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all geography including DSDP/ODP Sites and Legs
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Africa
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Invertebrata
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Precambrian
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upper Precambrian
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Proterozoic
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igneous rocks
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Primary terms
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absolute age (12)
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Africa
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North Africa
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Algeria (2)
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Libya (1)
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Morocco (1)
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Sahara (1)
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Southern Africa
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West Africa
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Cameroon (1)
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Taoudenni Basin (1)
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Antarctica
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Lake Vostok (1)
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Transantarctic Mountains
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Shackleton Range (1)
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Arctic region
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Greenland
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South Greenland (1)
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West Greenland (1)
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Asia
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Arabian Peninsula
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Oman (1)
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Lena River (1)
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Middle East
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Cyprus
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Troodos Massif (1)
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Ob River (1)
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Siberia (1)
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Yenisei River (1)
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Atlantic Ocean
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Cenozoic
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Innuitian ice sheet (1)
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upper Pleistocene
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Wisconsinan
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upper Quaternary
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Pinedale Glaciation (1)
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Tertiary
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Neogene
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Miocene
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upper Miocene
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Pliocene
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upper Cenozoic (1)
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Invertebrata
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Mesozoic
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metals
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alkaline earth metals
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
glacial rebound
Glacial isostatic adjustment driven by asymmetric ice sheet melt during the Last Interglacial causes multiple local sea-level peaks Available to Purchase
North American Midcontinent Pennsylvanian cyclothems and their implications Available to Purchase
Abstract Cyclothems are stratigraphic sequences deposited during glacial-eustatic transgressive–regressive inundations of land. Major cyclothems are most complete on lower shelves and become separated by exposure surfaces higher on the shelf. Minor cyclothems extend only onto lower shelves or are parasequences reflecting a reversal of sea level during general phases of transgression or regression. In Midcontinent North America, highstand condensed intervals of major cyclothems are conodont-rich black shales correlated eastwards into the Illinois and Appalachian basins. The number of cyclothems decreased by loss of lesser cyclothems across these basins, signifying an eastwards increase in their depositional elevations. Generalized palaeogeographical maps show that facies successions developed across these basins during a single major interglacial transgression and regression. The control of glacial eustasy by the interaction of Earth's orbital parameters, along with radiometric dating, allows subdivision of the cyclothem succession into c. 400 kyr groupings, which reflect the longest eccentricity cycle and facilitates global correlation. Delineation of the basinward extents of regression from the disappearance of exposure surfaces elucidates the history of basin-margin development. Major cyclothems that underwent reversals of general sea-level trend display ‘splays’ of lesser cycles onto the higher shelf. Geochemical cycles ‘nested’ within deepest-water shales on low shelves appear as thin nearshore facies between exposure surfaces at their high-shelf shorelines.
Evidence for a more extensive Greenland Ice Sheet in southwestern Greenland during the Last Glacial Maximum Open Access
The influence of glacial isostatic adjustment on continental shelf stratigraphic correlation Open Access
Narrow is normal: Exploring the extent and significance of flooded marine shelves in icehouse, transitional, and greenhouse climate settings Open Access
Lateral variation in slab window viscosity inferred from global navigation satellite system (GNSS)–observed uplift due to recent mass loss at Patagonia ice fields Available to Purchase
How Climate, Uplift and Erosion Shaped the Alpine Topography Available to Purchase
Postglacial Uplift: Record in the Gravity Field and in Neogene–Quaternary Structures Available to Purchase
Late Quaternary sea-level history of Saipan, Commonwealth of the Northern Mariana Islands, USA: A test of tectonic uplift and glacial isostatic adjustment models Available to Purchase
Glacial isostatic adjustment in central Cascadia: Insights from three-dimensional Earth modeling Available to Purchase
Glacial isostatic adjustment deflects the path of the ancestral Hudson River Open Access
Role of karst denudation on the accurate assessment of glacio-eustasy and tectonic uplift on carbonate coasts Available to Purchase
Abstract Quaternary glacio-eustasy has traditionally been determined in part by the examination of fossil coral reefs on carbonate islands and coasts uplifted by tectonics. These studies do not properly account for dissolutional denudation, which is cumulative, making higher and therefore older terraces exist at elevations far below their assumed depositional elevation. Karst pedestals (karrentische) on Guam reveal the extent of the denudation ( c. 50 mm ka −1 ) and demonstrate that theoretical denudation models can be accurately applied to eogenetic carbonates in tropical settings. Aeolian calcarenite islands such as the Bahamas have been used as tectonically stable sea-level calibrations for other islands, which may not be correct. Flank margin caves, forming in the distal margin of the freshwater lens within a carbonate island, are excellent sea-level indicators. Analysis of flank margin cave elevations indicates that the Bahamas have had past sea-level highstands >6 m, perhaps up to 15 m or more, for which no fossil coral data exist. Denudational removal of these older corals has biased the record to younger events and only flank margin caves remain as viable terrestrial signatures of these older sea-level highstands.