in their response, attempt to refute our conclusions and claim the deposits to be the result of a +21 m eustatic sea level highstand during marine isotope stage (MIS) 11. (deepdyve.com)
The authors found three main highstand phases, which occurred at about 3250 — 3000, 2600 — 950 and 650 — 160 cal yrs BP, respectively. (kaltesonne.de)
Mitrovica, J. X. & Milne, G. A. On the origin of late Holocene sea - level highstands within equatorial ocean basins. (nature.com)