Articles | Volume 15, issue 4
https://doi.org/10.5194/cp-15-1327-2019
https://doi.org/10.5194/cp-15-1327-2019
Research article
 | 
18 Jul 2019
Research article |  | 18 Jul 2019

Central Tethyan platform-top hypoxia during Oceanic Anoxic Event 1a

Alexander Hueter, Stefan Huck, Stéphane Bodin, Ulrich Heimhofer, Stefan Weyer, Klaus P. Jochum, and Adrian Immenhauser

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (10 May 2019) by Yannick Donnadieu
AR by Alexander Hueter on behalf of the Authors (29 May 2019)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (14 Jun 2019) by Yannick Donnadieu
AR by Alexander Hueter on behalf of the Authors (18 Jun 2019)  Author's response   Manuscript 
ED: Publish as is (01 Jul 2019) by Yannick Donnadieu
AR by Alexander Hueter on behalf of the Authors (02 Jul 2019)  Author's response   Manuscript 
Download
Short summary
In this multi-proxy study we present and critically discuss the hypothesis that during the early Aptian, platform-top hypoxia temporarily established in some of the vast epeiric seas of the central Tethys and triggered significant changes in reefal ecosystems. Data shown here shed light on the driving mechanisms that control poorly understood faunal patterns during OAE 1a in the neritic realm and provide evidence on the intricate relation between basinal and platform-top water masses.