@article{bernard_burial-induced_2017,
	title = {Burial-induced oxygen-isotope re-equilibration of fossil foraminifera explains ocean paleotemperature paradoxes},
	volume = {8},
	copyright = {2017 The Author(s)},
	issn = {2041-1723},
	url = {https://www.nature.com/articles/s41467-017-01225-9},
	doi = {10.1038/s41467-017-01225-9},
	abstract = {{\textless}p{\textgreater}The oxygen-isotope composition of fossil foraminifera tests is an established proxy for ocean paleotemperatures. Here, the authors show that isotope re-equilibration can occur during sediment burial without structural modification of the tests and cause a substantial overestimation of ocean paleotemperatures.{\textless}/p{\textgreater}},
	language = {En},
	number = {1},
	urldate = {2017-10-30},
	journal = {Nature Communications},
	author = {Bernard, S. and Daval, D. and Ackerer, P. and Pont, S. and Meibom, A.},
	month = oct,
	year = {2017},
	note = {00000},
	keywords = {boundaries, collapse, climate, oceans},
	pages = {1134},
	file = {Bernard et al. - 2017 - Burial-induced oxygen-isotope re-equilibration of .pdf:C\:\\Users\\rsrs\\Documents\\Zotero Database\\storage\\SG4RUHXM\\Bernard et al. - 2017 - Burial-induced oxygen-isotope re-equilibration of .pdf:application/pdf}
}

{"_id":"bddHu6JPhm4XDjvHj","bibbaseid":"bernard-daval-ackerer-pont-meibom-burialinducedoxygenisotopereequilibrationoffossilforaminiferaexplainsoceanpaleotemperatureparadoxes-2017","authorIDs":[],"author_short":["Bernard, S.","Daval, D.","Ackerer, P.","Pont, S.","Meibom, A."],"bibdata":{"bibtype":"article","type":"article","title":"Burial-induced oxygen-isotope re-equilibration of fossil foraminifera explains ocean paleotemperature paradoxes","volume":"8","copyright":"2017 The Author(s)","issn":"2041-1723","url":"https://www.nature.com/articles/s41467-017-01225-9","doi":"10.1038/s41467-017-01225-9","abstract":"\\textlessp\\textgreaterThe oxygen-isotope composition of fossil foraminifera tests is an established proxy for ocean paleotemperatures. Here, the authors show that isotope re-equilibration can occur during sediment burial without structural modification of the tests and cause a substantial overestimation of ocean paleotemperatures.\\textless/p\\textgreater","language":"En","number":"1","urldate":"2017-10-30","journal":"Nature Communications","author":[{"propositions":[],"lastnames":["Bernard"],"firstnames":["S."],"suffixes":[]},{"propositions":[],"lastnames":["Daval"],"firstnames":["D."],"suffixes":[]},{"propositions":[],"lastnames":["Ackerer"],"firstnames":["P."],"suffixes":[]},{"propositions":[],"lastnames":["Pont"],"firstnames":["S."],"suffixes":[]},{"propositions":[],"lastnames":["Meibom"],"firstnames":["A."],"suffixes":[]}],"month":"October","year":"2017","note":"00000","keywords":"boundaries, collapse, climate, oceans","pages":"1134","file":"Bernard et al. - 2017 - Burial-induced oxygen-isotope re-equilibration of .pdf:C\\:\\\\Users\\s̊rs\\\\Documents\\\\Zotero Database\\\\storage\\\\SG4RUHXM\\\\Bernard et al. - 2017 - Burial-induced oxygen-isotope re-equilibration of .pdf:application/pdf","bibtex":"@article{bernard_burial-induced_2017,\n\ttitle = {Burial-induced oxygen-isotope re-equilibration of fossil foraminifera explains ocean paleotemperature paradoxes},\n\tvolume = {8},\n\tcopyright = {2017 The Author(s)},\n\tissn = {2041-1723},\n\turl = {https://www.nature.com/articles/s41467-017-01225-9},\n\tdoi = {10.1038/s41467-017-01225-9},\n\tabstract = {{\\textless}p{\\textgreater}The oxygen-isotope composition of fossil foraminifera tests is an established proxy for ocean paleotemperatures. Here, the authors show that isotope re-equilibration can occur during sediment burial without structural modification of the tests and cause a substantial overestimation of ocean paleotemperatures.{\\textless}/p{\\textgreater}},\n\tlanguage = {En},\n\tnumber = {1},\n\turldate = {2017-10-30},\n\tjournal = {Nature Communications},\n\tauthor = {Bernard, S. and Daval, D. and Ackerer, P. and Pont, S. and Meibom, A.},\n\tmonth = oct,\n\tyear = {2017},\n\tnote = {00000},\n\tkeywords = {boundaries, collapse, climate, oceans},\n\tpages = {1134},\n\tfile = {Bernard et al. - 2017 - Burial-induced oxygen-isotope re-equilibration of .pdf:C\\:\\\\Users\\\\rsrs\\\\Documents\\\\Zotero Database\\\\storage\\\\SG4RUHXM\\\\Bernard et al. - 2017 - Burial-induced oxygen-isotope re-equilibration of .pdf:application/pdf}\n}\n\n","author_short":["Bernard, S.","Daval, D.","Ackerer, P.","Pont, S.","Meibom, A."],"key":"bernard_burial-induced_2017","id":"bernard_burial-induced_2017","bibbaseid":"bernard-daval-ackerer-pont-meibom-burialinducedoxygenisotopereequilibrationoffossilforaminiferaexplainsoceanpaleotemperatureparadoxes-2017","role":"author","urls":{"Paper":"https://www.nature.com/articles/s41467-017-01225-9"},"keyword":["boundaries","collapse","climate","oceans"],"downloads":0,"html":""},"bibtype":"article","biburl":"http://www.collapsologie.fr/bib.bib","creationDate":"2019-06-13T15:56:08.735Z","downloads":0,"keywords":["boundaries","collapse","climate","oceans"],"search_terms":["burial","induced","oxygen","isotope","equilibration","fossil","foraminifera","explains","ocean","paleotemperature","paradoxes","bernard","daval","ackerer","pont","meibom"],"title":"Burial-induced oxygen-isotope re-equilibration of fossil foraminifera explains ocean paleotemperature paradoxes","year":2017,"dataSources":["97shAbFSxL7A7SHoh"]}