Articles | Volume 14, issue 4
https://doi.org/10.5194/bg-14-885-2017
https://doi.org/10.5194/bg-14-885-2017
Research article
 | 
27 Feb 2017
Research article |  | 27 Feb 2017

Ecological response to collapse of the biological pump following the mass extinction at the Cretaceous–Paleogene boundary

Johan Vellekoop, Lineke Woelders, Sanem Açikalin, Jan Smit, Bas van de Schootbrugge, Ismail Ö. Yilmaz, Henk Brinkhuis, and Robert P. Speijer

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 (05 Oct 2016) by David Gillikin
AR by Johan Vellekoop on behalf of the Authors (18 Oct 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (02 Nov 2016) by David Gillikin
RR by Anonymous Referee #3 (15 Nov 2016)
ED: Reconsider after major revisions (23 Nov 2016) by David Gillikin
AR by Johan Vellekoop on behalf of the Authors (16 Dec 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (28 Dec 2016) by David Gillikin
RR by Peter Roopnarine (26 Jan 2017)
ED: Publish as is (26 Jan 2017) by David Gillikin
AR by Johan Vellekoop on behalf of the Authors (01 Feb 2017)  Manuscript 
Download
Short summary
The Cretaceous–Paleogene boundary, ~ 66 Ma, is characterized by a mass extinction. We studied groups of both surface-dwelling and bottom-dwelling organisms to unravel the oceanographic consequences of these extinctions. Our integrated records indicate that a reduction of the transport of organic matter to the sea floor resulted in enhanced recycling of nutrients in the upper water column and decreased food supply at the sea floor in the first tens of thousands of years after the extinctions.
Altmetrics
Final-revised paper
Preprint