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- W2923177917 abstract "The Pliocene was characterized by a gradual shift of global climate toward cooler and drier conditions. This shift fundamentally reorganized Earth's climate from the Miocene state toward conditions similar to the present. During the Pliocene, the progressive restriction of the Indonesian Throughflow (ITF) is suggested to have enhanced this shift toward stronger meridional thermal gradients. Reduced ITF, caused by the northward movement of Australia and uplift of Indonesia, impeded global thermohaline circulation, also contributing to late Pliocene Northern Hemisphere cooling via atmospheric and oceanographic teleconnections. Here we present an orbitally tuned high-resolution sediment geochemistry, calcareous nannofossil, and X-ray fluorescence record between 3.65 and 2.97 Ma from the northwest shelf of Australia within the Leeuwin Current. International Ocean Discovery Program Site U1463 provides a record of local surface water conditions and Australian climate in relation to changing ITF connectivity. Modern analogue-based interpretations of nannofossil assemblages indicate that ITF configuration culminated ~3.54 Ma. A decrease in warm, oligotrophic taxa such as Umbilicosphaera sibogae, with a shift from Gephyrocapsa sp. to Reticulofenestra sp., and an increase of mesotrophic taxa (e.g., Umbilicosphaera jafari and Helicosphaera spp.) suggest that tropical Pacific ITF sources were replaced by cooler, fresher, northern Pacific waters. This initial tectonic reorganization enhanced the Indian Oceans sensitivity to orbitally forced cooling in the southern high latitudes culminating in the M2 glacial event (~3.3 Ma). After 3.3 Ma the restructured ITF established the boundary conditions for the inception of the Sahul-Indian Ocean Bjerknes mechanism and increased the response to glacio-eustatic variability." @default.
- W2923177917 created "2019-04-01" @default.
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- W2923177917 date "2019-04-01" @default.
- W2923177917 modified "2023-10-16" @default.
- W2923177917 title "Timing and Pacing of Indonesian Throughflow Restriction and Its Connection to Late Pliocene Climate Shifts" @default.
- W2923177917 cites W1480411523 @default.
- W2923177917 cites W1482359583 @default.
- W2923177917 cites W1501100918 @default.
- W2923177917 cites W1511465418 @default.
- W2923177917 cites W1541334608 @default.
- W2923177917 cites W1558339174 @default.
- W2923177917 cites W1590681844 @default.
- W2923177917 cites W1614573089 @default.
- W2923177917 cites W1617498520 @default.
- W2923177917 cites W1625329436 @default.
- W2923177917 cites W1631559605 @default.
- W2923177917 cites W1848101001 @default.
- W2923177917 cites W1891540596 @default.
- W2923177917 cites W1958949482 @default.
- W2923177917 cites W1965142992 @default.
- W2923177917 cites W1966232279 @default.
- W2923177917 cites W1967649645 @default.
- W2923177917 cites W1968726430 @default.
- W2923177917 cites W1968988439 @default.
- W2923177917 cites W1971681662 @default.
- W2923177917 cites W1976015417 @default.
- W2923177917 cites W1978585247 @default.
- W2923177917 cites W1978694048 @default.
- W2923177917 cites W1980130942 @default.
- W2923177917 cites W1980336881 @default.
- W2923177917 cites W1980867451 @default.
- W2923177917 cites W1981709236 @default.
- W2923177917 cites W1985505543 @default.
- W2923177917 cites W1985619924 @default.
- W2923177917 cites W1990111902 @default.
- W2923177917 cites W1990468655 @default.
- W2923177917 cites W1994317552 @default.
- W2923177917 cites W1998521937 @default.
- W2923177917 cites W2000881839 @default.
- W2923177917 cites W2002382675 @default.
- W2923177917 cites W2005428926 @default.
- W2923177917 cites W2005812671 @default.
- W2923177917 cites W2006547330 @default.
- W2923177917 cites W2008353131 @default.
- W2923177917 cites W2008742345 @default.
- W2923177917 cites W2011114075 @default.
- W2923177917 cites W2013154469 @default.
- W2923177917 cites W2013399212 @default.
- W2923177917 cites W2016381774 @default.
- W2923177917 cites W2022195039 @default.
- W2923177917 cites W2024669465 @default.
- W2923177917 cites W2026889945 @default.
- W2923177917 cites W2027848164 @default.
- W2923177917 cites W2030344225 @default.
- W2923177917 cites W2033356481 @default.
- W2923177917 cites W2033735582 @default.
- W2923177917 cites W2042945306 @default.
- W2923177917 cites W2045059239 @default.
- W2923177917 cites W2048641142 @default.
- W2923177917 cites W2052001254 @default.
- W2923177917 cites W2062853562 @default.
- W2923177917 cites W2065073115 @default.
- W2923177917 cites W2067934106 @default.
- W2923177917 cites W2068365898 @default.
- W2923177917 cites W2068449011 @default.
- W2923177917 cites W2068491640 @default.
- W2923177917 cites W2069459176 @default.
- W2923177917 cites W2072618142 @default.
- W2923177917 cites W2072935186 @default.
- W2923177917 cites W2073287004 @default.
- W2923177917 cites W2074476857 @default.
- W2923177917 cites W2074883227 @default.
- W2923177917 cites W2075330616 @default.
- W2923177917 cites W2076464133 @default.
- W2923177917 cites W2083201546 @default.
- W2923177917 cites W2084368762 @default.
- W2923177917 cites W2087822101 @default.
- W2923177917 cites W2088636794 @default.
- W2923177917 cites W2091893697 @default.
- W2923177917 cites W2092012163 @default.
- W2923177917 cites W2092543864 @default.
- W2923177917 cites W2099549534 @default.
- W2923177917 cites W2099826005 @default.
- W2923177917 cites W2102397700 @default.
- W2923177917 cites W2103272092 @default.
- W2923177917 cites W2105118013 @default.