Silica stable isotopes and silicification in a carnivorous sponge Asbestopluma sp.

The stable isotope composition of benthic sponge spicule silica is a potential source of palaeoceanographic information about past deep seawater chemistry. The silicon isotope composition of spicules has been shown to relate to the silicic acid concentration of ambient water, although existing calib...

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Main Authors: Hendry, K.R., Swann, George E.A., Leng, Melanie J., Sloane, Hilary J., Goodwin, C., Berman, J., Maldonado, M.
Format: Article
Published: European Geosciences Union 2015
Online Access:https://eprints.nottingham.ac.uk/29155/
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author Hendry, K.R.
Swann, George E.A.
Leng, Melanie J.
Sloane, Hilary J.
Goodwin, C.
Berman, J.
Maldonado, M.
author_facet Hendry, K.R.
Swann, George E.A.
Leng, Melanie J.
Sloane, Hilary J.
Goodwin, C.
Berman, J.
Maldonado, M.
author_sort Hendry, K.R.
building Nottingham Research Data Repository
collection Online Access
description The stable isotope composition of benthic sponge spicule silica is a potential source of palaeoceanographic information about past deep seawater chemistry. The silicon isotope composition of spicules has been shown to relate to the silicic acid concentration of ambient water, although existing calibrations do exhibit a degree of scatter in the relationship. Less is known about how the oxygen isotope composition of sponge spicule silica relates to environmental conditions during growth. Here, we investigate the vital effects on silica, silicon and oxygen isotope composition in a carnivorous sponge, Asbestopluma sp., from the Southern Ocean. We find significant variations in silicon and oxygen isotopic composition within the specimen that are related to unusual spicule silicification. The largest variation in both isotope systems was associated with the differential distribution of an unconventional, hypersilicified spicule type (desma) along the sponge body. The absence an internal canal in the desmas suggests an unconventional silicification pattern leading to an unusually heavy isotope signature. Additional internal variability derives from a systematic offset between the peripheral skeleton of the body having systematically a higher isotopic composition than the internal skeleton. A simplified silicon isotope fractionation model, in which desmas were excluded, suggests that the lack of a system for seawater pumping in carnivorous sponges favours a low replenishment of dissolved silicon within the internal tissues, causing kinetic fractionation during silicification that impacts the isotope signature of the internal skeleton. Analysis of multiple spicules should be carried out to "average out" any artefacts in order to produce more robust downcore measurements.
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spelling nottingham-291552020-05-04T20:11:03Z https://eprints.nottingham.ac.uk/29155/ Silica stable isotopes and silicification in a carnivorous sponge Asbestopluma sp. Hendry, K.R. Swann, George E.A. Leng, Melanie J. Sloane, Hilary J. Goodwin, C. Berman, J. Maldonado, M. The stable isotope composition of benthic sponge spicule silica is a potential source of palaeoceanographic information about past deep seawater chemistry. The silicon isotope composition of spicules has been shown to relate to the silicic acid concentration of ambient water, although existing calibrations do exhibit a degree of scatter in the relationship. Less is known about how the oxygen isotope composition of sponge spicule silica relates to environmental conditions during growth. Here, we investigate the vital effects on silica, silicon and oxygen isotope composition in a carnivorous sponge, Asbestopluma sp., from the Southern Ocean. We find significant variations in silicon and oxygen isotopic composition within the specimen that are related to unusual spicule silicification. The largest variation in both isotope systems was associated with the differential distribution of an unconventional, hypersilicified spicule type (desma) along the sponge body. The absence an internal canal in the desmas suggests an unconventional silicification pattern leading to an unusually heavy isotope signature. Additional internal variability derives from a systematic offset between the peripheral skeleton of the body having systematically a higher isotopic composition than the internal skeleton. A simplified silicon isotope fractionation model, in which desmas were excluded, suggests that the lack of a system for seawater pumping in carnivorous sponges favours a low replenishment of dissolved silicon within the internal tissues, causing kinetic fractionation during silicification that impacts the isotope signature of the internal skeleton. Analysis of multiple spicules should be carried out to "average out" any artefacts in order to produce more robust downcore measurements. European Geosciences Union 2015 Article PeerReviewed Hendry, K.R., Swann, George E.A., Leng, Melanie J., Sloane, Hilary J., Goodwin, C., Berman, J. and Maldonado, M. (2015) Silica stable isotopes and silicification in a carnivorous sponge Asbestopluma sp. Biogeosciences, 12 . pp. 3489-3498. ISSN 1726-4170 http://www.biogeosciences.net/12/3489/2015/bg-12-3489-2015.html doi:10.5194/bg-12-3489-2015 doi:10.5194/bg-12-3489-2015
spellingShingle Hendry, K.R.
Swann, George E.A.
Leng, Melanie J.
Sloane, Hilary J.
Goodwin, C.
Berman, J.
Maldonado, M.
Silica stable isotopes and silicification in a carnivorous sponge Asbestopluma sp.
title Silica stable isotopes and silicification in a carnivorous sponge Asbestopluma sp.
title_full Silica stable isotopes and silicification in a carnivorous sponge Asbestopluma sp.
title_fullStr Silica stable isotopes and silicification in a carnivorous sponge Asbestopluma sp.
title_full_unstemmed Silica stable isotopes and silicification in a carnivorous sponge Asbestopluma sp.
title_short Silica stable isotopes and silicification in a carnivorous sponge Asbestopluma sp.
title_sort silica stable isotopes and silicification in a carnivorous sponge asbestopluma sp.
url https://eprints.nottingham.ac.uk/29155/
https://eprints.nottingham.ac.uk/29155/
https://eprints.nottingham.ac.uk/29155/