Sea level changes forced ice breakouts in the Last Glacial cycle: New results from coral terraces

Quaternary Science Reviews

Volumn 21, Issue 10, 2002, Pages 1229-1240

  Chappell, John ^a  

^a AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATE CHANGE; ISOTOPES; OCEANOGRAPHY; SEDIMENTS;

GLACIAL CYCLE;

SEA LEVEL;

CORAL; ICE; ISOTOPIC ANALYSIS; LAST GLACIAL; PALEOCLIMATE; QUATERNARY; SEA LEVEL CHANGE;

PAPUA NEW GUINEA;

ANTHOZOA;

EID: 0036261259     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0277-3791(01)00141-X     Document Type: Article

References (29)

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3. Correlations between climate records from North Atlantic sediments and Greenland ice
4. Computer simulation of reef growth
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8. Coral morphology, diversity, and reef growth
9. Oxygen isotopes and sea level
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13. Deceptively simple models of climatic change
14. Comparison of oxygen isotope records from the GISP-2 and GRIP Greenland ice cores
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16. Response
17. Carbon isotopic evidence for methane hydrate instability during Quaternary interstadials
18. Variations in mode of formation and temperature of oceanic deep waters over the past 125,000 years
19. Holocene coral reef terraces and coscismic uplift of Huon Peninsula, Papua New Guinea
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21. Correlation between climate events in the north Atlantic and China during the last glaciation
22. The 100,000-year cycle identified and found to lag temperature, carbon dioxide and orbital eccentricity
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24. Phase relationships between millenial scale events 64,000 to 24,000 years ago
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26. GSIP2 oxygen isotope ratios
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