Letter. Late cretaceous seasonal ocean variability from the arctic

Davies, Andrew, Kemp, Alan E.S. and Pike, Jennifer (2009) Letter. Late cretaceous seasonal ocean variability from the arctic Nature, 460, pp. 254-258. (doi:10.1038/nature08141).


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The modern Arctic Ocean is regarded as barometer of global change and amplifier of global warming1 and therefore records of past Arctic change are of a premium for palaeoclimate reconstruction. Little is known of the state of the Arctic Ocean in the greenhouse period of the late Cretaceous, yet records from such times may yield important clues to its future behaviour given current global warming trends. Here we present the first seasonally resolved sedimentary record from the Cretaceous from the Alpha Ridge of the Arctic Ocean. This “paleo-sediment trap” provides new insights into the workings of the Cretaceous marine biological carbon pump. Seasonal primary production was dominated by diatom algae but was not related to upwelling as previously hypothesised. Rather, production occurred within a stratified water column, involving specially adapted species in blooms resembling those of the modern North Pacific Subtropical Gyre, or those indicated for the Mediterranean sapropels. With increased CO2 levels and warming currently driving increased stratification in the global ocean, this style of production that is adapted to stratification may become more widespread. Our evidence for seasonal diatom production and flux testify to an ice-free summer, but thin accumulations of terrigenous sediment within the diatom ooze are consistent with the presence of intermittent sea ice in the winter, supporting a wide body of evidence for low temperatures in the Late Cretaceous Arctic Ocean, rather than recent suggestions of a 15 °C mean annual temperature at this time.

Item Type: Article
Digital Object Identifier (DOI): doi:10.1038/nature08141
ISSNs: 0028-0836 (print)
ePrint ID: 148555
Date :
Date Event
9 July 2009Published
Date Deposited: 19 May 2010 10:48
Last Modified: 18 Apr 2017 14:33
Further Information:Google Scholar
URI: http://eprints.soton.ac.uk/id/eprint/148555

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