scholarly journals A 200,000-year, high-resolution record of diatom productivity and community makeup from Lake Baikal shows high correspondence to the marine oxygen-isotope record of climate change

2000 ◽  
Vol 45 (4) ◽  
pp. 948-962 ◽  
Author(s):  
Mark B. Edlund ◽  
Eugene F. Stoermer
2000 ◽  
Vol 53 (3) ◽  
pp. 277-284 ◽  
Author(s):  
Minze Stuiver ◽  
Pieter M. Grootes

AbstractThe GISP2 oxygen isotope record, with its high-resolution detail, yields crucial information on past climate change. The glacial δ18O oscillations of the GISP2 core, with their very fast onsets, are templates of a prototype oscillation of variable duration with an amplitude of 3.9‰. The halfway mark of the cold–warm transition is reached in 2 years; the top is reached in 50 years. The δ18O–time gradient of the leading front is about 7.8‰ per 100 yr. After reaching the top, δ18O slowly declines by −0.14‰ per 100 yr. The duration of δ18O decline varies from a couple of centuries for fast oscillations to about 4000 yr for slower ones. The subsequent δ18O downturn during the warm–cold transition has a δ18O–time gradient of −3.2‰ per 100 yr and lasts about 80 yr.


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Vol 278 ◽  
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Author(s):  
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Byron A. Steinman ◽  
Broxton W. Bird ◽  
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Alexandria R. Aspey ◽  
...  

2013 ◽  
Vol 66 ◽  
pp. 45-54 ◽  
Author(s):  
Anson W. Mackay ◽  
George E.A. Swann ◽  
Nathalie Fagel ◽  
Susanne Fietz ◽  
Melanie J. Leng ◽  
...  

PAGES news ◽  
2002 ◽  
Vol 10 (2) ◽  
pp. 7-8 ◽  
Author(s):  
Dominik Fleitmann ◽  
SJ Burns ◽  
M Mudelsee ◽  
U Neff ◽  
J Kramers ◽  
...  

2016 ◽  
Author(s):  
Christopher J. Shea ◽  
◽  
Byron A. Steinman ◽  
Mark B. Abbott ◽  
Lino C. Rauzi

2011 ◽  
Vol 26 (6) ◽  
pp. 627-634 ◽  
Author(s):  
Anson W. Mackay ◽  
George E. A. Swann ◽  
Tim S. Brewer ◽  
Melanie J. Leng ◽  
David W. Morley ◽  
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2016 ◽  
Vol 175 ◽  
pp. 239-251 ◽  
Author(s):  
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Adina Paytan ◽  
Hong Li ◽  
Ulrich G. Wortmann

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