CaltechAUTHORS
  A Caltech Library Service

Precise chronology of the last interglacial period: ^(234)U-^(230)Th data from fossil coral reefs in the Bahamas

Chen, J. H. and Curran, H. A. and White, B. and Wasserburg, G. J. (1991) Precise chronology of the last interglacial period: ^(234)U-^(230)Th data from fossil coral reefs in the Bahamas. Geological Society of America Bulletin, 103 (1). pp. 82-97. ISSN 0016-7606. https://resolver.caltech.edu/CaltechAUTHORS:20131029-154031184

Full text is not posted in this repository. Consult Related URLs below.

Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20131029-154031184

Abstract

A detailed study of ^(238)U-^(234)U-^(230)Th ages was made for different coral species from two Bahamian reefs to determine the time scale of the sea-level high during the last interglacial period, using recently developed mass spectrometric techniques for the measurement of U and Th isotopes. Thirty-seven coral samples were analyzed in replicate. Typical errors at 125 ky are ±1.5 ky (2σ), and 3-ky time intervals appear to be well resolved. This high precision permits detailed chronologic study with time resolution adequate to define stages of the reef's history. These data demonstrate that the time between transgression and regression of the ocean in the last interglacial was about 12 ky, after which sea level fell rapidly at more than ∼2 m/ky. The high sea-level stand began possibly by 132 ky and certainly by 129 ky ago, when sea level reached ∼6 m above present mean low sea level. High sea level was sustained until 120 ky and then fell rapidly. This time period covers the Milankovitch insolation peak at 65°N but is not sharply defined, and the sea-level high lasted from about 4 ky before the insolation peak to 8 ky after it. We find no evidence for a double peak of sea-level rise in the last interglacial episode (that is, high stands at both ∼125 and 142 ky). There appears to be some discrepancy between this precise chronology for a coral reef on a tectonically stable platform and the chronology assigned to deep-sea sediments. The present results show that the duration of the last interglacial led to a 12-ky period of high sea-level stand which is much longer than the insolation peak. The study area consists of two sizeable bank/barrier coral reefs of Sangamon age that crop out along the coast northwest of Cockburn Town on San Salvador Island and at Devil's Point on Great Inagua Island. The initial stage of reef development is not revealed at either site, but the main parts of both reefs are well preserved. At Cockburn Town, the beginning of the reef was marked by colonization of Acropora palmata on hardground areas and possibly other corals at 132 ky ago. Patch reefs at the southeastern flank of the developing reef were growing by 129 to 126 ky ago. By 126 to 123 ky ago, the crest of the reef was formed by the frame-building coral A. palmata, and associated patch reefs flourished along its flanks. A. palmata coral heads grew upward to a mean low sea level ∼6 m above the present one. The reef began to decline as sea level dropped at about 123 to 120 ky ago. Near two measured profiles at Devil's Point, the top of a rubblestone, dominated by A. cervicornis, and patch-reef corals preserved in growth position have been beveled off and represent an ancient wave-cut surface. ^(230)Th ages on corals below and above this surface indicate that it was cut at about 125 ± 1 ky ago.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1130/0016-7606(1991)103<0082:PCOTLI>2.3.CO;2DOIArticle
http://gsabulletin.gsapubs.org/content/103/1/82.abstractPublisherArticle
http://bulletin.geoscienceworld.org/content/103/1/82PublisherArticle
Additional Information:© 1991 Geological Society of America. Manuscript received by the Society January 17, 1990. Revised Manuscript received June 19, 1990. Manuscript Accepted June 25, 1990. We are grateful to Dr. Donald T. Gerace, director of the Bahamian Field Station, for providing accommodations and transportation for field work on San Salvador Island. We are particularly grateful to A. G. Sylvester (editor), J. T. Hollin, R. L. Edwards, and an anonymous reviewer for constructive suggestions. Philosophical and technical advice from D. A. Papanastassiou is gratefully acknowledged. Funding of this work was partially supported by National Science Foundation Grant OCE87-21774 to Wasserburg and Chen. Petroleum Research Fund grants from the American Chemical Society to both Curran and White partially supported field work for this study.
Funders:
Funding AgencyGrant Number
NSFOCE87-21774
American Chemical Society Petroleum Research FundUNSPECIFIED
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological and Planetary Sciences 4819
Lunatic Asylum Lab652
Issue or Number:1
Record Number:CaltechAUTHORS:20131029-154031184
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20131029-154031184
Official Citation: J. H. CHEN, H. A. CURRAN, B. WHITE, and G. J. WASSERBURG Precise chronology of the last interglacial period: 234U-230Th data from fossil coral reefs in the Bahamas Geological Society of America Bulletin, January, 1991, v. 103, no. 1, p. 82-97, doi:10.1130/0016-7606(1991)103<0082:PCOTLI>2.3.CO;2
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:42126
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:30 Oct 2013 18:41
Last Modified:03 Oct 2019 05:55

Repository Staff Only: item control page