The mystery of the missing deglacial carbonate preservation maximum

Quaternary Science Reviews

Volumn 39, Issue , 2012, Pages 60-72

  Mekik, Figen A ^a   Anderson, Robert F ^b   Loubere, Paul ^c   François, Roger ^d   Richaud, Mathieu ^e  

^a GRAND VALLEY STATE UNIVERSITY   (United States)

^b International Research Institute for Climate and Society   (United States)

^c NORTHERN ILLINOIS UNIVERSITY   (United States)

^d UNIVERSITY OF BRITISH COLUMBIA   (Canada)

^e CALIFORNIA STATE UNIVERSITY   (United States)

Author keywords

Calcite preservation; Deglaciation; Organic carbon to calcite rain ratio; Sediment focusing

Indexed keywords

ACCUMULATION RATES; ANTARCTIC BOTTOM WATER; ATMOSPHERIC CO; BIOTURBATION; DEEP SEA SEDIMENT; DEEP WATER; DEEP WATER MASS; DEGLACIAL; DEGLACIATIONS; DISSOLVED INORGANIC CARBON; EASTERN EQUATORIAL PACIFIC; EQUATORIAL PACIFIC; FRAGMENTATION INDEX; GLACIAL PERIOD; INDIAN OCEAN; INTERMEDIATE DEPTHS; MULTI PROXIES; OCEAN STRATIFICATION; PROXY RECORDS; SEDIMENTATION RATES;

ANOXIC SEDIMENTS; CALCITE; CARBON DIOXIDE; CARBONATE MINERALS; GLACIAL GEOLOGY; SEDIMENTATION;

CALCIUM CARBONATE;

ACCUMULATION RATE; ANTARCTIC BOTTOM WATER; BIOTURBATION; CALCITE; CARBON DIOXIDE; CARBONATE; CORE ANALYSIS; DEGLACIATION; DISSOLVED INORGANIC CARBON; FORAMINIFERA; PALEOCEANOGRAPHY; PRESERVATION; STRATIFICATION; WATER MASS;

ATLANTIC OCEAN; PACIFIC OCEAN;

FORAMINIFERA; GLOBOROTALIA MENARDII;

EID: 84863410295     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2012.01.024     Document Type: Article

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