Loading…

New evidence of Hawaiian coral reef drowning in response to meltwater pulse-1A

Fossil coral reefs are valuable recorders of glacio-eustatic sea-level changes, as they provide key temporal information on deglacial meltwater pulses (MWPs). The timing, rate, magnitude, and meltwater source of these sea-level episodes remain controversial, despite their importance for understandin...

Full description

Saved in:
Bibliographic Details
Published in:Quaternary science reviews 2017-11, Vol.175, p.60-72
Main Authors: Sanborn, Kelsey L., Webster, Jody M., Yokoyama, Yusuke, Dutton, Andrea, Braga, Juan C., Clague, David A., Paduan, Jennifer B., Wagner, Daniel, Rooney, John J., Hansen, John R.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Fossil coral reefs are valuable recorders of glacio-eustatic sea-level changes, as they provide key temporal information on deglacial meltwater pulses (MWPs). The timing, rate, magnitude, and meltwater source of these sea-level episodes remain controversial, despite their importance for understanding ocean-ice sheet dynamics during periods of abrupt climatic change. This study revisits the west coast of the Big Island of Hawaii to investigate the timing of the −150 m H1d terrace drowning off Kawaihae in response to MWP-1A. We present eight new calibrated 14C-AMS ages, which constrain the timing of terrace drowning to at or after 14.75 + 0.33/-0.42 kyr BP, coeval with the age of reef drowning at Kealakekua Bay (U-Th age 14.72 ± 0.10 kyr BP), 70 kms south along the west coast. Integrating the chronology with high-resolution bathymetry and backscatter data, detailed sedimentological analysis, and paleoenvironmental interpretation, we conclude the H1d terrace drowned at the same time along the west coast of Hawaii in response to MWP-1A. The timing of H1d reef drowning is within the reported uncertainty of the timing of MWP-1A interpreted from the IODP Expedition 310 Tahitian reef record. [Display omitted] •−150 m reef terrace H1d is mapped along the west coast of the Big Island of Hawaii.•Sedimentological and geomorphic evidence of coral reef drowning.•New ages constrain the timing of reef drowning to 14.75 + 0.33/−0.42 kyr BP.•Evidence consistent with reef drowning in response to meltwater pulse-1A.
ISSN:0277-3791
1873-457X
DOI:10.1016/j.quascirev.2017.08.022