Introduction to the JoPL special issue, "Holocene paleoenvironmental records from Arctic lake sediment"

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11. 5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate.

Original languageEnglish (US)
Pages (from-to)1-7
Number of pages7
JournalJournal of Paleolimnology
Volume48
Issue number1
DOIs
StatePublished - Jun 2012

Fingerprint

lacustrine deposit
Arctic region
Holocene
lakes
sediments
paleolimnology
climate
atmospheric circulation
climate forcing
lake
late glacial
sedimentary sequence
paleoclimate
coolers
new record
environmental change
oceans
moisture
climate change
ocean

Keywords

  • Arctic lakes
  • Climate change
  • Holocene
  • Paleoenvironment
  • Proxy records

ASJC Scopus subject areas

  • Aquatic Science
  • Earth-Surface Processes

Cite this

@article{2ac66757726648ca93e762e372da4355,
title = "Introduction to the JoPL special issue, {"}Holocene paleoenvironmental records from Arctic lake sediment{"}",
abstract = "The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11. 5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate.",
keywords = "Arctic lakes, Climate change, Holocene, Paleoenvironment, Proxy records",
author = "Kaufman, {Darrell S.}",
year = "2012",
month = "6",
doi = "10.1007/s10933-012-9621-6",
language = "English (US)",
volume = "48",
pages = "1--7",
journal = "Journal of Paleolimnology",
issn = "0921-2728",
publisher = "Springer Netherlands",
number = "1",

}

TY - JOUR

T1 - Introduction to the JoPL special issue, "Holocene paleoenvironmental records from Arctic lake sediment"

AU - Kaufman, Darrell S.

PY - 2012/6

Y1 - 2012/6

N2 - The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11. 5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate.

AB - The 18 papers in this Special Issue of the Journal of Paleolimnology report new records of Holocene environmental and climate change from Arctic lake sediment. At least 15 distinct physical, chemical, and biological properties were analyzed at lakes located across the North American Arctic and subarctic, and northwestern Europe. The studies are notable for their multi-proxy approach (eight present data for at least five different proxies), and for the high quality of their geochronological control. Three of the studies analyzed sediment from more than one lake to test the influence of contrasting physiographic settings on the response of proxies to the same climate forcing. The sedimentary sequences analyzed in seven studies extend beyond 11. 5 cal ka, providing evidence for pronounced climate shifts that took place during the late-glacial period. Two-thirds extend beyond 8 cal ka; many of these records were interpreted in terms of the shift in temperature and moisture that occurred during the transition from the warm early to middle Holocene to the cooler late Holocene. These records contribute to the growing network of sites that is needed to reconstruct the spatial pattern of this pronounced paleoclimate transition, and to address how ocean-atmospheric circulation changed with the mean state of climate.

KW - Arctic lakes

KW - Climate change

KW - Holocene

KW - Paleoenvironment

KW - Proxy records

UR - http://www.scopus.com/inward/record.url?scp=84860825774&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84860825774&partnerID=8YFLogxK

U2 - 10.1007/s10933-012-9621-6

DO - 10.1007/s10933-012-9621-6

M3 - Article

AN - SCOPUS:84860825774

VL - 48

SP - 1

EP - 7

JO - Journal of Paleolimnology

JF - Journal of Paleolimnology

SN - 0921-2728

IS - 1

ER -