FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2046808001> ?p ?o ?g. }

• W2046808001 endingPage "55" @default.
• W2046808001 startingPage "40" @default.
• W2046808001 abstract "Abstract This study presents combined mineralogical, chemical, isotopic (87Sr/86Sr and U–Th disequilibria series) and palynological analyses on bulk sediments and on distinct mineral phases (carbonates and clays) from a 10-m-long core drilled in the southern Caspian Sea and containing a Late Pleistocene and Early Holocene record. The data allowed identifying 1) the main variations in sedimentation, 2) the processes causing these variations, 3) the modification of erosion vs weathering, and 4) the influence of climatic and/or Caspian Sea level changes in the region since the Late Pleistocene. The chemical and mineralogical results allowed the division of the sedimentary sequence into three main units and a transition zone. The lower unit (unit U1) primarily consists of silicate and carbonate-rich detritus. Sedimentation characteristics, including observation of detritus in secular equilibrium, are relatively constant within this unit and reflect mechanical erosion in a cold climate. Unit U1 probably corresponds to a glacial period when the vegetation cover was sparse and wind and river transport of pollen were strong. Subsequently, global increase in temperatures has greatly modified the sedimentation in the Caspian Sea south basin. Biogenic sedimentation is higher in units U2 and U3, and detrital inputs varied from unit U1. Variations in detrital input are likely to be caused by decreasing aeolian contribution and by relative changes in river volumes and origins. The study of the bulk sediments, clays and carbonates reflects an increase in chemical weathering since about 10 14C ka BP ago (base of unit U2), in line with an increase in the vegetation cover. Our results suggest an evolution of continental weathering conditions in the catchment area of the Caspian Sea, from dominantly mechanical/physical erosion during the cold period to a continuous increase in weathering since the Lateglacial period, as climate improved, which illustrates the strong relation between climate, vegetation cover and weathering processes. This paper also highlights how the U–Th disequilibrium series proxy, combined with other geochemical and palynological studies, could be a useful tool to record and constrain the modification of weathering regime in response to climatic and environmental changes at regional scale." @default.
• W2046808001 created "2016-06-24" @default.
• W2046808001 creator A5030103482 @default.
• W2046808001 creator A5047190823 @default.
• W2046808001 creator A5081714282 @default.
• W2046808001 creator A5086710204 @default.
• W2046808001 date "2012-09-01" @default.
• W2046808001 modified "2023-09-25" @default.
• W2046808001 title "A record of Late Quaternary continental weathering in the sediment of the Caspian Sea: evidence from U–Th, Sr isotopes, trace element and palynological data" @default.
• W2046808001 cites W1965900209 @default.
• W2046808001 cites W1967081859 @default.
• W2046808001 cites W1967259827 @default.
• W2046808001 cites W1973394078 @default.
• W2046808001 cites W1973425488 @default.
• W2046808001 cites W1974353877 @default.
• W2046808001 cites W1974914902 @default.
• W2046808001 cites W1977297193 @default.
• W2046808001 cites W1977370485 @default.
• W2046808001 cites W1977737528 @default.
• W2046808001 cites W1979117038 @default.
• W2046808001 cites W1979939669 @default.
• W2046808001 cites W1982308240 @default.
• W2046808001 cites W1983074079 @default.
• W2046808001 cites W1983715333 @default.
• W2046808001 cites W1984873628 @default.
• W2046808001 cites W1986664302 @default.
• W2046808001 cites W1988163817 @default.
• W2046808001 cites W1999888263 @default.
• W2046808001 cites W2003333807 @default.
• W2046808001 cites W2004997318 @default.
• W2046808001 cites W2005327714 @default.
• W2046808001 cites W2006456876 @default.
• W2046808001 cites W2008670387 @default.
• W2046808001 cites W2013338205 @default.
• W2046808001 cites W2013796674 @default.
• W2046808001 cites W2014233158 @default.
• W2046808001 cites W2015542659 @default.
• W2046808001 cites W2019907247 @default.
• W2046808001 cites W2024133647 @default.
• W2046808001 cites W2024608698 @default.
• W2046808001 cites W2025949885 @default.
• W2046808001 cites W2032574517 @default.
• W2046808001 cites W2033242016 @default.
• W2046808001 cites W2036580797 @default.
• W2046808001 cites W2045848830 @default.
• W2046808001 cites W2050042705 @default.
• W2046808001 cites W2050818497 @default.
• W2046808001 cites W2051391634 @default.
• W2046808001 cites W2065231332 @default.
• W2046808001 cites W2068420976 @default.
• W2046808001 cites W2068448933 @default.
• W2046808001 cites W2070843428 @default.
• W2046808001 cites W2075238897 @default.
• W2046808001 cites W2075991177 @default.
• W2046808001 cites W2077620271 @default.
• W2046808001 cites W2083730846 @default.
• W2046808001 cites W2084720486 @default.
• W2046808001 cites W2095361963 @default.
• W2046808001 cites W2100920216 @default.
• W2046808001 cites W2107843890 @default.
• W2046808001 cites W2114850632 @default.
• W2046808001 cites W2124688798 @default.
• W2046808001 cites W2126612937 @default.
• W2046808001 cites W2133008302 @default.
• W2046808001 cites W2133320116 @default.
• W2046808001 cites W2163822849 @default.
• W2046808001 cites W2167425355 @default.
• W2046808001 cites W2168453173 @default.
• W2046808001 cites W2184876481 @default.
• W2046808001 cites W59526064 @default.
• W2046808001 doi "https://doi.org/10.1016/j.quascirev.2012.07.020" @default.
• W2046808001 hasPublicationYear "2012" @default.
• W2046808001 type Work @default.
• W2046808001 sameAs 2046808001 @default.
• W2046808001 citedByCount "22" @default.
• W2046808001 countsByYear W20468080012012 @default.
• W2046808001 countsByYear W20468080012013 @default.
• W2046808001 countsByYear W20468080012014 @default.
• W2046808001 countsByYear W20468080012015 @default.
• W2046808001 countsByYear W20468080012016 @default.
• W2046808001 countsByYear W20468080012017 @default.
• W2046808001 countsByYear W20468080012018 @default.
• W2046808001 countsByYear W20468080012019 @default.
• W2046808001 countsByYear W20468080012020 @default.
• W2046808001 countsByYear W20468080012021 @default.
• W2046808001 countsByYear W20468080012023 @default.
• W2046808001 crossrefType "journal-article" @default.
• W2046808001 hasAuthorship W2046808001A5030103482 @default.
• W2046808001 hasAuthorship W2046808001A5047190823 @default.
• W2046808001 hasAuthorship W2046808001A5081714282 @default.
• W2046808001 hasAuthorship W2046808001A5086710204 @default.
• W2046808001 hasConcept C111368507 @default.
• W2046808001 hasConcept C127313418 @default.
• W2046808001 hasConcept C151730666 @default.
• W2046808001 hasConcept C160464908 @default.
• W2046808001 hasConcept C162501224 @default.
• W2046808001 hasConcept C17409809 @default.
• W2046808001 hasConcept C184751465 @default.

• next