FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2921088442> ?p ?o ?g. }

• W2921088442 endingPage "3437" @default.
• W2921088442 startingPage "3425" @default.
• W2921088442 abstract "Abstract. Neogloboquadrina pachyderma is the dominant planktonic foraminifera species in the polar regions. In the northern high-latitude ocean, it makes up more than 90 % of the total assemblages, making it the dominant pelagic calcifier and carrier of paleoceanographic proxies. To assess the reaction of this species to a future shaped by climate change and to be able to interpret the paleoecological signal contained in its shells, its depth habitat must be known. Previous work showed that N. pachyderma in the northern polar regions has a highly variable depth habitat, ranging from the surface mixed layer to several hundreds of metres below the surface, and the origin of this variability remained unclear. In order to investigate the factors controlling the depth habitat of N. pachyderma, we compiled new and existing population density profiles from 104 stratified plankton tow hauls collected in the Arctic and the North Atlantic oceans during 14 oceanographic expeditions. For each vertical profile, the depth habitat (DH) was calculated as the abundance-weighted mean depth of occurrence. We then tested to what degree environmental factors (mixed-layer depth, sea surface temperature, sea surface salinity, chlorophyll a concentration, and sea ice concentration) and ecological factors (synchronized reproduction and daily vertical migration) can predict the observed DH variability and compared the observed DH behaviour with simulations by a numerical model predicting planktonic foraminifera distribution. Our data show that the DH of N. pachyderma varies between 25 and 280 m (average ∼100 m). In contrast with the model simulations, which indicate that DH is associated with the depth of chlorophyll maximum, our analysis indicates that the presence of sea ice together with the concentration of chlorophyll a at the surface have the strongest influence on the vertical habitat of this species. N. pachyderma occurs deeper when sea ice and chlorophyll concentrations are low, suggesting a time-transgressive response to the evolution of (near) surface conditions during the annual cycle. Since only surface parameters appear to affect the vertical habitat of N. pachyderma, light or light-dependant processes might influence the ecology of this species. Our results can be used to improve predictions of the response of the species to climate change and thus to refine paleoclimatic reconstructions." @default.
• W2921088442 created "2019-03-22" @default.
• W2921088442 creator A5033371043 @default.
• W2921088442 creator A5052942659 @default.
• W2921088442 creator A5053519683 @default.
• W2921088442 creator A5056886068 @default.
• W2921088442 creator A5059774472 @default.
• W2921088442 date "2019-09-12" @default.
• W2921088442 modified "2023-10-14" @default.
• W2921088442 title "Depth habitat of the planktonic foraminifera &lt;i&gt;Neogloboquadrina pachyderma&lt;/i&gt; in the northern high latitudes explained by sea-ice and chlorophyll concentrations" @default.
• W2921088442 cites W1429673265 @default.
• W2921088442 cites W1504009252 @default.
• W2921088442 cites W1964328088 @default.
• W2921088442 cites W1968420924 @default.
• W2921088442 cites W1974298511 @default.
• W2921088442 cites W1974961819 @default.
• W2921088442 cites W1992187641 @default.
• W2921088442 cites W2023424529 @default.
• W2921088442 cites W2026985846 @default.
• W2921088442 cites W2032460841 @default.
• W2921088442 cites W2034453126 @default.
• W2921088442 cites W2044677507 @default.
• W2921088442 cites W2047274059 @default.
• W2921088442 cites W2051705212 @default.
• W2921088442 cites W2052620279 @default.
• W2921088442 cites W2063242400 @default.
• W2921088442 cites W2069197937 @default.
• W2921088442 cites W2070813616 @default.
• W2921088442 cites W2072151199 @default.
• W2921088442 cites W2079979380 @default.
• W2921088442 cites W2093669266 @default.
• W2921088442 cites W2104662774 @default.
• W2921088442 cites W2110646059 @default.
• W2921088442 cites W2113334140 @default.
• W2921088442 cites W2132460591 @default.
• W2921088442 cites W2143034401 @default.
• W2921088442 cites W2148972443 @default.
• W2921088442 cites W2155115995 @default.
• W2921088442 cites W2157370405 @default.
• W2921088442 cites W2160215857 @default.
• W2921088442 cites W2163558759 @default.
• W2921088442 cites W2165990255 @default.
• W2921088442 cites W2320724691 @default.
• W2921088442 cites W2522906567 @default.
• W2921088442 cites W2594800658 @default.
• W2921088442 cites W2750001334 @default.
• W2921088442 cites W2768649309 @default.
• W2921088442 cites W2787316635 @default.
• W2921088442 cites W2789674842 @default.
• W2921088442 cites W2803600541 @default.
• W2921088442 cites W2896775987 @default.
• W2921088442 cites W2914481998 @default.
• W2921088442 cites W4245021615 @default.
• W2921088442 cites W4300141286 @default.
• W2921088442 doi "https://doi.org/10.5194/bg-16-3425-2019" @default.
• W2921088442 hasPublicationYear "2019" @default.
• W2921088442 type Work @default.
• W2921088442 sameAs 2921088442 @default.
• W2921088442 citedByCount "37" @default.
• W2921088442 countsByYear W29210884422019 @default.
• W2921088442 countsByYear W29210884422020 @default.
• W2921088442 countsByYear W29210884422021 @default.
• W2921088442 countsByYear W29210884422022 @default.
• W2921088442 countsByYear W29210884422023 @default.
• W2921088442 crossrefType "journal-article" @default.
• W2921088442 hasAuthorship W2921088442A5033371043 @default.
• W2921088442 hasAuthorship W2921088442A5052942659 @default.
• W2921088442 hasAuthorship W2921088442A5053519683 @default.
• W2921088442 hasAuthorship W2921088442A5056886068 @default.
• W2921088442 hasAuthorship W2921088442A5059774472 @default.
• W2921088442 hasBestOaLocation W29210884421 @default.
• W2921088442 hasConcept C108469399 @default.
• W2921088442 hasConcept C111368507 @default.
• W2921088442 hasConcept C122523270 @default.
• W2921088442 hasConcept C127313418 @default.
• W2921088442 hasConcept C129513315 @default.
• W2921088442 hasConcept C13280743 @default.
• W2921088442 hasConcept C136894858 @default.
• W2921088442 hasConcept C144024400 @default.
• W2921088442 hasConcept C149923435 @default.
• W2921088442 hasConcept C2780368712 @default.
• W2921088442 hasConcept C2908647359 @default.
• W2921088442 hasConcept C39432304 @default.
• W2921088442 hasConcept C77942228 @default.
• W2921088442 hasConcept C83042747 @default.
• W2921088442 hasConceptScore W2921088442C108469399 @default.
• W2921088442 hasConceptScore W2921088442C111368507 @default.
• W2921088442 hasConceptScore W2921088442C122523270 @default.
• W2921088442 hasConceptScore W2921088442C127313418 @default.
• W2921088442 hasConceptScore W2921088442C129513315 @default.
• W2921088442 hasConceptScore W2921088442C13280743 @default.
• W2921088442 hasConceptScore W2921088442C136894858 @default.
• W2921088442 hasConceptScore W2921088442C144024400 @default.
• W2921088442 hasConceptScore W2921088442C149923435 @default.
• W2921088442 hasConceptScore W2921088442C2780368712 @default.
• W2921088442 hasConceptScore W2921088442C2908647359 @default.
• W2921088442 hasConceptScore W2921088442C39432304 @default.
• W2921088442 hasConceptScore W2921088442C77942228 @default.

• next