Late Quaternary Loess-palaosol succesion and atmospheric circulation, Central Siberia

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F03%3A00000103" target="_blank" >RIV/00025798:_____/03:00000103 - isvavai.cz</a>

Result on the web

—

DOI - Digital Object Identifier

—

Result language

angličtina

Original language name

Late Quaternary Loess-palaosol succesion and atmospheric circulation, Central Siberia

Original language description

Loess-palaeosol records in Central Siberia indicate establishment of periglacial steppe-tundra during OIS 4 and OIS 2, replaced by parkland steppe and boreal forest during warmer intervals within OIS 3. A gradual transition from parkland-steppe (OIS 5a)to moist tundra conditions (OIS 4) occurred ~75 ka BP. General cooling, punctuated by isolated short warm intervals, marked the period from ~75 to ~25 ka BP. OIS 2, ~25-18 ka BP, was marked by a sharp change to a dry tundra climate, followed by rapid arming ~15-8 ka BP. Mid- and latest Holocene conditions were warmer than those recorded during the OIS 5e maximum. Textural, magnetic susceptibility, and mineralogical analyses indicate that the OIS 4 and OIS 2 loess units were derived from different

Czech name

—

Czech description

—

Type

D - Article in proceedings

CEP classification

DB - Geology and mineralogy

OECD FORD branch

—

Project

—

Continuities

Z - Vyzkumny zamer (s odkazem do CEZ)

Publication year

2003

Confidentiality

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

Article name in the collection

XVI INQUA Congress Programs with Abstracts

ISBN

0-945920-51-2

ISSN

—

e-ISSN

—

Number of pages

1

Pages from-to

217

Publisher name

Neuveden

Place of publication

Reno

Event location

Reno

Event date

Jan 1, 2003

Type of event by nationality

WRD - Celosvětová akce

UT code for WoS article

—