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Hemipelagic sediment information


Hemipelagic sediment, or hemipelagite, is a type of marine sediment that consists of clay and silt-sized grains that are terrigenous and some biogenic material derived from the landmass nearest the deposits or from organisms living in the water.[1][2] Hemipelagic sediments are deposited on continental shelves and continental rises, and differ from pelagic sediment compositionally. Pelagic sediment is composed of primarily biogenic material from organisms living in the water column or on the seafloor and contains little to no terrigenous material.[1] Terrigenous material includes minerals from the lithosphere like feldspar or quartz. Volcanism on land, wind blown sediments as well as particulates discharged from rivers can contribute to Hemipelagic deposits.[3] These deposits can be used to qualify climatic changes and identify changes in sediment provenances.[4][5]

  1. ^ a b Cite error: The named reference Ochoa et al 2013 was invoked but never defined (see the help page).
  2. ^ Cite error: The named reference Stow 1994 was invoked but never defined (see the help page).
  3. ^ Cite error: The named reference Aksu et al 1995 was invoked but never defined (see the help page).
  4. ^ Cite error: The named reference Trentesaux et al 2001 was invoked but never defined (see the help page).
  5. ^ Cite error: The named reference Weedon 1986 was invoked but never defined (see the help page).

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Hemipelagic sediment

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Hemipelagic sediment, or hemipelagite, is a type of marine sediment that consists of clay and silt-sized grains that are terrigenous and some biogenic...

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Marine sediment

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Hemipelagic sediments are deposited on continental shelves and continental rises, and differ from pelagic sediment compositionally. Pelagic sediment is...

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Redox gradient

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waterlogged soils, wetlands, contaminant plumes, and marine pelagic and hemipelagic sediments. The following is a list of common reactions that occur in the environment...

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Continental rise

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the continental slope. More gradual accumulation of sediments occurs when hemipelagic sediments suspended in the ocean slowly settle to the ocean basin...

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Accretionary wedge

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terrestrial material, basalts from the ocean floor, and pelagic and hemipelagic sediments. For example, most of the geological basement of Japan is made up...

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Polycladomyces abyssicola

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bacterium from the genus of Planifilum which has been isolated from hemipelagic sediments from deep seawater. "Polycladomyces". List of Prokaryotic Names...

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Tarfaya Basin

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occurred via clastic deposition of fine-grain aeolian clastics and hemipelagic sediment. The result has been thinly bedded shale deposits that have grown...

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Madeira Abyssal Plain

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layer of hemipelagic sediments. These sediments average 200 meters (660 ft) in thickness and are expected to consist predominantly of hemipelagic clay. Overlying...

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Manila Trench

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‘t0’ represents the unconformity between the hemipelagic sediments and overlying trench-fill sediments. This surface lessens in slope and decreases in...

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Submarine landslide

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plasticity silts, rapid formation of moraines and till above hemipelagic interstaidal sediments. An example where glacial loading leads to submarine landsliding...

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Sea of Japan

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covered in hemipelagic sediments (i.e., of semi-oceanic origin); these sediments are composed of blue mud rich in organic matter. Pelagic sediments of red...

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Birnessite

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et al. (2007). "Formation of todorokite from vernadite in Ni-rich hemipelagic sediments". Geochimica et Cosmochimica Acta. 71 (23): 5698–5716. Bibcode:2007GeCoA...

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Bioturbation

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(1998). "Biogeochemical heterogeneity and suboxic diagenesis in hemipelagic sediments of the Panama Basin". Deep Sea Research Part I: Oceanographic Research...

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Cascadia Channel

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Cenozoic, the volcanic basement was covered by transparent pelagic and hemipelagic sediment, which horizontally deposited turbidites covered. During late Pleistocene...

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Polycladomyces

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nov., sp. nov., a thermophilic filamentous bacterium isolated from hemipelagic sediment". International Journal of Systematic and Evolutionary Microbiology...

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Windermere Supergroup

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thinner-bedded, and anoxic hemipelagics give way to oxygenated sediments, with storm beds becoming more and more common, and intertidal sediments topping the group...

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Paleocene

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exposed record 165 m (541 ft) thick, mainly composed of alternating hemipelagic sediments deposited at a depth of about 1,000 m (3,300 ft). The Danian deposits...

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Academician Ridge

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Academician Ridge is restricted to fine, continuous hemipelagic sedimentation with dispersed coarse-grained sediment deposited by ice rafting (Kuzmin et al., 2000)...

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Val Verde Basin

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24–40 km wide by 240 km long. It is an unconventional system and its sediments were deposited during a long period of flooding during the Middle to Late...

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Tropic Seamount

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coral debris, hemipelagic sediments, breccia, limestones, felsite, foraminiferal sand, pelagic ooze, reefal limestones and sediments have been recovered...

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Tyrrhenian Basin

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the syn-rift sediments are 200 meters of Pliocene to Pleistocene hemipelagic marine sediment with intermittent volcanic glass. This sediment layer is believed...

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Geology of the Pyrenees

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Pyrenees, shallow marine facies prevail, whereas in the eastern Pyrenees, hemipelagic facies with occasional high grounds predominate. The Devonian has highly...

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La Caja Formation

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well-preserved ammonites. It was deposited in hemipelagic conditions, and predominantly consists of siliclastic sediments, including marl, with limestone. It is...

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Posidonia Shale

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delimited to several minibasins, including the Southwest German Basin, a hemipelagic deposit, with the influence of open sea currents from the North and the...

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Marne di Monte Serrone

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layers located towards Pozzale are of typical hemipelagic nature, lacking proper amounts of carbonate sediments. By contrast, towards Colle d’orlando and...

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Tremp Formation

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sedimentary thickness of 4,650 metres (15,260 ft) comprising mostly hemipelagic marls and limestones, deposited in a back-arc basin setting with normal...

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Fogo Seamounts

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sediments were found to overlie the guyot and were abruptly overlain by hemipelagic shales. A series of coastal transgressions above the basalt suggest that...

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