Woodlands and steppes: Pleistocene vegetation in Yakutia's most continental part recorded in the Batagay permafrost sequenceAshastina K.,
Kuzmina S.,
Rudaya N.,
Troeva E.,
Schoch W.,
Römermann C.,
Reinecke J.,
Otte V.,
Savvinov G.,
Wesche K.,
Kienast F. as a refugium also for other organisms of the Pleistocene
mammoth steppe including the iconic large
Geochemistry and U-Pb geochronology of 1590 and 1550 Ma mafic dyke swarms of western Laurentia: Mantle plume magmatism shared with AustraliaKamo, S. L.,
Söderlund, Ulf,
Hamilton, Mike А.,
Ernst, Richard E.,
Cousens, Brian,
Harlan, Stephen S.,
Wade, C. E.,
Thorkelson, D. J.,
Rogers, C. -central Laurentia represent components of a large igneous province (LIP), which we name the “ca. 1590 Ma
Mammoth Опорный разрез каргинских отложений в среднем течении р. Чулым (Томская область) in the middle part of the outcrop. Remains of large mammals from
mammoth complex (from 13 species) are confined
Paleo-ecology of the Yedoma Ice Complex on Sobo-Sise Island (EasternLena Delta, Siberian Arctic)Wetterich, S.,
Rudaya, N.,
Nazarova, L.,
Syrykh, L.,
Pavlova, M.,
Palagushkina, O.,
Kizyakov, A.,
Wolter, J.,
Kuznetsova, T.,
Aksenov, A.,
Stoof-Leichsenring, K. R.,
Schirrmeister, L.,
Fritz, M. Beringian tundra-steppe that maintained the
Mammoth fauna including rare evidence for woolly rhinoceros