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Main Authors: Ellwood, Michael J, Wille, Martin, Maher, William
Format: Dataset Open Access
Language:en
Published: PANGAEA 2010
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.771607
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author Ellwood, Michael J
Wille, Martin
Maher, William
author_facet Ellwood, Michael J
Wille, Martin
Maher, William
collection Datos científicos de ciencias marinas y ambientales
contents Reconstruction of nutrient concentrations in the deep Southern Ocean has produced conflicting results. The cadmium/calcium (Cd/Ca) data set suggests little change in nutrient concentrations during the last glacial period, whereas the carbon isotope data set suggests that nutrient concentrations were higher. We determined the silicon isotope composition of sponge spicules from the Atlantic and Pacific sectors of the Southern Ocean and found higher silicic acid concentrations in the Pacific sector during the last glacial period. We propose that this increase results from changes in the stoichiometric uptake of silicic acid relative to nitrate and phosphate by diatoms, thus facilitating a redistribution of nutrients across the Pacific and Southern Oceans. Our results are consistent with the global Cd/Ca data set and support the silicic acid leakage hypothesis.
format Dataset Open Access
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institution PANGAEA
language en
publishDate 2010
publisher PANGAEA
record_format pangaea
spellingShingle Silicon isotope ratios of ODP Site 177-1089 and sediment core E33-22
Ellwood, Michael J
Wille, Martin
Maher, William
177-1089; COMPCORE; Composite Core; DRILL; Drilling/drill rig; E33-22; Joides Resolution; Leg177; Ocean Drilling Program; ODP; South Atlantic Ocean; South Pacific Ocean
Reconstruction of nutrient concentrations in the deep Southern Ocean has produced conflicting results. The cadmium/calcium (Cd/Ca) data set suggests little change in nutrient concentrations during the last glacial period, whereas the carbon isotope data set suggests that nutrient concentrations were higher. We determined the silicon isotope composition of sponge spicules from the Atlantic and Pacific sectors of the Southern Ocean and found higher silicic acid concentrations in the Pacific sector during the last glacial period. We propose that this increase results from changes in the stoichiometric uptake of silicic acid relative to nitrate and phosphate by diatoms, thus facilitating a redistribution of nutrients across the Pacific and Southern Oceans. Our results are consistent with the global Cd/Ca data set and support the silicic acid leakage hypothesis.
title Silicon isotope ratios of ODP Site 177-1089 and sediment core E33-22
topic 177-1089; COMPCORE; Composite Core; DRILL; Drilling/drill rig; E33-22; Joides Resolution; Leg177; Ocean Drilling Program; ODP; South Atlantic Ocean; South Pacific Ocean
url https://doi.org/10.1594/PANGAEA.771607