Age constraints on surface deformation recorded by fossil shorelines at Cape Range, Western Australia: Reply

Michael R. Sandstrom; Michael J. O’Leary; Milo Barham; Yue Cai; E. Troy Rasbury; Kathleen M. Wooton; Maureen E. Raymo

doi:10.1130/B36330.1

Age constraints on surface deformation recorded by fossil shorelines at Cape Range, Western Australia: Reply

Michael R. Sandstrom, Michael J. O’Leary, Milo Barham, Yue Cai, E. Troy Rasbury, Kathleen M. Wooton, Maureen E. Raymo

School of Earth Sciences

Research output: Contribution to journal › Article › peer-review

Abstract

Whitney et al. (2021) challenge our conclusions about rates of deformation and amount of uplift along the Cape Range, Western Australia, particularly the elevation constraints we place on the last interglacial shoreline along the northern half of Cape Range. They selectively focus almost entirely on the northern half of Cape Range, completely omitting our extensive analysis of the southern section, which provides the bulk of our paleo–sea-level interpretations. They also raise concerns about some of the nomenclature and methodology used.

Original language	English
Pages (from-to)	1621-1624
Number of pages	4
Journal	Bulletin of the Geological Society of America
Volume	134
Issue number	5-6
DOIs	https://doi.org/10.1130/B36330.1
Publication status	Published - May 2022

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10.1130/B36330.1Licence: CC BY

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abstract = "Whitney et al. (2021) challenge our conclusions about rates of deformation and amount of uplift along the Cape Range, Western Australia, particularly the elevation constraints we place on the last interglacial shoreline along the northern half of Cape Range. They selectively focus almost entirely on the northern half of Cape Range, completely omitting our extensive analysis of the southern section, which provides the bulk of our paleo–sea-level interpretations. They also raise concerns about some of the nomenclature and methodology used.",

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Age constraints on surface deformation recorded by fossil shorelines at Cape Range, Western Australia: Reply

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