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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)
DOI PMC
Open Access Green möglich sobald Postprint bei der ZB eingereicht worden ist.
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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Publikationstyp Artikel: Journalartikel
Dokumenttyp Letter to the Editor
Korrespondenzautor
Schlagwörter Matter; Degradation; Carbon
ISSN (print) / ISBN 0036-8075
e-ISSN 1095-9203
Zeitschrift Science
Quellenangaben Band: 356, Heft: 6340, Seiten: , Artikelnummer: 813 Supplement: ,
Verlag American Association for the Advancement of Science (AAAS)
Verlagsort Washington
Nichtpatentliteratur Publikationen
Begutachtungsstatus Peer reviewed
Institut(e) Research Unit BioGeoChemistry and Analytics (BGC)