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Main Authors: Janecek, Thomas R, Rea, David K
Format: Dataset Open Access
Language:en
Published: PANGAEA 1985
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Online Access:https://doi.org/10.1594/PANGAEA.757068
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author Janecek, Thomas R
Rea, David K
author_facet Janecek, Thomas R
Rea, David K
collection Datos científicos de ciencias marinas y ambientales
contents The mass accumulation rate and grain size of the total colian component isolated from pelagic sediment in two North Pacific cores, piston core KK75-02 under the prevailing westerlies and Deep-Sea Drilling Project Site 503 beneath the trade winds, have been used to evaluate changes in the intensity of atmospheric circulation and source-area aridity over the past 700,000 yr. The eolian grain size, a direct indicator of wind intensity, fluctuates at periodicities similar to those calculated for the earth's orbital parameters of precession, obliquity, and eccentricity. Both sites display greater variability in wind intensity prior to 250,000 yr ago. Eolian accumulation rates, an indicator of source-area aridity, fluctuate at periodicities similar to those of the glacial-interglacial cycles. Lower eolian accumulation rates during colder (glacial) times most likely reflect increased glacial-age humidity at central Asian and Central American source areas.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_757068
institution PANGAEA
language en
publishDate 1985
publisher PANGAEA
record_format pangaea
spellingShingle Linear sedimentation rates of ODP Hole 68-503B and sediment core KK75-02 (Table 1)
Janecek, Thomas R
Rea, David K
68-503B; Age model; Boundary description; Datum level; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; KK75-02; Leg68; North Pacific/FLANK; Pacific Ocean; PC; Piston corer; Sedimentation rate
The mass accumulation rate and grain size of the total colian component isolated from pelagic sediment in two North Pacific cores, piston core KK75-02 under the prevailing westerlies and Deep-Sea Drilling Project Site 503 beneath the trade winds, have been used to evaluate changes in the intensity of atmospheric circulation and source-area aridity over the past 700,000 yr. The eolian grain size, a direct indicator of wind intensity, fluctuates at periodicities similar to those calculated for the earth's orbital parameters of precession, obliquity, and eccentricity. Both sites display greater variability in wind intensity prior to 250,000 yr ago. Eolian accumulation rates, an indicator of source-area aridity, fluctuate at periodicities similar to those of the glacial-interglacial cycles. Lower eolian accumulation rates during colder (glacial) times most likely reflect increased glacial-age humidity at central Asian and Central American source areas.
title Linear sedimentation rates of ODP Hole 68-503B and sediment core KK75-02 (Table 1)
topic 68-503B; Age model; Boundary description; Datum level; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Event label; Glomar Challenger; KK75-02; Leg68; North Pacific/FLANK; Pacific Ocean; PC; Piston corer; Sedimentation rate
url https://doi.org/10.1594/PANGAEA.757068