Matches in SemOpenAlex for { <https://semopenalex.org/work/W2566566381> ?p ?o ?g. }
- W2566566381 endingPage "89" @default.
- W2566566381 startingPage "74" @default.
- W2566566381 abstract "Abstract The application of transfer functions on fossil assemblages to reconstruct past environments is fundamentally based on the assumption of stable environmental niches in both space and time. We quantitatively test this assumption for six dominant planktic foraminiferal species ( Globigerinoides ruber (pink), G. ruber (white), Trilobatus sacculifer , Truncorotalia truncatulinoides , Globigerina bulloides , and Neogloboquadrina pachyderma ) by contrasting reconstructions of species realized and optimum distributions in the modern and during the Last Glacial Maximum (LGM) using an ecological niche model (ENM; MaxEnt) and ordination framework. Global ecological niche models calibrated in the modern ocean have high predictive performance when projected to the LGM for subpolar and polar species, indicating that the environmental niches of these taxa are largely stable at the global scale across this interval. In contrast, ENMs had much poorer predictive performance for the optimal niche of tropical‐dwelling species, T. sacculifer and G. ruber (pink). This finding is supported by independent metrics of niche margin change, suggesting that niche stability in environmental space was greatest for (sub)polar species, with greatest expansion of the niche observed for tropical species. We find that globally calibrated ENMs showed good predictions of species occurrences globally, whereas models calibrated in either the Pacific or Atlantic Oceans only and then projected globally performed less well for T. sacculifer . Our results support the assumption of environmental niche stability over the last ~21,000 years for most of our focal planktic foraminiferal species and, thus, the application of transfer function techniques for palaeoenvironmental reconstruction during this interval. However, the lower observed niche stability for (sub)tropical taxa T. sacculifer and G. ruber (pink) suggests that (sub)tropical temperatures could be underestimated in the glacial ocean with the strongest effect in the equatorial Atlantic where both species are found today." @default.
- W2566566381 created "2017-01-06" @default.
- W2566566381 creator A5061627377 @default.
- W2566566381 creator A5066867168 @default.
- W2566566381 creator A5074514382 @default.
- W2566566381 creator A5083027838 @default.
- W2566566381 date "2017-01-01" @default.
- W2566566381 modified "2023-10-16" @default.
- W2566566381 title "Quantifying the stability of planktic foraminiferal physical niches between the Holocene and Last Glacial Maximum" @default.
- W2566566381 cites W1040565711 @default.
- W2566566381 cites W1489155911 @default.
- W2566566381 cites W1523155080 @default.
- W2566566381 cites W1548333476 @default.
- W2566566381 cites W1549142192 @default.
- W2566566381 cites W1575470282 @default.
- W2566566381 cites W1612072633 @default.
- W2566566381 cites W1755693869 @default.
- W2566566381 cites W1901684278 @default.
- W2566566381 cites W1939517098 @default.
- W2566566381 cites W1961275969 @default.
- W2566566381 cites W1966396962 @default.
- W2566566381 cites W1966811787 @default.
- W2566566381 cites W1967117311 @default.
- W2566566381 cites W1974298511 @default.
- W2566566381 cites W1975991602 @default.
- W2566566381 cites W1976474576 @default.
- W2566566381 cites W1978667390 @default.
- W2566566381 cites W1978851947 @default.
- W2566566381 cites W1980341376 @default.
- W2566566381 cites W1981566966 @default.
- W2566566381 cites W1990955220 @default.
- W2566566381 cites W1994361934 @default.
- W2566566381 cites W2001748407 @default.
- W2566566381 cites W2002435629 @default.
- W2566566381 cites W2007049610 @default.
- W2566566381 cites W2008177998 @default.
- W2566566381 cites W2008290113 @default.
- W2566566381 cites W2008401121 @default.
- W2566566381 cites W2013388152 @default.
- W2566566381 cites W2013879881 @default.
- W2566566381 cites W2019578472 @default.
- W2566566381 cites W2024229200 @default.
- W2566566381 cites W2029323798 @default.
- W2566566381 cites W2032460841 @default.
- W2566566381 cites W2033676403 @default.
- W2566566381 cites W2036199712 @default.
- W2566566381 cites W2037658781 @default.
- W2566566381 cites W2041010189 @default.
- W2566566381 cites W2043619113 @default.
- W2566566381 cites W2046669039 @default.
- W2566566381 cites W2047248056 @default.
- W2566566381 cites W2047717614 @default.
- W2566566381 cites W2051870778 @default.
- W2566566381 cites W2057950738 @default.
- W2566566381 cites W2061955941 @default.
- W2566566381 cites W2063948326 @default.
- W2566566381 cites W2073097106 @default.
- W2566566381 cites W2073208340 @default.
- W2566566381 cites W2073259396 @default.
- W2566566381 cites W2079868285 @default.
- W2566566381 cites W2080697333 @default.
- W2566566381 cites W2081840989 @default.
- W2566566381 cites W2090689755 @default.
- W2566566381 cites W2092367603 @default.
- W2566566381 cites W2095766166 @default.
- W2566566381 cites W2095774692 @default.
- W2566566381 cites W2100226004 @default.
- W2566566381 cites W2100533358 @default.
- W2566566381 cites W2100858543 @default.
- W2566566381 cites W2104843820 @default.
- W2566566381 cites W2112315008 @default.
- W2566566381 cites W2115268776 @default.
- W2566566381 cites W2118387673 @default.
- W2566566381 cites W2120160157 @default.
- W2566566381 cites W2120573898 @default.
- W2566566381 cites W2120812618 @default.
- W2566566381 cites W2121285138 @default.
- W2566566381 cites W2125029846 @default.
- W2566566381 cites W2139416101 @default.
- W2566566381 cites W2140482289 @default.
- W2566566381 cites W2141707502 @default.
- W2566566381 cites W2147717392 @default.
- W2566566381 cites W2152809912 @default.
- W2566566381 cites W2155413854 @default.
- W2566566381 cites W2156096990 @default.
- W2566566381 cites W2156212706 @default.
- W2566566381 cites W2160141904 @default.
- W2566566381 cites W2166477777 @default.
- W2566566381 cites W2176020666 @default.
- W2566566381 cites W2179336569 @default.
- W2566566381 cites W2180247159 @default.
- W2566566381 cites W2275025710 @default.
- W2566566381 cites W2318447889 @default.
- W2566566381 cites W2325833156 @default.
- W2566566381 cites W2332856963 @default.
- W2566566381 cites W2342587802 @default.
- W2566566381 cites W2497763638 @default.
- W2566566381 cites W3209802665 @default.