Sealevel changes control diagenetic dolomite formation in hemipelagic sediments of the Peru Margin

Marine Geology

Volumn 252, Issue 3-4, 2008, Pages 166-173

  Meister, Patrick ^a,b   Bernasconi, Stefano M ^b   Vasconcelos, Crisógono ^b   McKenzie, Judith A ^b  

^a MAX PLANCK INSTITUTE FOR MARINE MICROBIOLOGY   (Germany)

^b GEOLOGICAL INSTITUTE   (Switzerland)

Author keywords

deep biosphere; dolomite; glacial interglacial cycles; oxygen isotopes; paleo temperatures; Peru Margin

Indexed keywords

DIAGENETIC; DOLOMITE FORMATIONS; FRACTIONATION FACTORS; HEMIPELAGIC SEDIMENTS; LOW TEMPERATURE (LTR); OXYGEN-18; SEA LEVEL CHANGES; TEMPERATURE DEPENDENT;

OXYGEN; SEDIMENTATION;

SEDIMENTS;

CONTINENTAL MARGIN; DIAGENESIS; DOLOMITE; POREWATER; PRECIPITATION (CHEMISTRY); SEA LEVEL CHANGE;

PERU; SOUTH AMERICA;

EID: 45049083800     PISSN: 00253227     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.margeo.2008.04.001     Document Type: Article

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