Monsoonal forcing of cold-water coral growth off southeastern Brazil during the past 160&thinsp;kyr

Bahr, André; Doubrawa, Monika; Titschack, Jürgen; Austermann, Gregor; Koutsodendris, Andreas; Nürnberg, Dirk; Albuquerque, Ana Luiza; Friedrich, Oliver; Raddatz, Jacek

doi:https://doi.org/10.5194/bg-17-5883-2020

Articles | Volume 17, issue 23

https://doi.org/10.5194/bg-17-5883-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/bg-17-5883-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 17, issue 23

Research article

|

01 Dec 2020

Research article |

| 01 Dec 2020

Monsoonal forcing of cold-water coral growth off southeastern Brazil during the past 160 kyr

André Bahr, Monika Doubrawa, Jürgen Titschack, Gregor Austermann, Andreas Koutsodendris, Dirk Nürnberg, Ana Luiza Albuquerque, Oliver Friedrich, and Jacek Raddatz

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Final revised paper (published on 01 Dec 2020)
Preprint (discussion started on 30 Jun 2020)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'Review of Bahr et al.', Robin Fentimen, 24 Aug 2020
- AC1: 'Response to RC1 (Robin Fentimen)', André Bahr, 20 Sep 2020
RC2: 'Comments to the Authors MS- bg-2020-206', Anonymous Referee #2, 02 Sep 2020
- AC2: 'Reply to RC2', André Bahr, 20 Sep 2020

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (review by editor) (21 Sep 2020) by Aninda Mazumdar

AR by André Bahr on behalf of the Authors (23 Sep 2020) Manuscript

ED: Publish as is (10 Oct 2020) by Aninda Mazumdar

AR by André Bahr on behalf of the Authors (13 Oct 2020)

Short summary

We explore the sensitivity of cold-water corals (CWCs) to environmental changes utilizing a multiproxy approach on a coral-bearing sediment core from off southeastern Brazil. Our results reveal that over the past 160 kyr, CWCs flourished during glacial high-northern-latitude cold events (Heinrich stadials). These periods were associated with anomalous wet phases on the continent enhancing terrigenous nutrient and organic-matter supply to the continental margin, boosting food supply to the CWCs.