FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2893386024> ?p ?o ?g. }

• W2893386024 endingPage "173" @default.
• W2893386024 startingPage "159" @default.
• W2893386024 abstract "The Bengal Fan contains the most complete record of Himalayan climate and tectonics. As the largest fan system of the world it is fed by the Ganges-Brahmaputra river systems. International Ocean Discovery Program (IODP) Expedition 354 cored seven sites along an east-west core transect at 8°N in the lower Bengal Fan. We studied the Pleistocene sections of these sites to provide constraints on the depositional history of the last 1.25 Ma. Low-resolution bio- and magnetostratigraphic constraints identified two regionally-extensive hemipelagic units and intercalated turbidite deposits that provide a chronostratigraphic framework for the 320 km transect. Using a combination of lithostratigraphy and sediment physical properties that vary on orbital timescales, we tuned high-resolution data sets to the LR04 benthic δ18O isotope stack to obtain new constraints on the timing of depositional changes. Above the underlying Unit 1, which consists of Early to Middle Pleistocene turbiditic deposits, we divide four more units for the last 1.25 Ma: Unit 2, a Middle Pleistocene hemipelagic layer deposited at all sites from Marine Isotopic Stages (MIS) 37 to ∼17 (∼1.24–0.68 Ma) during the entire time of the Mid-Pleistocene Transition, when the Bengal Fan depocenter must have been distal to our transect; Unit 3, mostly turbidites with some intercalated hemipelgic sediments deposited from ∼MIS 16–∼13 (∼0.68–0.48 Ma), with sandy lithologies only found at the easternmost site on the west flank of the Ninetyeast Ridge; Unit 4, massive turbiditic sediments that started to dominate deposition with the Mid-Brunhes Transition (∼MIS 12) until MIS 7/8 (∼0.48–0.25 Ma), when the channel-levee system was focused east of the 85°E basement ridge at 8°N; and Unit 5, a Late Pleistocene hemipelagic layer at the top that spans MIS 7/8–1 (∼0.25 Ma to present) while the turbidite deposition was focused west of the 85°E basement ridge at 8°N. We find evidence that, on these timescales, deposition across the lower Bengal Fan changed with the evolution of Pleistocene climate, monsoon and sea-level history and hence responded to external controls on sediment accumulation and fan architecture rather than only fan-internal, autocyclic mechanisms." @default.
• W2893386024 created "2018-10-05" @default.
• W2893386024 creator A5004973436 @default.
• W2893386024 creator A5054535874 @default.
• W2893386024 date "2018-11-01" @default.
• W2893386024 modified "2023-10-02" @default.
• W2893386024 title "Hemipelagic and turbiditic deposits constrain lower Bengal Fan depositional history through Pleistocene climate, monsoon, and sea level transitions" @default.
• W2893386024 cites W1606159312 @default.
• W2893386024 cites W1957133103 @default.
• W2893386024 cites W1964841874 @default.
• W2893386024 cites W1970259090 @default.
• W2893386024 cites W1971269388 @default.
• W2893386024 cites W1973935658 @default.
• W2893386024 cites W1984430746 @default.
• W2893386024 cites W1990397580 @default.
• W2893386024 cites W1992855123 @default.
• W2893386024 cites W2003954381 @default.
• W2893386024 cites W2013543659 @default.
• W2893386024 cites W2013648360 @default.
• W2893386024 cites W2015252820 @default.
• W2893386024 cites W2022752707 @default.
• W2893386024 cites W2030174121 @default.
• W2893386024 cites W2031171042 @default.
• W2893386024 cites W2032598945 @default.
• W2893386024 cites W2036241768 @default.
• W2893386024 cites W2052736701 @default.
• W2893386024 cites W2064086442 @default.
• W2893386024 cites W2066148746 @default.
• W2893386024 cites W2067699267 @default.
• W2893386024 cites W2072336607 @default.
• W2893386024 cites W2072470725 @default.
• W2893386024 cites W2073551687 @default.
• W2893386024 cites W2076850342 @default.
• W2893386024 cites W2079989213 @default.
• W2893386024 cites W2080589433 @default.
• W2893386024 cites W2080958987 @default.
• W2893386024 cites W2087354441 @default.
• W2893386024 cites W2087943977 @default.
• W2893386024 cites W2095016078 @default.
• W2893386024 cites W2101372386 @default.
• W2893386024 cites W2103765846 @default.
• W2893386024 cites W2122295209 @default.
• W2893386024 cites W2143337505 @default.
• W2893386024 cites W2165255116 @default.
• W2893386024 cites W2171153098 @default.
• W2893386024 cites W2335961020 @default.
• W2893386024 cites W2366526863 @default.
• W2893386024 cites W2577534579 @default.
• W2893386024 cites W2746620662 @default.
• W2893386024 cites W2754828531 @default.
• W2893386024 cites W2765720958 @default.
• W2893386024 cites W2772225377 @default.
• W2893386024 cites W2799800305 @default.
• W2893386024 cites W2803765031 @default.
• W2893386024 cites W2887838026 @default.
• W2893386024 cites W2890433812 @default.
• W2893386024 doi "https://doi.org/10.1016/j.quascirev.2018.09.027" @default.
• W2893386024 hasPublicationYear "2018" @default.
• W2893386024 type Work @default.
• W2893386024 sameAs 2893386024 @default.
• W2893386024 citedByCount "21" @default.
• W2893386024 countsByYear W28933860242019 @default.
• W2893386024 countsByYear W28933860242020 @default.
• W2893386024 countsByYear W28933860242021 @default.
• W2893386024 countsByYear W28933860242022 @default.
• W2893386024 countsByYear W28933860242023 @default.
• W2893386024 crossrefType "journal-article" @default.
• W2893386024 hasAuthorship W2893386024A5004973436 @default.
• W2893386024 hasAuthorship W2893386024A5054535874 @default.
• W2893386024 hasConcept C109007969 @default.
• W2893386024 hasConcept C126753816 @default.
• W2893386024 hasConcept C127313418 @default.
• W2893386024 hasConcept C138841024 @default.
• W2893386024 hasConcept C151730666 @default.
• W2893386024 hasConcept C157954998 @default.
• W2893386024 hasConcept C53570757 @default.
• W2893386024 hasConcept C6494504 @default.
• W2893386024 hasConceptScore W2893386024C109007969 @default.
• W2893386024 hasConceptScore W2893386024C126753816 @default.
• W2893386024 hasConceptScore W2893386024C127313418 @default.
• W2893386024 hasConceptScore W2893386024C138841024 @default.
• W2893386024 hasConceptScore W2893386024C151730666 @default.
• W2893386024 hasConceptScore W2893386024C157954998 @default.
• W2893386024 hasConceptScore W2893386024C53570757 @default.
• W2893386024 hasConceptScore W2893386024C6494504 @default.
• W2893386024 hasLocation W28933860241 @default.
• W2893386024 hasOpenAccess W2893386024 @default.
• W2893386024 hasPrimaryLocation W28933860241 @default.
• W2893386024 hasRelatedWork W1868012504 @default.
• W2893386024 hasRelatedWork W1981062320 @default.
• W2893386024 hasRelatedWork W2016995231 @default.
• W2893386024 hasRelatedWork W2021012877 @default.
• W2893386024 hasRelatedWork W2167050352 @default.
• W2893386024 hasRelatedWork W2263405633 @default.
• W2893386024 hasRelatedWork W2983263553 @default.
• W2893386024 hasRelatedWork W3124051389 @default.
• W2893386024 hasRelatedWork W4304890768 @default.
• W2893386024 hasRelatedWork W2741962369 @default.

• next