C
Clark Sherman
Researcher at University of Puerto Rico at Mayagüez
Publications - 25
Citations - 780
Clark Sherman is an academic researcher from University of Puerto Rico at Mayagüez. The author has contributed to research in topics: Reef & Coral reef. The author has an hindex of 13, co-authored 25 publications receiving 713 citations. Previous affiliations of Clark Sherman include University of Hawaii at Manoa & University of Hawaii.
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Journal ArticleDOI
Geomorphology of mesophotic coral ecosystems: current perspectives on morphology, distribution, and mapping strategies
Stanley D. Locker,Roy A. Armstrong,T. A. Battista,John J. B. Rooney,Clark Sherman,David G. Zawada +5 more
TL;DR: A general review of the distribution of mesophotic coral ecosystems (MCEs) in relationship to geomorphology in US waters is presented in this paper. But, the work in this paper is concerned with the depth range of 30-100 m, where more than 186,000 km2 of potential seafloor area was identified within the US Gulf of Mexico/Florida, Caribbean, and main Hawaiian Islands.
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Marine and Meteoric Diagenesis of Pleistocene Carbonates from a Nearshore Submarine Terrace, Oahu, Hawaii
TL;DR: In this paper, a series of short cores taken from a nearshore terrace were used to identify three periods of diagenesis: early shallow marine, meteoric, and post-meteoric shallow marine.
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Stratigraphic constraints on the timing and emplacement of the Alika 2 giant Hawaiian submarine landslide
Gary M. McMurtry,Emilio Herrero-Bervera,Maximilian D. Cremer,John R. Smith,Johanna M. Resig,Clark Sherman,Michael E. Torresan +6 more
TL;DR: This paper used a suite of seven piston, gravity and box cores collected in the vicinity of the Alika 2 slide and used U-series dating techniques, including excess 230 Th and 210 Pb profiling, high-resolution paleomagnetic stratigraphy, including continuous, U-channel analysis, δ 18 O stratigraphic, visual and X-ray sediment lithology, and the petrology and geochemistry of the included turbidites and ash layers.
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Fossiliferous Lana'i deposits formed by multiple events rather than a single giant tsunami
TL;DR: It is shown that the Hulopoe gravel was formed by multiple depositional events, separated by considerable periods of time, thus invalidating the main premise of the ‘giant wave’ hypothesis.
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New evidence for two highstands of the sea during the last interglacial, oxygen isotope substage 5e
TL;DR: Sedimentologic, stratigraphic, and geochronologic analyses of a previously undescribed carbonate section on Oahu, Hawaii, provide new evidence for two distinct sea-level highstands during the last interglacial period as discussed by the authors.