Nature, Volume 434 |
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Page 64
temperature change between glacial and interglacial climates in the subtropics15,16 . Furthermore , the colder temperatures ... We conclude that d13 of speleothem BT2 primarily reflects changes in d13O of regional precipitation . 18 .
temperature change between glacial and interglacial climates in the subtropics15,16 . Furthermore , the colder temperatures ... We conclude that d13 of speleothem BT2 primarily reflects changes in d13O of regional precipitation . 18 .
Page 496
Moreover , facies changes cannot explain the observed variation ; although proposed water - column deepenings at beds 24e , 25 and 28 ( refs . 11-13 ) do coincide with 2 - MHP minima , the maxima in 2 - MHP indices are not associated ...
Moreover , facies changes cannot explain the observed variation ; although proposed water - column deepenings at beds 24e , 25 and 28 ( refs . 11-13 ) do coincide with 2 - MHP minima , the maxima in 2 - MHP indices are not associated ...
Page 831
this variability might affect the fraction . of climate change attributable to various causes , particularly with regard to the hydrological cycle . But it seems unlikely that the simulated changes would be quantitatively consistent ...
this variability might affect the fraction . of climate change attributable to various causes , particularly with regard to the hydrological cycle . But it seems unlikely that the simulated changes would be quantitatively consistent ...
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Contents
eating at heart p | 37 |
letters to nature | 50 |
Mesozoic Alpine facies deposition as a result | 59 |
16 other sections not shown
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Bibliographic information
| Title | Nature, Volume 434 |
| Editor | Sir Norman Lockyer |
| Publisher | Macmillan Journals Limited, 2005 |
| Original from | University of Illinois at Urbana-Champaign |
| Digitized | 25 Nov 2019 |
| Export Citation | BiBTeX EndNote RefMan |