A 3.6 Ma sedimentological, geochemical and palynological record of sediment core ICDP5011-1 in Lake Elgygytgyn, NE Russia

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Autores principales: Brigham-Grette, Julie, Melles, Martin, Minyuk, Pavel S, Andreev, Andrei A, Tarasov, Pavel E, DeConto, Robert M, König, Sebastian, Nowaczyk, Norbert R, Wennrich, Volker, Rosén, Peter, Haltia-Hovi, Eeva, Cook, Timothy L, Gebhardt, Andrea Catalina, Meyer-Jacob, Carsten, Snyder, Jeffrey A, Herzschuh, Ulrike
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2013
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author Brigham-Grette, Julie
Melles, Martin
Minyuk, Pavel S
Andreev, Andrei A
Tarasov, Pavel E
DeConto, Robert M
König, Sebastian
Nowaczyk, Norbert R
Wennrich, Volker
Rosén, Peter
Haltia-Hovi, Eeva
Cook, Timothy L
Gebhardt, Andrea Catalina
Meyer-Jacob, Carsten
Snyder, Jeffrey A
Herzschuh, Ulrike
author_facet Brigham-Grette, Julie
Melles, Martin
Minyuk, Pavel S
Andreev, Andrei A
Tarasov, Pavel E
DeConto, Robert M
König, Sebastian
Nowaczyk, Norbert R
Wennrich, Volker
Rosén, Peter
Haltia-Hovi, Eeva
Cook, Timothy L
Gebhardt, Andrea Catalina
Meyer-Jacob, Carsten
Snyder, Jeffrey A
Herzschuh, Ulrike
collection Datos científicos de ciencias marinas y ambientales
contents Understanding the evolution of Arctic polar climate from the protracted warmth of the middle Pliocene into the earliest glacial cycles in the Northern Hemisphere has been hindered by the lack of continuous, highly resolved Arctic time series. Evidence from Lake El'gygytgyn, NE Arctic Russia, shows that 3.6-3.4 million years ago, summer temperatures were ~8°C warmer than today when pCO2 was ~400 ppm. Multiproxy evidence suggests extreme warmth and polar amplification during the middle Pliocene, sudden stepped cooling events during the Pliocene-Pleistocene transition, and warmer than present Arctic summers until ~2.2 Ma, after the onset of Northern Hemispheric glaciation. Our data are consistent with sea-level records and other proxies indicating that Arctic cooling was insufficient to support large-scale ice sheets until the early Pleistocene.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_808834
institution PANGAEA
language en
publishDate 2013
publisher PANGAEA
record_format pangaea
spellingShingle A 3.6 Ma sedimentological, geochemical and palynological record of sediment core ICDP5011-1 in Lake Elgygytgyn, NE Russia
Brigham-Grette, Julie
Melles, Martin
Minyuk, Pavel S
Andreev, Andrei A
Tarasov, Pavel E
DeConto, Robert M
König, Sebastian
Nowaczyk, Norbert R
Wennrich, Volker
Rosén, Peter
Haltia-Hovi, Eeva
Cook, Timothy L
Gebhardt, Andrea Catalina
Meyer-Jacob, Carsten
Snyder, Jeffrey A
Herzschuh, Ulrike
COMPCORE; Composite Core; ELGYGYTGYN; Elgygytgyn crater lake, Sibiria, Russia; ICDP_Elgygytgyn-Drilling-Project; ICDP5011-1; Lake Elgygytgyn - Climate History of the Arctic since 3.6 Million Years; Sampling on land
Understanding the evolution of Arctic polar climate from the protracted warmth of the middle Pliocene into the earliest glacial cycles in the Northern Hemisphere has been hindered by the lack of continuous, highly resolved Arctic time series. Evidence from Lake El'gygytgyn, NE Arctic Russia, shows that 3.6-3.4 million years ago, summer temperatures were ~8°C warmer than today when pCO2 was ~400 ppm. Multiproxy evidence suggests extreme warmth and polar amplification during the middle Pliocene, sudden stepped cooling events during the Pliocene-Pleistocene transition, and warmer than present Arctic summers until ~2.2 Ma, after the onset of Northern Hemispheric glaciation. Our data are consistent with sea-level records and other proxies indicating that Arctic cooling was insufficient to support large-scale ice sheets until the early Pleistocene.
title A 3.6 Ma sedimentological, geochemical and palynological record of sediment core ICDP5011-1 in Lake Elgygytgyn, NE Russia
topic COMPCORE; Composite Core; ELGYGYTGYN; Elgygytgyn crater lake, Sibiria, Russia; ICDP_Elgygytgyn-Drilling-Project; ICDP5011-1; Lake Elgygytgyn - Climate History of the Arctic since 3.6 Million Years; Sampling on land
url https://doi.org/10.1594/PANGAEA.808834