oa Organic Matter in Bottom Sediments of the Northeastern Part of the Kara Sea as an Indicator of Sedimentation

References

1. ConnanJ., CassouA.
   , 1980. Properties of gases and petroleum liquids derived from terrestrial kerogen at various maturation levels. Geochem.Cosmochim.Acta. V.44(1). P.1–23.
   [Google Scholar]
2. LevitanM.A., LavrushinYu.A., SteinR.
   , 2007. Outlines of sedimentation history of the Arctic Ocean and Subarctic Seas for the last 130 ka. M.: GEOS, 404p.
   [Google Scholar]
3. PolyakL., NiessenF., GataullinV., GainanovV.
   , 2008. The eastern extent of the Barents–Kara ice sheet during the Last Glacial Maximum based on seismic-reflection data from the eastern Kara Sea. Polar Research. V.27. P.162–174.
   [Google Scholar]
4. RomankevichE.A., VetrovA.A.
   , 2001. Cycle of Carbon in the Russian Arctic Seas. Moscow: Nauka, 302 p.