Pleistocene sediment offloading and the global sulfur cycle

Quaternary sea level fluctuations have greatly affected the sediment budgets of the continental shelves. Previous studies suggested that this caused a considerable increase in the net loss of shelf sediments. Since sediment accumulation and erosion are closely tied to the formation and re-oxidation...

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Main Authors: S. Markovic, A. Paytan, U. G. Wortmann
Format: Article
Language:English
Published: Copernicus Publications 2015-05-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/12/3043/2015/bg-12-3043-2015.pdf
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author S. Markovic
A. Paytan
U. G. Wortmann
author_facet S. Markovic
A. Paytan
U. G. Wortmann
author_sort S. Markovic
collection DOAJ
description Quaternary sea level fluctuations have greatly affected the sediment budgets of the continental shelves. Previous studies suggested that this caused a considerable increase in the net loss of shelf sediments. Since sediment accumulation and erosion are closely tied to the formation and re-oxidation of pyrite, we use a high-resolution record of sulfur isotope ratios (<sup>34</sup>S / <sup>32</sup>S) of marine sulfate to evaluate the implications of the so-called "shelf sediment offloading" on the global sulfur cycle. Modeling of our &delta;<sup>34</sup>S record suggests that erosion during sea level lowstands was only partly compensated by increased sedimentation during times of rising sea level and sea level highstands. Furthermore, our data suggests that shelf systems reached a new equilibrium state about 700 ka, which considerably slowed or terminated shelf sediment offloading.
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spelling doaj.art-f3d0dfcbbeec49cf94decc46cb6960c42022-12-21T23:29:41ZengCopernicus PublicationsBiogeosciences1726-41701726-41892015-05-0112103043306010.5194/bg-12-3043-2015Pleistocene sediment offloading and the global sulfur cycleS. Markovic0A. Paytan1U. G. Wortmann2Department of Geology, University of Toronto, 22 Russell St. M5S3B1, Toronto, CanadaInstitute of Marine Sciences, University of California Santa Cruz, Santa Cruz, CA 94064, USADepartment of Geology, University of Toronto, 22 Russell St. M5S3B1, Toronto, CanadaQuaternary sea level fluctuations have greatly affected the sediment budgets of the continental shelves. Previous studies suggested that this caused a considerable increase in the net loss of shelf sediments. Since sediment accumulation and erosion are closely tied to the formation and re-oxidation of pyrite, we use a high-resolution record of sulfur isotope ratios (<sup>34</sup>S / <sup>32</sup>S) of marine sulfate to evaluate the implications of the so-called "shelf sediment offloading" on the global sulfur cycle. Modeling of our &delta;<sup>34</sup>S record suggests that erosion during sea level lowstands was only partly compensated by increased sedimentation during times of rising sea level and sea level highstands. Furthermore, our data suggests that shelf systems reached a new equilibrium state about 700 ka, which considerably slowed or terminated shelf sediment offloading.http://www.biogeosciences.net/12/3043/2015/bg-12-3043-2015.pdf
spellingShingle S. Markovic
A. Paytan
U. G. Wortmann
Pleistocene sediment offloading and the global sulfur cycle
Biogeosciences
title Pleistocene sediment offloading and the global sulfur cycle
title_full Pleistocene sediment offloading and the global sulfur cycle
title_fullStr Pleistocene sediment offloading and the global sulfur cycle
title_full_unstemmed Pleistocene sediment offloading and the global sulfur cycle
title_short Pleistocene sediment offloading and the global sulfur cycle
title_sort pleistocene sediment offloading and the global sulfur cycle
url http://www.biogeosciences.net/12/3043/2015/bg-12-3043-2015.pdf
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AT apaytan pleistocenesedimentoffloadingandtheglobalsulfurcycle
AT ugwortmann pleistocenesedimentoffloadingandtheglobalsulfurcycle