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Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?

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An Emerging Paradigm for the UNESCO Global Geoparks: The Ecosystem’s Health Provision

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Far-Field Deformation Resulting from Rheologic Differences Interacting with Tectonic Stresses: An Example from the Pacific/Australian Plate Boundary in Southern New Zealand

By Upton Phaedra   Craw Dave   Walcott Rachel  

Geosciences, Vol. 4, Iss. 3, 2014-07 ,pp. : 93-113

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Development of a Seamless, High-Resolution Bathymetric Model to Compare Reef Morphology around the Subtropical Island Shelves of Lord Howe Island and Balls Pyramid, Southwest Pacific Ocean

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