Articles | Volume 14, issue 3
https://doi.org/10.5194/cp-14-321-2018
https://doi.org/10.5194/cp-14-321-2018
Research article
 | 
08 Mar 2018
Research article |  | 08 Mar 2018

Reinforcing the North Atlantic backbone: revision and extension of the composite splice at ODP Site 982

Anna Joy Drury, Thomas Westerhold, David Hodell, and Ursula Röhl

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: Publish subject to minor revisions (review by editor) (08 Dec 2017) by Pierre Francus
AR by Anna Joy Drury on behalf of the Authors (30 Dec 2017)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (17 Jan 2018) by Pierre Francus
AR by Anna Joy Drury on behalf of the Authors (18 Jan 2018)  Manuscript 
ED: Publish as is (19 Jan 2018) by Pierre Francus
AR by Anna Joy Drury on behalf of the Authors (23 Jan 2018)
Download
Short summary
North Atlantic Site 982 is key to our understanding of climate evolution over the past 12 million years. However, the stratigraphy and age model are unverified. We verify the composite splice using XRF core scanning data and establish a revised benthic foraminiferal stable isotope astrochronology from 8.0–4.5 million years ago. Our new stratigraphy accurately correlates the Atlantic and the Mediterranean and suggests a connection between late Miocene cooling and dynamic ice sheet expansion.