A high-resolution Late Quaternary climatostratigraphic record from Iskitim, Priobie Loess Plateau, SW Siberia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F70883521%3A28160%2F11%3A43865270" target="_blank" >RIV/70883521:28160/11:43865270 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.quaint.2011.01.045" target="_blank" >http://dx.doi.org/10.1016/j.quaint.2011.01.045</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.quaint.2011.01.045" target="_blank" >10.1016/j.quaint.2011.01.045</a>

Jazyk výsledku

angličtina

Název v původním jazyce

A high-resolution Late Quaternary climatostratigraphic record from Iskitim, Priobie Loess Plateau, SW Siberia

Popis výsledku v původním jazyce

The Siberian loess, being a part of the Eurasian loess belt, has provided the most complete terrestrial record of past climate change in the north-central Asia. The continuous high-resolution sections of aeolian dust deposits inter-bedded with fossil soils from the Priobie Loess Plateau and the Northern Altai Plains ? mapped as a part of the 2000 km W?E Siberian palaeoclimate transect ? have produced extraordinary evidence of the Late Quaternary climate evolution and landscape development in the parkland-steppe north of the Altai-Sayan Mountains. A complete stratigraphic loess-palaeosol record was studied at the Iskitim reference section, spanning the last c. 250 ka (MIS 7-1). The climate-indicative proxy data (magnetic susceptibility, grain size, %CaCO3, %TOC) and thin-section studies show marked and cyclic climatic variations, particularly pronounced during the Last Interglacial?Glacial cycle equivalent to the loess reference sites from the Yenisei and Katun/Altai Plain areas (the Ku

Název v anglickém jazyce

A high-resolution Late Quaternary climatostratigraphic record from Iskitim, Priobie Loess Plateau, SW Siberia

Popis výsledku anglicky

The Siberian loess, being a part of the Eurasian loess belt, has provided the most complete terrestrial record of past climate change in the north-central Asia. The continuous high-resolution sections of aeolian dust deposits inter-bedded with fossil soils from the Priobie Loess Plateau and the Northern Altai Plains ? mapped as a part of the 2000 km W?E Siberian palaeoclimate transect ? have produced extraordinary evidence of the Late Quaternary climate evolution and landscape development in the parkland-steppe north of the Altai-Sayan Mountains. A complete stratigraphic loess-palaeosol record was studied at the Iskitim reference section, spanning the last c. 250 ka (MIS 7-1). The climate-indicative proxy data (magnetic susceptibility, grain size, %CaCO3, %TOC) and thin-section studies show marked and cyclic climatic variations, particularly pronounced during the Last Interglacial?Glacial cycle equivalent to the loess reference sites from the Yenisei and Katun/Altai Plain areas (the Ku

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

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Projekt

—

Návaznosti

V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Rok uplatnění

2011

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Quaternary International

ISSN

1040-6182

e-ISSN

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Svazek periodika

240

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

11

Strana od-do

139-149

Kód UT WoS článku

000293551600015

EID výsledku v databázi Scopus

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