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The Taconite Inlet Lakes Project: a systems approach to paleoclimatic reconstruction

Identifieur interne : 001292 ( Istex/Corpus ); précédent : 001291; suivant : 001293

The Taconite Inlet Lakes Project: a systems approach to paleoclimatic reconstruction

Auteurs : R. S. Bradley ; M. J. Retelle ; S. D. Ludlam ; D. R. Hardy ; B. Zolitschka ; S. F. Lamoureux ; M. S. V. Douglas

Source :

RBID : ISTEX:1243E2B2AFF475C28C061CCF33C2ACC362EB04F4

Abstract

Abstract: A comprehensive study of meteorological, hydrological, limnological and sedimentological conditions in the watersheds of density-stratified (meromictic) lakes around Taconite Inlet, Northern Ellesmere Island, N.W.T., Canada was carried out from 1990–1992. Lakes C1 and C2 contain seawater ‘trapped’ by isostatic uplift as the former embayments became isolated from the sea. These lakes, and Lake C3, contain varved sediments which provide an annually resolvable paleoclimatic record. By studing the major systems influencing sedimentation in one of these lakes (Lake C2) a better understanding of the climatic controls on varve formation, and hence on the paleoclimatic signal in the varved sediment record, was obtained. The varves of Lake C2 provide a proxy record of summer temperature for the region.

Url:
DOI: 10.1007/BF00176930

Links to Exploration step

ISTEX:1243E2B2AFF475C28C061CCF33C2ACC362EB04F4

Le document en format XML

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<State>MA</State>
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<City>Trier</City>
<Country>Germany</Country>
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<City>Edmonton</City>
<Country>Canada</Country>
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<Para>A comprehensive study of meteorological, hydrological, limnological and sedimentological conditions in the watersheds of density-stratified (meromictic) lakes around Taconite Inlet, Northern Ellesmere Island, N.W.T., Canada was carried out from 1990–1992. Lakes C1 and C2 contain seawater ‘trapped’ by isostatic uplift as the former embayments became isolated from the sea. These lakes, and Lake C3, contain varved sediments which provide an annually resolvable paleoclimatic record. By studing the major systems influencing sedimentation in one of these lakes (Lake C2) a better understanding of the climatic controls on varve formation, and hence on the paleoclimatic signal in the varved sediment record, was obtained. The varves of Lake C2 provide a proxy record of summer temperature for the region.</Para>
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<Heading>Key words</Heading>
<Keyword>paleoclimatic</Keyword>
<Keyword>meromictic</Keyword>
<Keyword>varves</Keyword>
<Keyword>arctic</Keyword>
<Keyword>drainage basin characteristics</Keyword>
<Keyword>lacustrine sedimentation</Keyword>
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<SimplePara>This is the first in a series of papers published in this issue on the Taconite Inlet Lakes Project. These papers were collected by Dr R. S. Bradley.</SimplePara>
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<abstract lang="en">Abstract: A comprehensive study of meteorological, hydrological, limnological and sedimentological conditions in the watersheds of density-stratified (meromictic) lakes around Taconite Inlet, Northern Ellesmere Island, N.W.T., Canada was carried out from 1990–1992. Lakes C1 and C2 contain seawater ‘trapped’ by isostatic uplift as the former embayments became isolated from the sea. These lakes, and Lake C3, contain varved sediments which provide an annually resolvable paleoclimatic record. By studing the major systems influencing sedimentation in one of these lakes (Lake C2) a better understanding of the climatic controls on varve formation, and hence on the paleoclimatic signal in the varved sediment record, was obtained. The varves of Lake C2 provide a proxy record of summer temperature for the region.</abstract>
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<topic>Geochemistry</topic>
<topic>Hydrogeology</topic>
<topic>Meteorology/Climatology</topic>
<topic>Sedimentology</topic>
<topic>Hydrobiology</topic>
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<identifier type="ISSN">0921-2728</identifier>
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