Marine Isotope Stage 13

5 million year history, representing the Lisiecki and Raymo (2005) LR04 Benthic Stack

Marine Isotope Stage 13 or MIS 13 is a Marine isotope stage in the geologic temperature record, in Britain covering the Cromerian interglacial period between ~524,000 and 474,000 years ago. It is split into three substages, MIS 13a MIS 13b, and MIS 13c. Some records indicate that MIS 13a was an unstable warm peak with a cold split in the middle at MIS 13.12 - separating warm MIS 13.11 and 13.13[1]

Sites

Britain

High Lodge, Suffolk

Waverley Wood, Warwickshire

Happisburgh 1, Norfolk

Boxgrove, West Sussex

Ecology

Flora

Early domination of birch, pine, and spruce. Mixed-oak forests follow (predominantly Alder, Oak, Hornbeam, and Hazel).

Fauna

Mammals

BinomialCommon nameDirection
Erinaceus sp.Hedgehog?
Sorex minutusPygmy shrew?
Sorex runtonensis †?
Sorex savini †?
Neomys sp.Water shrew?
Talpa europaeaCommon mole?
Talpa minor †Pygmy mole?
Homo sp.Hominid?
Lepus timidusMountain hare?
Oryctolagus cuniculusCommon European rabbit?
Plecotus auritusLong-eared bat?
Myotis mystacinusWhiskered bat?
Myotis bechsteiniBechstein's bat?
Scuirus sp.Squirrel?
Canis lupusWolf?
Ursus deningeri †Bear?

[2]

References

  1. Bassinot, Franck C.; Labeyrie, Laurent D.; Vincent, Edith; Quidelleur, Xavier; Shackleton, Nicholas J.; Lancelot, Yves (1994). "The astronomical theory of climate and the age of the Brunhes-Matuyama magnetic reversal". Earth and Planetary Science Letters. 1 (126): 103. Bibcode:1994E&PSL.126...91B. doi:10.1016/0012-821x(94)90244-5.
  2. Pettitt, Paul; White, Mark (2012). The British Palaeolithic. Routledge. p. 65. ISBN 978-0-415-67455-3.


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