@article{
 title = {Sea-surface temperature from coral skeletal strontium/calcium ratios.},
 type = {article},
 year = {1992},
 identifiers = {[object Object]},
 pages = {644-7},
 volume = {257},
 websites = {http://www.ncbi.nlm.nih.gov/pubmed/17740731},
 month = {7},
 day = {31},
 id = {22c90ac1-e76b-3e1a-aed7-cd81a115e295},
 created = {2012-12-06T09:09:03.000Z},
 file_attached = {true},
 profile_id = {0b777e31-8c9d-39dd-97a3-3e054bd99cfe},
 group_id = {764582e8-5773-3a66-8d6b-9b40e4fb5a88},
 last_modified = {2017-03-14T17:27:14.020Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Beck1992},
 abstract = {Seasonal records of tropical sea-surface temperature (SST) over the past 10(5) years can be recovered from high-precision measurements of coral strontium/calcium ratios with the use of thermal ionization mass spectrometry. The temperature dependence of these ratios was calibrated with corals collected at SST recording stations and by (18)O/(16)O thermometry. The results suggest that mean monthly SST may be determined with an apparent accuracy of better than 0.5 degrees C. Measurements on a fossil coral indicate that 10,200 years ago mean annual SSTs near Vanuatu in the southwestern Pacific Ocean were about 5 degrees C colder than today and that seasonal variations in SST were larger. These data suggest that tropical climate zones were compressed toward the equator during deglaciation.},
 bibtype = {article},
 author = {Beck, J W and Edwards, R L and Ito, E and Taylor, F W and Recy, J and Rougerie, F and Joannot, P and Henin, C},
 journal = {Science (New York, N.Y.)},
 number = {5070}
}

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