Journal cover Journal topic
The Cryosphere An interactive open-access journal of the European Geosciences Union
doi:10.5194/tc-2016-203
© Author(s) 2016. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
21 Sep 2016
Review status
A revision of this discussion paper was accepted for the journal The Cryosphere (TC) and is expected to appear here in due course.
Could promontories have restricted sea-glacier penetration into marine embayments during Snow ball Earth events?
Adam J. Campbell1,a, Betzalel Massarano1,b, Edwin D. Waddington1, and Stephen G. Warren1,2 1Department of Earth and Space Sciences, University of Washington, Seattle, Washington, USA
2Astrobiology Program, University of Washington, Seattle, Washington, USA
anow at: School of Surveying, University of Otago, Dunedin, New Zealand
bnow at: Pacific Science Center, Seattle, Washington, USA
Abstract. During the Neoproterozoic, Earth experienced several climate excursions of extreme cold, often referred to as the Snowball Earth events. During these periods, thick flowing ice, referred to as sea glaciers, covered the entire planet’s oceans. In addition, there is evidence that photosynthetic eukaryotic algae survived during these periods. With thick sea glaciers covering the oceans, it is uncertain where these organisms survived. One hypothesis is that these algae survived in marine embayments hydrologically connected to the global ocean, where the flow of sea glacier could be resisted. In order for an embayment to act as a refugium, the invading sea glacier must not completely penetrate the embayment. Recent studies have shown that straight-sided, marine embayments could have prevented full sea-glacier penetration under a narrow range of climate conditions suitable for the Snowball Earth events. Here we test whether promontories, i.e. headlands emerging from a side shoreline, could further restrict sea-glacier flow. We use an ice-flow model, suitable for floating ice, to determine the flow of an invading sea glacier. We show that promontories can expand the range of climate conditions allowing refugia by resisting the flow of invading sea glaciers.

Citation: Campbell, A. J., Massarano, B., Waddington, E. D., and Warren, S. G.: Could promontories have restricted sea-glacier penetration into marine embayments during Snow ball Earth events?, The Cryosphere Discuss., doi:10.5194/tc-2016-203, in review, 2016.
Adam J. Campbell et al.
Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'Referee comment', Anonymous Referee #1, 03 Nov 2016 Printer-friendly Version 
AC1: 'Response', Adam Campbell, 15 Mar 2017 Printer-friendly Version 
 
RC2: 'review of tc-2016-203', Stephen Cornford, 29 Nov 2016 Printer-friendly Version 
AC2: 'Response', Adam Campbell, 15 Mar 2017 Printer-friendly Version 
Adam J. Campbell et al.
Adam J. Campbell et al.

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Short summary
How could plant life, that needs light to survive, live on a planet covered with ice? Such a situation is thought to have existed during what are called the Snowball Earth events over 600 million years ago. Here we find that "ice shadows", regions where ice has difficulty flowing into, may have a played a role in that survival of early plant life.
How could plant life, that needs light to survive, live on a planet covered with ice? Such a...
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