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Toomey, Michael, Ashton, Andrew D., Perron, J. Taylor (2013) Profiles of ocean island coral reefs controlled by sea-level history and carbonate accumulation rates. Geology, 41 (7) 731-734 doi:10.1130/g34109.1

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Reference TypeJournal (article/letter/editorial)
TitleProfiles of ocean island coral reefs controlled by sea-level history and carbonate accumulation rates
JournalGeology
AuthorsToomey, MichaelAuthor
Ashton, Andrew D.Author
Perron, J. TaylorAuthor
Year2013 (July)Volume41
Issue7
PublisherGeological Society of America
DOIdoi:10.1130/g34109.1Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID142110Long-form Identifiermindat:1:5:142110:5
GUID0
Full ReferenceToomey, Michael, Ashton, Andrew D., Perron, J. Taylor (2013) Profiles of ocean island coral reefs controlled by sea-level history and carbonate accumulation rates. Geology, 41 (7) 731-734 doi:10.1130/g34109.1
Plain TextToomey, Michael, Ashton, Andrew D., Perron, J. Taylor (2013) Profiles of ocean island coral reefs controlled by sea-level history and carbonate accumulation rates. Geology, 41 (7) 731-734 doi:10.1130/g34109.1
In(2013, July) Geology Vol. 41 (7) Geological Society of America

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Toomey, Michael R., Ashton, Andrew D., Raymo, Maureen E., Perron, J. Taylor (2017) Reply to: Terry, J. and Goff, J. comment on “Late Cenozoic sea level and the rise of modern rimmed atolls” by Toomey et al. (2016), Palaeogeography, Palaeoclimatology, Palaeoecology 4 51: 73–83. Palaeogeography, Palaeoclimatology, Palaeoecology, 469. 159-160 doi:10.1016/j.palaeo.2016.11.028
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Woodroffe, Colin D., Webster, Jody M. (2014) Coral reefs and sea-level change. Marine Geology, 352. 248-267 doi:10.1016/j.margeo.2013.12.006
Krug, A. Z., Jablonski, D. (2012) Long-term origination rates are reset only at mass extinctions. Geology, 40 (8) 731-734 doi:10.1130/g33091.1
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Kench, Paul S., Ford, Murray R., Bramante, James F., Ashton, Andrew D., Donnelly, Jeffrey P., Sullivan, Richard M., Toomey, Michael R. (2022) Heightened storm activity drives late Holocene reef island formation in the central Pacific Ocean. Global and Planetary Change, 215. 103888 doi:10.1016/j.gloplacha.2022.103888
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