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- W2289132008 endingPage "20150224" @default.
- W2289132008 startingPage "20150224" @default.
- W2289132008 abstract "The Cenozoic planktonic foraminifera (PF) (calcareous zooplankton) have arguably the most detailed fossil record of any group. The quality of this record allows models of environmental controls on macroecology, developed for Recent assemblages, to be tested on intervals with profoundly different climatic conditions. These analyses shed light on the role of long-term global cooling in establishing the modern latitudinal diversity gradient (LDG)—one of the most powerful generalizations in biogeography and macroecology. Here, we test the transferability of environment-diversity models developed for modern PF assemblages to the Eocene epoch (approx. 56–34 Ma), a time of pronounced global warmth. Environmental variables from global climate models are combined with Recent environment–diversity models to predict Eocene richness gradients, which are then compared with observed patterns. The results indicate the modern LDG—lower richness towards the poles—developed through the Eocene. Three possible causes are suggested for the mismatch between statistical model predictions and data in the Early Eocene: the environmental estimates are inaccurate, the statistical model misses a relevant variable, or the intercorrelations among facets of diversity—e.g. richness, evenness, functional diversity—have changed over geological time. By the Late Eocene, environment–diversity relationships were much more similar to those found today." @default.
- W2289132008 created "2016-06-24" @default.
- W2289132008 creator A5005369163 @default.
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- W2289132008 creator A5030701670 @default.
- W2289132008 creator A5061956568 @default.
- W2289132008 creator A5069811512 @default.
- W2289132008 date "2016-04-05" @default.
- W2289132008 modified "2023-10-10" @default.
- W2289132008 title "The impact of Cenozoic cooling on assemblage diversity in planktonic foraminifera" @default.
- W2289132008 cites W1531553460 @default.
- W2289132008 cites W1603378435 @default.
- W2289132008 cites W1612072633 @default.
- W2289132008 cites W1614214072 @default.
- W2289132008 cites W1664106343 @default.
- W2289132008 cites W1724522583 @default.
- W2289132008 cites W1859465057 @default.
- W2289132008 cites W1935868227 @default.
- W2289132008 cites W1963379118 @default.
- W2289132008 cites W1964974843 @default.
- W2289132008 cites W1967252261 @default.
- W2289132008 cites W1970779668 @default.
- W2289132008 cites W1979486458 @default.
- W2289132008 cites W1984188157 @default.
- W2289132008 cites W1984961131 @default.
- W2289132008 cites W1986969158 @default.
- W2289132008 cites W1989146507 @default.
- W2289132008 cites W1992325342 @default.
- W2289132008 cites W1994060496 @default.
- W2289132008 cites W1998843668 @default.
- W2289132008 cites W1999638079 @default.
- W2289132008 cites W2001748407 @default.
- W2289132008 cites W2003019046 @default.
- W2289132008 cites W2006959409 @default.
- W2289132008 cites W2008811990 @default.
- W2289132008 cites W2009590780 @default.
- W2289132008 cites W2011657860 @default.
- W2289132008 cites W2016325533 @default.
- W2289132008 cites W2020571159 @default.
- W2289132008 cites W2021408515 @default.
- W2289132008 cites W2024032230 @default.
- W2289132008 cites W2028572537 @default.
- W2289132008 cites W2034357743 @default.
- W2289132008 cites W2034519944 @default.
- W2289132008 cites W2035253017 @default.
- W2289132008 cites W2036199712 @default.
- W2289132008 cites W2041010189 @default.
- W2289132008 cites W2043619113 @default.
- W2289132008 cites W2044435308 @default.
- W2289132008 cites W2046948141 @default.
- W2289132008 cites W2050597362 @default.
- W2289132008 cites W2055442076 @default.
- W2289132008 cites W2064187509 @default.
- W2289132008 cites W2065871027 @default.
- W2289132008 cites W2069397196 @default.
- W2289132008 cites W2073551687 @default.
- W2289132008 cites W2075429173 @default.
- W2289132008 cites W2083189830 @default.
- W2289132008 cites W2087189381 @default.
- W2289132008 cites W2087699297 @default.
- W2289132008 cites W2093009406 @default.
- W2289132008 cites W2094849893 @default.
- W2289132008 cites W2095018223 @default.
- W2289132008 cites W2097547447 @default.
- W2289132008 cites W2099629218 @default.
- W2289132008 cites W2100858543 @default.
- W2289132008 cites W2101224191 @default.
- W2289132008 cites W2101283217 @default.
- W2289132008 cites W2102299211 @default.
- W2289132008 cites W2104767862 @default.
- W2289132008 cites W2104910083 @default.
- W2289132008 cites W2104969110 @default.
- W2289132008 cites W2105838375 @default.
- W2289132008 cites W2107986998 @default.
- W2289132008 cites W2112600318 @default.
- W2289132008 cites W2114795157 @default.
- W2289132008 cites W2119182375 @default.
- W2289132008 cites W2120812618 @default.
- W2289132008 cites W2123462919 @default.
- W2289132008 cites W2123694424 @default.
- W2289132008 cites W2124408914 @default.
- W2289132008 cites W2130653110 @default.
- W2289132008 cites W2136506315 @default.
- W2289132008 cites W2140595946 @default.
- W2289132008 cites W2141282655 @default.
- W2289132008 cites W2141846515 @default.
- W2289132008 cites W2142834673 @default.
- W2289132008 cites W2143644603 @default.
- W2289132008 cites W2146562456 @default.
- W2289132008 cites W2147544980 @default.
- W2289132008 cites W2148665127 @default.
- W2289132008 cites W2149772679 @default.
- W2289132008 cites W2150741383 @default.
- W2289132008 cites W2155413854 @default.
- W2289132008 cites W2157452947 @default.
- W2289132008 cites W2158311065 @default.