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Martin Konert

Researcher at VU University Amsterdam

Publications -  11
Citations -  1584

Martin Konert is an academic researcher from VU University Amsterdam. The author has contributed to research in topics: Glacial period & Particle. The author has an hindex of 9, co-authored 11 publications receiving 1446 citations.

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Comparison of laser grain size analysis with pipette and sieve analysis: a solution for the underestimation of the clay fraction

TL;DR: In this paper, the grain size of soil and sediment samples is determined by the sieve method for the coarse fractions and by the pipette method, based on the Stokes sedimentation rates, for the fine fractions.
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Penetration of Atlantic westerly winds into Central and East Asia

TL;DR: The geographical position of the convergence zone where the western Atlantic climate system meets the Asian (winter) monsoonal system depends on their relative strength as discussed by the authors, which is determined by the intensities of the air pressure gradients over the North Atlantic, and the Siberian High Pressure Cell, respectively.
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Ultra-high resolution pollen record from the northern Andes reveals rapid shifts in montane climates within the last two glacial cycles

TL;DR: In this article, a composite pollen-based record of altitudinal vegetation changes from Lake Fuquene (5° N) in Colombia at 2540 m elevation was developed, and the reconstructed MAT record largely concurred with the ~100 and 41-kyr (obliquity) paced glacial cycles and is superimposed by extreme changes of up to 7 to 10° Celsius within a few hundred years at the major glacial terminations and during marine isotope stage 3.
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The late Miocene and Pliocene climate in East Asia as recorded by grain size and magnetic susceptibility of the Red Clay deposits (Chinese Loess Plateau)

TL;DR: Grain-size characteristics of the aeolian Red Clay sediment series in China demonstrate the existence of warm-cool alternations during the late Miocene and Pliocene.
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Late Glacial fluvial response of the Niers-Rhine (western Germany) to climate and vegetation change

TL;DR: The Niers-Rhine experienced a channel pattern change from braided, via a transformational phase, to meandering in the early Late Glacial as discussed by the authors, which is explained by climate amelioration at the Late Pleniglacial to late Glacial transition and climate-related hydrological, lithological and vegetation changes.