two major concerns regarding some of the key data presented in this paper. Both of these concerns are associated with the natural abundance radiocarbon-methane (14C-CH4) data. First, no systematic methodology is presented, nor previous peer-reviewed publication referenced, for how these samples were collected, prepared, and ultimately analyzed for 14C-CH4. Not only are these procedural details missing, but the critical evaluation of them using gaseous and aqueous blanks and standards was omitted although these details are essential for any reader to evaluate the quality of data and subsequent interpretations. Second, due to the lack of methodological details, the source of the sporadic anthropogenic contamination cannot be determined and thus it is premature for the authors to suggest it was in the natural environment prior to sample collection. As the natural 14C-CH4 data are necessary for the authors' stated scientific objectives of understanding the origin of methane in the East Siberian Arctic Shelf, our comment serves to highlight that the study's objectives have not been met.


Science ◽  
2010 ◽  
Vol 329 (5996) ◽  
pp. 1146-1147 ◽  
Author(s):  
V. V. Petrenko ◽  
D. M. Etheridge ◽  
R. F. Weiss ◽  
E. J. Brook ◽  
H. Schaefer ◽  
...  
Keyword(s):  

2016 ◽  
Vol 9 (6) ◽  
pp. 470-470 ◽  
Author(s):  
Igor Semiletov ◽  
Irina Pipko ◽  
Örjan Gustafsson ◽  
Leif G. Anderson ◽  
Valentin Sergienko ◽  
...  

2018 ◽  
Author(s):  
Birgit Wild ◽  
Natalia Shakhova ◽  
Oleg Dudarev ◽  
Alexey Ruban ◽  
Denis Kosmach ◽  
...  

2016 ◽  
Author(s):  
Célia J. Sapart ◽  
Natalia Shakhova ◽  
Igor Semiletov ◽  
Joachim Jansen ◽  
Sönke Szidat ◽  
...  

Polar Science ◽  
2020 ◽  
pp. 100571 ◽  
Author(s):  
Yasunori Tohjima ◽  
Jiye Zeng ◽  
Tomoko Shirai ◽  
Yosuke Niwa ◽  
Shigeyuki Ishidoya ◽  
...  

2019 ◽  
Author(s):  
Ö. Gustafsson ◽  
N. Shakhova ◽  
I.P. Semiletov ◽  
J. Steinbach ◽  
H Holmstrand ◽  
...  

2010 ◽  
Vol 51 (1) ◽  
pp. 83-87 ◽  
Author(s):  
A.F. Safronov ◽  
E.Yu. Shits ◽  
M.N. Grigor'ev ◽  
M.E. Semenov

Author(s):  
Natalia Shakhova ◽  
Igor Semiletov ◽  
Valentin Sergienko ◽  
Leopold Lobkovsky ◽  
Vladimir Yusupov ◽  
...  

Sustained release of methane (CH 4 ) to the atmosphere from thawing Arctic permafrost may be a positive and significant feedback to climate warming. Atmospheric venting of CH 4 from the East Siberian Arctic Shelf (ESAS) was recently reported to be on par with flux from the Arctic tundra; however, the future scale of these releases remains unclear. Here, based on results of our latest observations, we show that CH 4 emissions from this shelf are likely to be determined by the state of subsea permafrost degradation. We observed CH 4 emissions from two previously understudied areas of the ESAS: the outer shelf, where subsea permafrost is predicted to be discontinuous or mostly degraded due to long submergence by seawater, and the near shore area, where deep/open taliks presumably form due to combined heating effects of seawater, river run-off, geothermal flux and pre-existing thermokarst. CH 4 emissions from these areas emerge from largely thawed sediments via strong flare-like ebullition, producing fluxes that are orders of magnitude greater than fluxes observed in background areas underlain by largely frozen sediments. We suggest that progression of subsea permafrost thawing and decrease in ice extent could result in a significant increase in CH 4 emissions from the ESAS.


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