A review of MIS 5e sea-level proxies around Japan

Tam, Evan; Yokoyama, Yusuke

doi:https://doi.org/10.5194/essd-13-1477-2021

Articles | Volume 13, issue 4

https://doi.org/10.5194/essd-13-1477-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

WALIS – the World Atlas of Last Interglacial...

https://doi.org/10.5194/essd-13-1477-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 13, issue 4

Data description paper

|

06 Apr 2021

Data description paper |

| 06 Apr 2021

A review of MIS 5e sea-level proxies around Japan

Evan Tam and Yusuke Yokoyama

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Final revised paper (published on 06 Apr 2021)
Supplement to the final revised paper
Preprint (discussion started on 14 Dec 2020)
Supplement to the preprint

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

RC1: 'review', Thomas M. Cronin, 23 Dec 2020
- AC1: 'Reply on RC1', Evan Tam, 02 Feb 2021
RC2: 'Referee comment', Luigi Ferranti, 13 Jan 2021
- AC2: 'Reply on RC2', Evan Tam, 02 Feb 2021

Peer-review completion

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

AR by Evan Tam on behalf of the Authors (13 Feb 2021) Author's response Manuscript

ED: Publish as is (19 Feb 2021) by Colin V. Murray-Wallace

AR by Evan Tam on behalf of the Authors (02 Mar 2021) Manuscript

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Short summary

Changes in sea level during Marine Isotope Stage (MIS) 5e are comparable to modern sea levels in our global climate. Contributing to the World Atlas of Last Interglacial Shorelines (WALIS), this paper reviewed data from over 70 studies detailing sea-level markers for MIS 5e around Japan. Most sea-level markers were found as marine terraces and are often dated by comparison to dated volcanic ash or sediment layers, which has connected Japan’s landforms to global patterns of sea-level change.