Results 21 to 30 of about 561 (169)

Morphological record of pedogenesis and landscape evolution in the upper quaternary pedosediments within the upper Volga river basin

open access: yesБюллетень Почвенного института им. В.В. Докучаева, 2016
The morphological record of pedogenesis (mostly at a micromorphological scale) and the features of paleosols developed at the northern geographical extremity of the MIS3 paleopedoshpere (including the Bryansk fossil soils) are described.
A. V. Rusakov, S. N. Sedov
doaj   +1 more source

How did Marine Isotope Stage 3 and Last Glacial Maximum climates differ? – Perspectives from equilibrium simulations [PDF]

open access: yesClimate of the Past, 2009
Dansgaard-Oeschger events occurred frequently during Marine Isotope Stage 3 (MIS3), as opposed to the following MIS2 period, which included the Last Glacial Maximum (LGM).
C. J. Van Meerbeeck   +2 more
doaj  

PALEOCLIMATE AND PALEOENVIRONMENT IN NORTH-WESTERN ITALY (SOUTHERN ALPS) DURING THE LAST GLACIAL STAGE: THE SMALL-MAMMAL RECORD FROM THE BUCO DEL FRATE CAVE (PREVALLE – BRESCIA)

open access: yesRivista Italiana di Paleontologia e Stratigrafia, 2023
The palaeoclimatic and palaeoenvironmental data obtained by the study of the Buco del Frate cave small-mammals indicate that, around 40,000 years ago (MIS3), the eastern part of the province of Brescia, immediately to the west of Lake Garda, was ...
Fabio Bona   +2 more
doaj   +1 more source

Hominid Alluvial Corridor (HAC) of the Guadalquivir and Guadaíra River Valleys (Southern Spain): Geoarchaeological Functionality of the Middle Paleolithic Assemblages during the Upper Pleistocene

open access: yesGeosciences, 2023
This research addresses the geomorphological connectivity existing amid the piedmont’s karstic fillings (Sierra de Esparteros) and the Guadaíra and Guadalquivir Rivers’ alluvial terraces (SW of Spain), spotted with vestiges of human activities (Middle ...
Fernando Díaz del Olmo   +5 more
doaj   +1 more source

Establishing a Luminescence-Based Chronostratigraphy for the Last Glacial-Interglacial Cycle of the Loess-Palaeosol Sequence Achajur (Armenia)

open access: yesFrontiers in Earth Science, 2021
The loess-palaeosol section Achajur is part of the Sevkar loess area in north-eastern Armenia and comprises three prominent pedocomplexes with intercalated loess units, probably spanning at least three glacial-interglacial cycles.
Johanna Lomax   +6 more
doaj   +1 more source

Climate-Induced Vegetation Changes Leading to Polygenetic Soil Development in NE Hungary at the MIS3/MIS 2 Transition

open access: yesGeosciences
The transition from MIS3 interstadial to the coldest stadial of the last glacial (MIS 2) marked a rapid change in the climate. Findings of multiproxy (sedimentological, MS, geochemical (AAS, XRD), micromorphological, anthracological, phytolith and ...
Sándor Gulyás   +9 more
doaj   +1 more source

Chronology of Late Saalian and Middle Weichselian episodes of ice-free lacustrine sedimentation recorded in the Arumetsa section, southwestern Estonia [PDF]

open access: yesEstonian Journal of Earth Sciences, 2010
The information obtained from a 21 m thick open-pit section of silty-clayey sediments in the Arumetsa bedrock valley, southwestern Estonia, revealed that lacustrine to glaciolacustrine sedimentation at the site started prior to 151 ka ago and lasted to ...
Maris Rattas   +6 more
doaj   +1 more source

PLEISTOCENE-HOLOCENE PALAEOENVIRONMENTAL RECORDS FROM PERMAFROST SEQUENCES AT THE KARA SEA COAST (NW SIBERIA, RUSSIA)

open access: yesGeography, Environment, Sustainability, 2013
The Kara Sea coasts were studied using comprehensive stratigraphic and geocryological methods. The paper presents the new analytical studies of ground ice and Quaternary deposits of Western Taymyr and presents the results of spore and pollen ...
Irina Streletskaya   +4 more
doaj   +1 more source

Fossil population structure and mortality analysis of the cave bears from Urşilor Cave, north-western Romania [PDF]

open access: yesActa Palaeontologica Polonica, 2016
Research in cave bear palaeobiology focusing on population structure and mortality analysis may improve our understanding regarding the ecology of this species which vanished at the end of Marine Isotope Stage (MIS) 3, prior to Last Glacial Maximum (LGM),
Marius Robu
doaj   +1 more source

Climate and ice sheet dynamics in Patagonia throughout marine isotope stages 2 and 3 [PDF]

open access: yesClimate of the Past
During the Last Glacial Maximum (LGM, ∼ 23 000 to 19 000 years ago), the Patagonian Ice Sheet (PIS) covered the central chain of the Andes between ∼ 38 to 55° S.
A. Castillo-Llarena   +12 more
doaj   +1 more source

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