Figure of the fossil ostracod from the Dry Valleys. The specimen is less than 1mm long, but preserves an array of soft tissues including legs and mouth parts. The head end is to the right. The specimen comes from a fossil lake in the Dry Valleys of the Antarctic. The lake sediments have been dated at 14 million years old (Middle Miocene). This is the only fossil of its kind from the Antarctic, and is special from the point of view of fossilization style and for its implications about a warmer tundra climate persisting here in the Miocene. Image Credit: Mark Williams, University of Leicester
Unique fossil discovery shows Antarctic was once much warmer
Rare find has implication for tracking polar ice cap
Issued on 23 July
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A new fossil discovery- the first of its kind from the whole of the Antarctic continent- provides scientists with new evidence to support the theory that the polar region was once much warmer.
The discovery by an international team of scientists is published today (Wednesday 23 July) in Proceedings of the Royal Society B. It involved researchers from the University of Leicester, North Dakota State University, the British Geological Survey, Queen Mary University of London, and Boston University.
The team made a new fossil discovery in the Dry Valleys of the East Antarctic region. The fossils (ostracods) come from an ancient lake - 14 million years old - and are exceptionally well preserved, with all of their soft anatomy in 3-dimensions.
Dr Mark Williams from the Department of Geology, who studied the fossil at Leicester with Professor David Siveter, said: “This is a rare occurrence in the fossil record - but is the first of its kind from the whole of the Antarctic continent.
“Notwithstanding the significance of the fossil preservation, the presence of lake ostracods at this latitude, 77 degrees south, is also of great note. Present conditions in this Antarctic region show mean annual temperatures of minus 25 degrees C. These are impossible conditions to sustain a lake fauna with ostracods.”
“The fossils therefore show that there has been a substantial and very intense cooling of the Antarctic climate after this time interval that is important for tracking the development of the Antarctic icesheet – a key factor in understanding the effects of global warming.
“The fossil ostracods of the Dry Valleys signal a high latitude lake viable for animal colonisation that indicates a dramatic change in the climate of this region, from tundra conditions 14 million years ago, to the intensely cold continental interior climate experienced today.”
The researchers point out that there is no evidence to suggest the fossil discovery points to a once widespread Antarctic lake ostracod fauna: “It is most likely their introduction was by chance, perhaps via birds as dispersal of ostracod eggs attached to the feathers or feet of migratory birds is an important influence on modern ostracod distribution.”
The ostracods were discovered by Richard Thomasson, an undergraduate student, during screening of the sediment in Prof. Allan Ashworth’s lab at North Dakota State University.
The research was funded by NSF grants to Allan Ashworth (at NDSU) and Dave Marchant (at Boston University).
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Mark Williams1,*, David J. Siveter1, Allan C. Ashworth2, Philip R. Wilby3,
David J. Horne4, Adam R. Lewis2 and David R. Marchant5
1Department of Geology, University of Leicester, Leicester LE1 7RH, UK
2Department of Geosciences, North Dakota State University, Stevens Hall, Fargo, ND 58105-5517, USA
3British Geological Survey, Keyworth, Nottingham NG12 5GG, UK
4Department of Geography, Queen Mary, University of London, Mile End Road, London E1 4NS, UK
5Department of Earth Sciences, Boston University, Boston, MA 02215, USA
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