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John E. Damuth [4]John Damuth [1]
  1. Alternative Formulations of Multilevel Selection.John Damuth & I. Lorraine Heisler - 1988 - Biology and Philosophy 3 (4):407-430.
    Hierarchical expansions of the theory of natural selection exist in two distinct bodies of thought in evolutionary biology, the group selection and the species selection traditions. Both traditions share the point of view that the principles of natural selection apply at levels of biological organization above the level of the individual organism. This leads them both to considermultilevel selection situations, where selection is occurring simultaneously at more than one level. Impeding unification of the theoretical approaches of the multilevel selection traditions (...)
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    Latest Quaternary Sedimentation in the Northern Gulf of Mexico Intraslope Basin Province: II — Stratigraphic Analysis and Relationship to Glacioeustatic Climate Change.Hilary Clement Olson, John E. Damuth & C. Hans Nelson - 2016 - Interpretation: SEG 4 (1):SC81-SC95.
    Stratigraphic zonation of 139 piston cores from the intraslope basin province of the northern Gulf of Mexico based on the Globorotalia menardii complex and calcium carbonate fluctuations shows that the vast majority of the cores contain sediments only of Holocene and Late Wisconsin age. Only 13 widely spaced cores penetrate sediments of Last Interglacial age. Overall, sedimentation rates average approximately 13 cm for the Holocene, but they range up to 600 cm. Redeposited sediments occur in cores from the Rio Grande (...)
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    Late Pleistocene Bryant Canyon Turbidite System: Implications for Gulf of Mexico Minibasin Petroleum Systems.C. Hans Nelson, John E. Damuth & Hilary Clement Olson - 2018 - Interpretation 6 (2):SD89-SD114.
    The western ancestral Mississippi shelf-margin delta fed the Bryant Canyon turbidite system in the intraslope basin province of the northwestern Gulf of Mexico during the penultimate glacial lowstand of sea level. The Bryant Canyon links a chain of 15 fill-and-spill minibasins on the continental slope. On the upper and lower continental slopes, minibasins are narrow, elongate, and follow salt ridges. On the middle slope, minibasins are larger semicircular basins. Three main depositional facies are recognized based on seismic-facies interpretation: ponded turbidites, (...)
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    Late Pleistocene Bryant Canyon Turbidite System: Implications for Gulf of Mexico Minibasin Petroleum Systems.C. Hans Nelson, John E. Damuth & Hilary Clement Olson - 2018 - Interpretation: SEG 6 (2):SD89-SD114.
    The western ancestral Mississippi shelf-margin delta fed the Bryant Canyon turbidite system in the intraslope basin province of the northwestern Gulf of Mexico during the penultimate glacial lowstand of sea level. The Bryant Canyon links a chain of 15 fill-and-spill minibasins on the continental slope. On the upper and lower continental slopes, minibasins are narrow, elongate, and follow salt ridges. On the middle slope, minibasins are larger semicircular basins. Three main depositional facies are recognized based on seismic-facies interpretation: ponded turbidites, (...)
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    To: “Latest Quaternary Sedimentation in the Northern Gulf of Mexico Intraslope Basin Province: II — Stratigraphic Analysis and Relationship to Glacioeustatic Climate Change,” Hilary Clement Olson, John E. Damuth, and C. Hans Nelson, Interpretation, 4, No. 1, SC81–SC95, Doi: Http://Dx.Doi.Org/10.1190/INT-2015-0111.1. [REVIEW]Hilary Clement Olson, John E. Damuth & C. Hans Nelson - 2016 - Interpretation: SEG 4 (3):Y1-Y1.
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