FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2964909467> ?p ?o ?g. }

• W2964909467 endingPage "345" @default.
• W2964909467 startingPage "345" @default.
• W2964909467 abstract "The Djibouti Ville Drift is part of a contourite depositional system located on the southern side of the Djibouti Ville Seamount in the Alboran Sea (Western Mediterranean). The sedimentary record of a core located in the drift deposits has been characterized to achieve the possible sediment sources for the Saharan dust supply and the paleocurrent variability related to Mediterranean intermediate waters for the last 133 kyr. Three end-member grain-size distributions characterize the sediment record transported by the bottom current to address the different aeolian populations, i.e., coarse EM1, silty EM2, and fine EM3. For these particles, the most likely source areas are the Saharan sedimentary basins and deserts, as well as the cratonic basins of the Sahara-Sahel Dust Corridor. The prevalence of these main source areas is shown in the core record, where a noticeable change occurs during the MIS 5 to MIS 4 transition. Some punctual sediment inputs from the seamount have been recognized during sea-level lowstand, but there is no evidence of fluvial supply in the drift deposits. The paleocurrent reconstruction allows the characterizing of the stadial and cold periods by large increases in the mean sortable silt fraction and UP10, which point to an enhanced bottom current strength related to intermediate water masses. Conversely, interglacial periods are characterized by weaker bottom current activity, which is associated with denser deep water masses. These proxies also recorded the intensified Saharan wind transport that occurred during interstadial/stadial transitions. All these results point to the importance of combining sediment source areas with major climatic oscillations and paleocurrent variability in palaeoceanographic sedimentary archives, which may help to develop future climate prediction models." @default.
• W2964909467 created "2019-08-13" @default.
• W2964909467 creator A5002669602 @default.
• W2964909467 creator A5008194070 @default.
• W2964909467 creator A5010844378 @default.
• W2964909467 creator A5013032128 @default.
• W2964909467 creator A5017938382 @default.
• W2964909467 creator A5021633239 @default.
• W2964909467 creator A5025889615 @default.
• W2964909467 creator A5036982782 @default.
• W2964909467 creator A5040867996 @default.
• W2964909467 creator A5060452166 @default.
• W2964909467 creator A5061857057 @default.
• W2964909467 creator A5073941887 @default.
• W2964909467 creator A5075071181 @default.
• W2964909467 creator A5078506654 @default.
• W2964909467 date "2019-08-07" @default.
• W2964909467 modified "2023-10-16" @default.
• W2964909467 title "133,000 Years of Sedimentary Record in a Contourite Drift in the Western Alboran Sea: Sediment Sources and Paleocurrent Reconstruction" @default.
• W2964909467 cites W1590129562 @default.
• W2964909467 cites W1610630489 @default.
• W2964909467 cites W1746443254 @default.
• W2964909467 cites W1919635784 @default.
• W2964909467 cites W1965430736 @default.
• W2964909467 cites W1965807239 @default.
• W2964909467 cites W1970535386 @default.
• W2964909467 cites W1971815143 @default.
• W2964909467 cites W1980498694 @default.
• W2964909467 cites W1984282652 @default.
• W2964909467 cites W1995252080 @default.
• W2964909467 cites W1995471679 @default.
• W2964909467 cites W1998236113 @default.
• W2964909467 cites W1999956578 @default.
• W2964909467 cites W2001769537 @default.
• W2964909467 cites W2003073603 @default.
• W2964909467 cites W2003450165 @default.
• W2964909467 cites W2004979428 @default.
• W2964909467 cites W2009411107 @default.
• W2964909467 cites W2011848041 @default.
• W2964909467 cites W2012006566 @default.
• W2964909467 cites W2012223487 @default.
• W2964909467 cites W2016349369 @default.
• W2964909467 cites W2018517457 @default.
• W2964909467 cites W2018530452 @default.
• W2964909467 cites W2021771753 @default.
• W2964909467 cites W2024504016 @default.
• W2964909467 cites W2025940654 @default.
• W2964909467 cites W2025974824 @default.
• W2964909467 cites W2026935997 @default.
• W2964909467 cites W2030347013 @default.
• W2964909467 cites W2031999703 @default.
• W2964909467 cites W2032321488 @default.
• W2964909467 cites W2044662500 @default.
• W2964909467 cites W2049445265 @default.
• W2964909467 cites W2051631509 @default.
• W2964909467 cites W2056622109 @default.
• W2964909467 cites W2058403430 @default.
• W2964909467 cites W2058909952 @default.
• W2964909467 cites W2059505838 @default.
• W2964909467 cites W2062312345 @default.
• W2964909467 cites W2063728128 @default.
• W2964909467 cites W2063957648 @default.
• W2964909467 cites W2073279142 @default.
• W2964909467 cites W2077267127 @default.
• W2964909467 cites W2079313912 @default.
• W2964909467 cites W2084475884 @default.
• W2964909467 cites W2086764528 @default.
• W2964909467 cites W2091381985 @default.
• W2964909467 cites W2092897417 @default.
• W2964909467 cites W2099826005 @default.
• W2964909467 cites W2113418246 @default.
• W2964909467 cites W2132829210 @default.
• W2964909467 cites W2133520730 @default.
• W2964909467 cites W2145619152 @default.
• W2964909467 cites W2146159291 @default.
• W2964909467 cites W2149498600 @default.
• W2964909467 cites W2151920552 @default.
• W2964909467 cites W2159525271 @default.
• W2964909467 cites W2165651847 @default.
• W2964909467 cites W2167130289 @default.
• W2964909467 cites W2169243413 @default.
• W2964909467 cites W2171032009 @default.
• W2964909467 cites W2212446569 @default.
• W2964909467 cites W2280624662 @default.
• W2964909467 cites W2568176443 @default.
• W2964909467 cites W2793481095 @default.
• W2964909467 cites W2904411916 @default.
• W2964909467 cites W2925105310 @default.
• W2964909467 cites W4235241007 @default.
• W2964909467 cites W4249751050 @default.
• W2964909467 doi "https://doi.org/10.3390/geosciences9080345" @default.
• W2964909467 hasPublicationYear "2019" @default.
• W2964909467 type Work @default.
• W2964909467 sameAs 2964909467 @default.
• W2964909467 citedByCount "9" @default.
• W2964909467 countsByYear W29649094672019 @default.
• W2964909467 countsByYear W29649094672021 @default.
• W2964909467 countsByYear W29649094672022 @default.

• next