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Late Pleistocene 100-kyr glacial cycles paced by precession forcing of summer insolation
Climate variability over the past 800,000 years has long been described as being dominated by ~100-kyr glacial cycles, and researchers have debated...
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Morphodynamics and Morphotectonics of the Varzuga River Estuary Area in the Late Glacial and Holocene (Terskiy Coast of the White Sea)
AbstractThe late-glacial and post-glacial history of the development of the White Sea coastal zone in the area of the Varzuga River estuary is...
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Glacial reconstruction and periglacial dynamics at the end of Late Pleistocene on the surface of Cofre de Perote volcano, México: a climatological retrospective
Despite being within the intertropical region of the planet, the Mexican territory still has glacier-covered mountains. In recent decades, important...
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Pollen and grain size characteristics recorded from evaporite in the Kumishi Basin in arid Central Asia: implications for climate and environmental change since the late glacial
Climatic and environmental changes in the arid region of Central Asia since the late glacial period have long been a research focus. This study...
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Reconstruction of Late Glacial Conditions of Exogenic Landscape Formation of Central Kamchatka: Data on Spore–Pollen Analysis
AbstractSpore–pollen analysis of lacustrine and subaerial sediments of the KamPlen reference section in the Central Kamchatka Depression (CKD) is...
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Morphology and History of Development of the Moscow River Valley in the Late Glacial and Holocene
AbstractThe morphology of the floodplain–channel complex of the Moscow River and its development history before the beginning of intensive human...
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Multidisciplinary Analysis to Interpret the Palaeoclimate and Depositional Environment of the Late Paleozoic Post-glacial Sediments from Wardha Basin, Maharashtra, Central India
A multidisciplinary analysis has been applied to subsurface samples from borehole MAWP 114, Wardha basin, Maharashtra State, central India, in order...
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Use of δ13С Variations in Organic Matter of Paleosols of Western Transbaikalia for Reconstruction of Paleoprecipitation Dynamics in the Late Glacial and Holocene
AbstractAnalysis of the stable carbon isotopic composition (δ 13 C) of soil organic matter is important for assessing past climate changes and the...
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Late Glacial Glaciomarine and Holocene Marine Sediments in the Eastern Part of the Barents Sea: Structure, Composition, Thickness, and Conditions of Formation
AbstractGeological-geophysical data show that the Holocene marine and Late Glacial glaciomarine sediments in the eastern part of the Barents Sea are...
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Kosa Mesolithic Sites in the Context of the Palaeoenvironmental History of the Upper Kama Basin in the Late Glacial and Early Holocene
AbstractThe results of interdisciplinary (archaeological and palaeoecological) studies conducted in 2018–2021 in the northern part of Perm Territory...
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Late Pleistocene Glacial-Paleosol-cosmic record of the Viso Massif—France and Italy: New evidence in support of the Younger Dryas boundary (12.8 ka)
Mount Viso (3841 m asl), one of the highest mountains in the Western European Alps carries not only a glacial record following the end of the last...
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Mosses recognized as glacial relicts from their postglacial distribution in Poland
Some glacial relict (mosses) have survived from the Ice Age up to the present time in specific, long-lasting habitats. Mires are one of the most...
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Near-synchronous Northern Hemisphere and Patagonian Ice Sheet variation over the last glacial cycle
Northern Hemisphere insolation intensity is roughly in phase with Southern Hemisphere climate proxies, leading to a common conclusion that northern...
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The Records of Environmental Changes in Lacustrine–Swamp Sequences within the Mountain Area of Iturup Island since the Late Glacial Period
AbstractWe have received unique material on the development of the natural environment for the last 12 400 cal. yr. BP in the central part of Iturup...
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Glacial Sedimentation
Moraines are landforms of glacial deposition. They are formed in different locations and by different, active and passive processes. For this reason,...
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Freeze-thaw cycles and associated geomorphology in a post-glacial environment: current glacial, paraglacial, periglacial and proglacial scenarios at Pico de Orizaba volcano, Mexico
The glacial history of Pico de Orizaba indicates that during the Last Glacial Maximum, its icecap covered up to ∼3000 m asl; due to the air...
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Geomorphology and the Formation History of Glacial Materials of the Ev’vayam River Valley (Koryak Highlands)
AbstractThree moraines of different ages and morphology were identified in the valley of the Ev’vayam River on the basis of the interpretation of...
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The hidden glacial landscape of the Monti della Laga (central Apennines, Italy)
The geological and geomorphological record of the Last Glaciation in the Apennines is extensively documented, except for the Monti della Laga sector,...
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Potential late glacial maximum refugial areas of Alaska-Yukon postglacial migrant plants
About 38% of indigenous vascular plants in Alaska and Yukon (609 of 1,620 taxa) were likely postglacial migrants from the Last Glacial Maximum (LGM)...
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Geomorphological Evidence of High River Runoff in the Volga Basin during the Late Glacial
AbstractLarge paleochannels are considered to be a geomorphological phenomenon. The landscape–geomorphological traces of large paleochannels on the...
