Show simple item record

FieldValueLanguage
dc.contributor.authorSanborn, Kelsey L.
dc.contributor.authorWebster, Jody Michael
dc.contributor.authorYokoyama, Yusuke
dc.contributor.authorDutton, Andrea
dc.contributor.authorBraga, Juan C
dc.contributor.authorClague, David A
dc.contributor.authorPaduan, Jennifer B
dc.contributor.authorWagner, Daniel
dc.contributor.authorRooney, John J.B
dc.contributor.authorHansen, John R
dc.date.accessioned2020-01-31
dc.date.available2020-01-31
dc.date.issued2017-11-01
dc.identifier.citationSanborn, K. L., Webster, J. M., Yokoyama, Y., Dutton, A., Braga, J. C., Clague, D. A., … Hansen, J. R. (2017). New evidence of Hawaiian coral reef drowning in response to meltwater pulse-1A. Quaternary Science Reviews, 175, 60–72. https://doi.org/10.1016/j.quascirev.2017.08.022en
dc.identifier.issn02773791
dc.identifier.urihttps://hdl.handle.net/2123/21764
dc.descriptionThe paper is dedicated to the memory of John Rooney. This research was supported by grants from the Australian Research Council ( DP1094001, DP120101793 ), the NSF-OCE ( 1559040 to Andrea Dutton), and JSPS KAKENHI ( JP15KK0151 and 17H01168 ).en
dc.description.abstractFossil 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. © 2017 Elsevier Ltden
dc.description.sponsorshipAustralian Research Council-DP1094001, DP120101793, NSF-OCE-1559040, and Japan Society for the Promotion of -JP15KK0151 and 17H01168en
dc.language.isoen_AUen
dc.publisherElsevieren
dc.relationJapan Society for the Promotion of Science-17H01168,JP15KK0151, Australian Research Council-DP1094001,DP120101793, NSF-OCE- 1559040en
dc.rightsOtheren
dc.subjectCoastalen
dc.subjectCoral reef drowningen
dc.subjectDeglaciationen
dc.subjectGeomorphologyen
dc.subjectHawaiien
dc.subjectLate pleistoceneen
dc.subjectMeltwater Pulse-1Aen
dc.subjectSea-level changesen
dc.subjectSubmerged terracesen
dc.titleNew evidence of Hawaiian coral reef drowning in response to meltwater pulse-1Aen
dc.typeArticleen
dc.subject.asrc040305en
dc.identifier.doi10.1016/j.quascirev.2017.08.022
dc.type.pubtypeAuthor accepted manuscripten
dc.relation.arcDP1094001
dc.relation.arcDP120101793
usyd.facultySeS faculties schools::Faculty of Scienceen


Show simple item record

Associated file/s

Associated collections

Show simple item record

There are no previous versions of the item available.