CaltechAUTHORS
  A Caltech Library Service

Eustasy as a test of a Cretaceous superplume hypothesis

Hardebeck, Jeanne and Anderson, Don L. (1996) Eustasy as a test of a Cretaceous superplume hypothesis. Earth and Planetary Science Letters, 137 (1-4). pp. 101-108. ISSN 0012-821X. http://resolver.caltech.edu/CaltechAUTHORS:20121005-113037500

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

Use this Persistent URL to link to this item: http://resolver.caltech.edu/CaltechAUTHORS:20121005-113037500

Abstract

The mantle plume model has been used to explain a variety of geological and geodynamic events. For instance, a large plume, or ‘superplume’, under the Pacific basin has been proposed to account for a number of Cretaceous events, such as a global sealevel rise, an increase in global average temperature, and a pause in the reversals of the Earth's magnetic field [1,2]. The primary evidence for this hypothesis is a model for the rate of production of ocean ridge material and ocean plateaus, with a high from about 120-80 Ma, mostly due to activity in the Pacific basin, which is claimed to have been driven by the upwelling of a large plume from the core-mantle boundary. The hypothesis requires that a large part of the primary evidence for this high productivity has disappeared by subduction. Here, we test this hypothesis by comparing the Cretaceous eustatic sealevel highstand which would result from the superplume model with generally accepted values. Our model includes estimates of eustatic sealevel change resulting from phenomena explicitly specified for the proposed plume, such as the volume of ocean crust produced and the extent of lithospheric swelling associated with the plume head, as well as other events known to affect eustatic sealevel, such as glaciation and continental collision. The estimated Cretaceous highstand resulting from all the modeled effects is 220–470 m, compared to the observed value of 120–200 m. This discrepancy indicates a probable overestimate of the rate of seafloor and plateau creation and of the size of plume that could have existed. The breakup of the Pangean supercontinent is a more viable explanation of the Cretaceous sealevel rise.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/0012-821X(95)00222-XDOIUNSPECIFIED
http://www.sciencedirect.com/science/article/pii/0012821X9500222XPublisherUNSPECIFIED
Additional Information:© 1996 Elsevier Science B.V. Received 14 August 1995; accepted 16 November 1995. We thank Michael Gurnis, Paul Heller and Peter Burgess for their helpful comments and suggestions. This research was supported by NSF Grant EAR 92-18390. Contribution No. 5587, Division of Geological and Planetary Sciences, Caltech. [MK]
Funders:
Funding AgencyGrant Number
NSFEAR92-18390
Subject Keywords:Cretaceous; superplumes; eustacy
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological and Planetary Sciences5587
Record Number:CaltechAUTHORS:20121005-113037500
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20121005-113037500
Official Citation:Jeanne Hardebeck, Don L. Anderson, Eustasy as a test of a Cretaceous superplume hypothesis, Earth and Planetary Science Letters, Volume 137, Issues 1–4, January 1996, Pages 101-108, ISSN 0012-821X, 10.1016/0012-821X(95)00222-X. (http://www.sciencedirect.com/science/article/pii/0012821X9500222X)
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:34713
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:05 Oct 2012 18:54
Last Modified:05 Oct 2012 18:54

Repository Staff Only: item control page