Science, Volume 293John Michels (Journalist) American Association for the Advancement of Science, 2001 |
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Page 92
... Present address : Department of Biogeochemsitry , Max Planck Institute for Marine Microbiology , Celci- usstrasse 1 , Bremen , 28359 Germany . + Present address : Department of Analytical and Ap- plied Spectroscopy , Vrije Universiteit ...
... Present address : Department of Biogeochemsitry , Max Planck Institute for Marine Microbiology , Celci- usstrasse 1 , Bremen , 28359 Germany . + Present address : Department of Analytical and Ap- plied Spectroscopy , Vrije Universiteit ...
Page 94
... present in the sediment ( 22 ) , ev- idence for a substantial ( > 10 % ) prokaryotic contribution to Phanerozoic OC - rich sedi- ments is generally lacking ( 23 ) . Therefore , the abundance of OM derived from archaea during OAElb is ...
... present in the sediment ( 22 ) , ev- idence for a substantial ( > 10 % ) prokaryotic contribution to Phanerozoic OC - rich sedi- ments is generally lacking ( 23 ) . Therefore , the abundance of OM derived from archaea during OAElb is ...
Page 676
... present , these results suggest that the octahedral tilt ( Fig . 1 ) is large enough to accommodate local distortions , thus effectively decoupling the ferroelectric order parameter and the crystal structure . Then , given the bcc ...
... present , these results suggest that the octahedral tilt ( Fig . 1 ) is large enough to accommodate local distortions , thus effectively decoupling the ferroelectric order parameter and the crystal structure . Then , given the bcc ...
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