Orbital-scale climate change and glacioeustasy during the early late ordovician (pre-Hirnantian) determined from δ18O values in marine apatite

Geology

Volumn 41, Issue 7, 2013, Pages 775-778

  Elrick, M ^a   Reardon, D ^a   Labor, W ^a   Martin, J ^a   Desrochers, A ^b   Pope, M ^c  

^a UNIVERSITY OF NEW MEXICO   (United States)

^b UNIVERSITY OF OTTAWA   (Canada)

^c TEXAS A AND M UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATIC FLUCTUATIONS; GLACIAL STAGES; ISOTOPIC VALUES; LATE ORDOVICIAN; SEA SURFACE TEMPERATURES; SEALEVEL CHANGE; SEDIMENTARY CYCLES; SHALLOW-WATER;

APATITE; ATMOSPHERIC TEMPERATURE; GLACIAL GEOLOGY; PHASE TRANSITIONS;

CLIMATE CHANGE;

APATITE; CLIMATE VARIATION; CONODONT; GLACIATION; GLACIER DYNAMICS; GLACIOEUSTACY; GREENHOUSE EFFECT; HIRNANTIAN; HYPOTHESIS TESTING; OXYGEN ISOTOPE; PALEOCLIMATE; SEA SURFACE TEMPERATURE;

EID: 84880323316     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/G34363.1     Document Type: Article

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