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Author Topic: Greenland really was green, world's oldest DNA reveals  (Read 125 times)
Description: DNA hints warm era didn't melt entire cap
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Solomon
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« on: July 07, 2007, 11:05:23 AM »


Depiction of Greenland half a million years ago

Scientists using DNA extracted from ice buried deep below the surface have found evidence that a lush forest once existed in southern Greenland, a finding that sheds light on how climate change affects Earth's frozen areas.

The researchers analyzed ice cores 2-3 km below the surface from several locations in southern Greenland and discovered what they believe to be the oldest authenticated DNA ever recorded.


 > Dye 3: 2km long ice core
 > Greenland Ice Core Project (GRIP): 3km long ice core
 > John Evans Glacier (JEG): Control site
 > Kap Kobenhavn: Previously youngest known Greenland forest


At present, glaciers cover about 10% of Earth's terrestrial surface, but there is only limited knowledge about the biota that occupied these vast areas before the ice formed; most fossil evidence is either deeply hidden or has been scoured away during periods of glacial expansion. Willerslev et al. (p. 111; see the news story by Curry) were able to extract and amplify ancient DNA reproducibly from plants and insect remains from the silty sections of deep ice cores from just above the bedrock. At the time when this ice formed, southern Greenland was covered by a diverse boreal forest consisting of pine, spruce, alder, and yew and inhabited by insects such as butterflies and moths. These results could be indicative of either extensive deglaciation of southern Greenland during the last interglacial (Eemian) or DNA survival over longer time scales of up to 1 million years.

Science 6 July 2007:
Vol. 317. no. 5834, pp. 111 - 114
DOI: 10.1126/science.1141758
Ancient Biomolecules from Deep Ice Cores Reveal a Forested Southern Greenland

Ancient Biomolecules from Deep Ice Cores Reveal a Forested Southern Greenland
Eske Willerslev,1* Enrico Cappellini,2 Wouter Boomsma,3 Rasmus Nielsen,4 Martin B. Hebsgaard,1 Tina B. Brand,1 Michael Hofreiter,5 Michael Bunce,6,7 Hendrik N. Poinar,7 Dorthe Dahl-Jensen,8 Sigfus Johnsen,8 J�rgen Peder Steffensen,8 Ole Bennike,9 Jean-Luc Schwenninger,10 Roger Nathan,10 Simon Armitage,11 Cees-Jan de Hoog,12 Vasily Alfimov,13 Marcus Christl,13 Juerg Beer,14 Raimund Muscheler,15 Joel Barker,16 Martin Sharp,16 Kirsty E. H. Penkman,2 James Haile,17 Pierre Taberlet,18 M. Thomas P. Gilbert,1 Antonella Casoli,19 Elisa Campani,19 Matthew J. Collins2

It is difficult to obtain fossil data from the 10% of Earth's terrestrial surface that is covered by thick glaciers and ice sheets, and hence, knowledge of the paleoenvironments of these regions has remained limited. We show that DNA and amino acids from buried organisms can be recovered from the basal sections of deep ice cores, enabling reconstructions of past flora and fauna. We show that high-altitude southern Greenland, currently lying below more than 2 kilometers of ice, was inhabited by a diverse array of conifer trees and insects within the past million years. The results provide direct evidence in support of a forested southern Greenland and suggest that many deep ice cores may contain genetic records of paleoenvironments in their basal sections.

1 Centre for Ancient Genetics, University of Copenhagen, Denmark.
2 BioArch, Departments of Biology and Archaeology, University of York, UK.
3 Bioinformatics Centre, University of Copenhagen, Denmark.
4 Centre for Comparative Genomics, University of Copenhagen, Denmark.
5 Max Planck Institute for Evolutionary Anthropology, Germany.
6 Murdoch University Ancient DNA Research Laboratory, Murdoch University, Australia.
7 McMaster Ancient DNA Center, McMaster University, Canada.
8 Ice and Climate, University of Copenhagen, Denmark.
9 Geological Survey of Denmark and Greenland, Denmark.
10 Research Laboratory for Archaeology and the History of Art, University of Oxford, UK.
11 Department of Geography, Royal Holloway, University of London, UK.
12 Department of Earth Sciences, University of Oxford, UK.
13 Paul Scherrer Institut (PSI)/Eidgen�ssische Technische Hochschule (ETH) Laboratory for Ion Beam Physics, Institute for Particle Physics, ETH Zurich, Switzerland.
14 Swiss Federal Institute of Aquatic Science and Technology (EAWAG), Switzerland.
15 GeoBiosphere Science Center, Lund University, Sweden.
16 Department of Earth and Atmospheric Sciences, University of Alberta, Canada.
17 Ancient Biomolecules Centre, Oxford University, UK.
18 Laboratoire d'Ecologie Alpine, CNRS Unit� Mixte de Recherche 5553, Universit� Joseph Fourier, Bo�te Postale 53, 38041 Grenoble Cedex 9, France.
19 Dipartimento di Chimica Generale e Inorganica, Universit� di Parma, Italy.

* To whom correspondence should be addressed. E-mail:
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Solomon
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« Reply #1 on: July 13, 2007, 11:30:25 AM »


Scientists analysed the sediment-rich base of the ice cores

Greenland's ancient forests shed light on stability of ice sheet

Contact: Craig Brierley


Wellcome Trust

Ice cores drilled from southern Greenland have revealed the first evidence of a surprisingly lush forest that existed in the region within the past million years. The findings from an international study published today in the journal Science suggest that the southern Greenland ice sheet may be much more stable against rising temperatures than previously thought.

Researchers analysed ice cores from a number of locations in Greenland, including Dye 3 in the south of the country. From the base of the 2km deep Dye 3 core, they were able to extract what they believe is likely to be the oldest authenticated DNA obtained to date.

By analysing these DNA samples, the researchers identified a surprising variety of plant and insect life, including species of trees such as alder, spruce, pine and members of the yew family, as well as invertebrates related to beetles, flies, spiders, butterflies and moths. The researchers believe that the samples date back to between 450,000 and 800,000 years ago.

"We have shown for the first time that southern Greenland, which is currently hidden under more than 2km of ice, was once very different to the Greenland we see today," explains Professor Eske Willerslev, a Wellcome Trust Bioarchaeology Fellow from the University of Copenhagen, who led the study."Back then, it was inhabited by a diverse array of conifer trees and insects."

The research implies that ancient forests covered southern Greenland during a period of increased global temperatures, known as an interglacial period. When temperatures fell again, the area became covered in ice. This ice sheet appears to have remained during the last interglacial period (116,000-130,000 years ago) when the temperature was 5�C warmer than today, contrary to the view currently held by scientists. Professor Dorthe Dahl-Jensen, also at the University of Copenhagen, has shown that in fact, even during this interglacial period, the ice thickness at Dye 3 would have been reduced to between 1 km to 1.5km.

"If our data is correct, then this means that the southern Greenland ice cap is more stable than previously thought," says Professor Willerslev. "This may have implications for how the ice sheets respond to global warming."

However, Professor Willerslev was keen to dismiss the idea that this meant sea levels would not rise to the levels predicted by scientific models.

"We know that during the last interglacial, sea levels rose by 5-6m, but this must have come from other sources additional to the Greenland ice cap, such as Antarctic ice. I would anticipate that as the Earth warms from man-made climate change, these sources would still contribute to a rise in sea levels."

The results also show conclusively that ancient biomolecules from the base of ice cores can be used by scientists to reconstruct the environments hidden underneath ice-covered areas and can yield insights into the climate and the ecology of communities from the distant past.

"Analysing ancient biomolecules from beneath glaciers and ice sheets is challenging due to the very low concentrations, but the information is worth the effort," says Dr Enrico Cappellini, a member of the University of York's new PALAEO Group and another of the paper's co-authors, whose work is supported by the European Commission. "Our study suggests a solution to this problem. Given that ten per cent of the Earth's terrestrial surface is covered by thick ice sheets, it could open up a world of new discoveries."
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