Results 151 to 160 of about 1,205 (177)
Yedoma - loess or not loess – that’s the question
Late Pleistocene Yedoma is often described as arctic loess, but its formation is still disputed in literature. Differences of interpretation remain between researchers of western and eastern Beringia.
Strauss, Jens +3 more
core +3 more sources
Characterization of organic matter stored in Yedoma and thermokarst permafrost
The permafrost region approximately makes up one quarter of the land surface of the Northern Hemisphere. Its soil organic carbon pool is estimated to be about twice the size of carbon in the modern atmosphere.
Strauss, Jens +3 more
core +5 more sources
Past and recent thermal erosion degrades Siberian Yedoma
The high thaw vulnerability of Yedoma (Ice Complex) in combination with its high contents of labile organic matter makes these ice-rich permafrost deposits an object of research activities that investigate permafrost degradation and the permafrost-carbon
Bornemann, Niko +13 more
core +3 more sources
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Increasing organic carbon biolability with depth in yedoma permafrost
2019Permafrost thaw subjects previously frozen organic carbon (OC) to microbial decomposition, generating the greenhouse gases (GHG) carbon dioxide (CO2) and methane (CH4) and fueling a positive climate feedback. Over one quarter of permafrost OC is stored in deep, ice-rich Pleistocene-aged yedoma permafrost deposits.
Heslop, J. K. +8 more
openaire +1 more source
Yedoma sediments with gravel and rock debris inclusions: Characteristics and origin
Permafrost and Periglacial Processes, 2023Yurij K Vasil'Chuk
exaly
Quantifying Wedge-Ice Volumes in Yedoma and Thermokarst Basin Deposits
Permafrost and Periglacial Processes, 2015Mathias Ulrich +3 more
openaire +3 more sources
The deep permafrost carbon pool of the Yedoma region in Siberia and Alaska
Geophysical Research Letters, 2013Guido Grosse +2 more
exaly

