FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1981845140> ?p ?o ?g. }

• W1981845140 endingPage "3629" @default.
• W1981845140 startingPage "3599" @default.
• W1981845140 abstract "To understand the processes controlling the formation of the sediment record, seasonal variations of living communities, fluxes through the water column, and sediment accumulation rates of diatoms, coccolithophores (phytoplankton), and planktic foraminifera (zooplankton) were studied through seasonal water-column sampling, sediment traps, and box- and multi-core sediment sampling in the Canary Islands region (29°N), from the productive NW African coastal area to offshore oligotrophic waters. A close relationship between the phytoplankton composition and hydrographic conditions was observed. Coccolithophores dominate the phytoplankton community throughout the year. The seasonal flux variability of the various groups as measured in the upper-trap samples (≈500–900 m water depth) reflects the seasonal changes of their vertically integrated standing stocks in the overlying water column. Distinct high-standing stocks of all three groups can be related to the influence of upwelling filaments at the near-shore site (EBC). At the offshore sites (ESTOC and LaPalma) all groups display a late winter/early spring maxima related to local increased production. In addition, the increase in flux of all the organisms observed in the deeper traps at both offshore sites can be explained by lateral advection of living material by surface filaments. In addition, the occurrence in the traps of diatom and foraminifera species characteristic of high-productivity coastal areas indicates that the material must come from a highly productive coastal region, rather than production in the overlying oligotrophic surface water. Investigation of the phytoplankton assemblages in the water column, sediment traps, and surface sediments reveals: (i) sediment assemblages have been somewhat modified both by differential dissolution in the water column and the sediments and possibly also by reworking and (ii) the original composition is fundamentally preserved. Diatoms, in spite of being the most affected by differential dissolution both during settling and within the sediments, show a clear relation to the upwelling process. Planktic foraminifera (zooplankton) appear to be less altered by dissolution. For both groups, however, the dominant taxa during the upwelling episodic events (Chaetoceros and Globigerina bulloides) dominate the assemblages found in the sediments underlying Cape Ghir, the most productive area of the Canary Islands region." @default.
• W1981845140 created "2016-06-24" @default.
• W1981845140 creator A5001833515 @default.
• W1981845140 creator A5010321851 @default.
• W1981845140 creator A5012847386 @default.
• W1981845140 creator A5014861948 @default.
• W1981845140 creator A5034350687 @default.
• W1981845140 creator A5062673931 @default.
• W1981845140 creator A5074648456 @default.
• W1981845140 creator A5074761839 @default.
• W1981845140 creator A5076350979 @default.
• W1981845140 creator A5089453253 @default.
• W1981845140 creator A5091713611 @default.
• W1981845140 date "2002-01-01" @default.
• W1981845140 modified "2023-09-26" @default.
• W1981845140 title "Fluxes of micro-organisms along a productivity gradient in the Canary Islands region (29°N): implications for paleoreconstructions" @default.
• W1981845140 cites W1484670402 @default.
• W1981845140 cites W1505852232 @default.
• W1981845140 cites W1558445336 @default.
• W1981845140 cites W1977537427 @default.
• W1981845140 cites W1980372891 @default.
• W1981845140 cites W1980540284 @default.
• W1981845140 cites W1982588318 @default.
• W1981845140 cites W1993270174 @default.
• W1981845140 cites W1995863362 @default.
• W1981845140 cites W1996764260 @default.
• W1981845140 cites W1999811737 @default.
• W1981845140 cites W2003952131 @default.
• W1981845140 cites W2007449945 @default.
• W1981845140 cites W2014830499 @default.
• W1981845140 cites W2019578472 @default.
• W1981845140 cites W2028148749 @default.
• W1981845140 cites W2030835188 @default.
• W1981845140 cites W2037994995 @default.
• W1981845140 cites W2039249654 @default.
• W1981845140 cites W2039373764 @default.
• W1981845140 cites W2047353257 @default.
• W1981845140 cites W2053881792 @default.
• W1981845140 cites W2060070232 @default.
• W1981845140 cites W2061351626 @default.
• W1981845140 cites W2077941204 @default.
• W1981845140 cites W2078114051 @default.
• W1981845140 cites W2082146267 @default.
• W1981845140 cites W2082852727 @default.
• W1981845140 cites W2089947924 @default.
• W1981845140 cites W2090757189 @default.
• W1981845140 cites W2093961499 @default.
• W1981845140 cites W2105625415 @default.
• W1981845140 cites W2143416660 @default.
• W1981845140 cites W2152809912 @default.
• W1981845140 cites W2154494747 @default.
• W1981845140 cites W2170066557 @default.
• W1981845140 cites W2312561488 @default.
• W1981845140 cites W2334710360 @default.
• W1981845140 cites W2335459898 @default.
• W1981845140 cites W4252663299 @default.
• W1981845140 cites W4254731778 @default.
• W1981845140 cites W4300141286 @default.
• W1981845140 doi "https://doi.org/10.1016/s0967-0645(02)00100-5" @default.
• W1981845140 hasPublicationYear "2002" @default.
• W1981845140 type Work @default.
• W1981845140 sameAs 1981845140 @default.
• W1981845140 citedByCount "64" @default.
• W1981845140 countsByYear W19818451402012 @default.
• W1981845140 countsByYear W19818451402013 @default.
• W1981845140 countsByYear W19818451402014 @default.
• W1981845140 countsByYear W19818451402015 @default.
• W1981845140 countsByYear W19818451402016 @default.
• W1981845140 countsByYear W19818451402017 @default.
• W1981845140 countsByYear W19818451402018 @default.
• W1981845140 countsByYear W19818451402019 @default.
• W1981845140 countsByYear W19818451402020 @default.
• W1981845140 countsByYear W19818451402021 @default.
• W1981845140 countsByYear W19818451402022 @default.
• W1981845140 countsByYear W19818451402023 @default.
• W1981845140 crossrefType "journal-article" @default.
• W1981845140 hasAuthorship W1981845140A5001833515 @default.
• W1981845140 hasAuthorship W1981845140A5010321851 @default.
• W1981845140 hasAuthorship W1981845140A5012847386 @default.
• W1981845140 hasAuthorship W1981845140A5014861948 @default.
• W1981845140 hasAuthorship W1981845140A5034350687 @default.
• W1981845140 hasAuthorship W1981845140A5062673931 @default.
• W1981845140 hasAuthorship W1981845140A5074648456 @default.
• W1981845140 hasAuthorship W1981845140A5074761839 @default.
• W1981845140 hasAuthorship W1981845140A5076350979 @default.
• W1981845140 hasAuthorship W1981845140A5089453253 @default.
• W1981845140 hasAuthorship W1981845140A5091713611 @default.
• W1981845140 hasConcept C108469399 @default.
• W1981845140 hasConcept C111368507 @default.
• W1981845140 hasConcept C114793014 @default.
• W1981845140 hasConcept C122846477 @default.
• W1981845140 hasConcept C127313418 @default.
• W1981845140 hasConcept C139719470 @default.
• W1981845140 hasConcept C142796444 @default.
• W1981845140 hasConcept C149348798 @default.
• W1981845140 hasConcept C152382732 @default.
• W1981845140 hasConcept C158836135 @default.
• W1981845140 hasConcept C162284963 @default.

• next