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Koch, B.P.* ; Ksionzek, K.B.* ; Lechtenfeld, O.J.* ; McCallister, S.L.* ; Schmitt-Kopplin, P. ; Geuer, J.K.* ; Geibert, W.*

Response to Comment on "Dissolved organic sulfur in the ocean: Biogeochemistry of a petagram inventory".

Science 356:813 (2017)

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Open Access Green as soon as Postprint is submitted to ZB.

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Dittmar et al. proposed thatmixing alone can explain our observed decrease inmarine dissolved organic sulfur with age. However, their simple model lacks an explanation for the origin of sulfur-depleted organic matter in the deep ocean and cannot adequately reproduce our observed stoichiometric changes. Using radiocarbon age also implicitlymodels the preferential cycling of sulfur that they are disputing.

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Publication type Article: Journal article

Document type Letter to the Editor

Corresponding Author

Keywords Matter; Degradation; Carbon

ISSN (print) / ISBN 0036-8075

e-ISSN 1095-9203

Journal Science

Quellenangaben Volume: 356, Issue: 6340, Article Number: 813

Publisher American Association for the Advancement of Science (AAAS)

Publishing Place Washington

Non-patent literature Publications

Reviewing status Peer reviewed

Institute(s) Research Unit BioGeoChemistry and Analytics (BGC)