Articles | Volume 13, issue 24
https://doi.org/10.5194/bg-13-6683-2016
https://doi.org/10.5194/bg-13-6683-2016
Research article
 | 
22 Dec 2016
Research article |  | 22 Dec 2016

Variations in triple isotope composition of dissolved oxygen and primary production in a subtropical reservoir

Hana Jurikova, Tania Guha, Osamu Abe, Fuh-Kwo Shiah, Chung-Ho Wang, and Mao-Chang Liang

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (04 Jul 2016) by Jack Middelburg
AR by Hana Jurikova on behalf of the Authors (23 Aug 2016)  Author's response 
ED: Referee Nomination & Report Request started (25 Aug 2016) by Jack Middelburg
ED: Publish subject to technical corrections (14 Oct 2016) by Jack Middelburg
AR by Hana Jurikova on behalf of the Authors (21 Oct 2016)  Author's response   Manuscript 
ED: Publish subject to minor revisions (Editor review) (22 Nov 2016) by Jack Middelburg
AR by Hana Jurikova on behalf of the Authors (23 Nov 2016)  Author's response   Manuscript 
ED: Publish as is (24 Nov 2016) by Jack Middelburg
AR by Hana Jurikova on behalf of the Authors (24 Nov 2016)
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Short summary
Life on Earth is directly or indirectly linked to primary production (PP), the quantification of which poses a challenge. In our study we use the oxygen isotopes and oxygen–argon ratios technique to estimate PP in situ. To date this method has been used to assess PP in the ocean and we expand on its application to freshwater systems. Providing that the physical structure of the water column is constrained, this method presents a powerful tracer for atmospheric vs. photosynthetic oxygen input.
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