17731593

Source:http://linkedlifedata.com/resource/pubmed/id/17731593

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Predicate	Object
rdf:type	pubmed:Citation
lifeskim:mentions	umls-concept:C0024467, umls-concept:C0205686, umls-concept:C0719712
pubmed:issue	3938
pubmed:dateCreated	2010-6-7
pubmed:abstractText	The high-magnesian calcite fraction of a shallow-water carbonate sand was converted to low-magnesian calcite after transport to the deep sea; strontium was also leached from the carbonate. Oxygen isotopic ratios indicate that loss of magnesium and strontium took place during recrystallization of the carbonate in the deep sea; this process did not alter textures of skeletal fragments. Previously, high-magnesian, calcite was thought only to dissolve in the deep sea.
pubmed:language	eng
pubmed:journal	http://linkedlifedata.com/resource/pubmed/journal/0404511
pubmed:status	PubMed-not-MEDLINE
pubmed:month	Jun
pubmed:issn	0036-8075
pubmed:author	pubmed-author:BonattiEE, pubmed-author:GombergD NDN
pubmed:issnType	Print
pubmed:day	19
pubmed:volume	168
pubmed:owner	NLM
pubmed:authorsComplete	Y
pubmed:pagination	1451-3
pubmed:year	1970
pubmed:articleTitle	High-magnesian calcite: leaching of magnesium in the deep sea.
pubmed:publicationType	Journal Article