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• W2260892310 endingPage "240" @default.
• W2260892310 startingPage "213" @default.
• W2260892310 abstract "Abstract. The Forada section (northeastern Italy) provides a continuous, expanded deep-sea record of the Paleocene–Eocene Thermal Maximum (PETM) in the central-western Tethys. We combine a new, high-resolution, benthic foraminiferal assemblage record with published calcareous plankton, mineralogical and biomarker data to document climatic and environmental changes across the PETM, highlighting the benthic foraminiferal extinction event (BEE). The onset of the PETM, occurring ∼ 30 kyr after a precursor event, is marked by a thin, black, barren clay layer, possibly representing a brief pulse of anoxia and carbonate dissolution. The BEE occurred within the 10 cm interval including this layer. During the first 3.5 kyr of the PETM, several agglutinated recolonizing taxa show rapid species turnover, indicating a highly unstable, CaCO3-corrosive environment. Calcareous taxa reappeared after this interval, and the next ∼9 kyr were characterized by rapid alternation of peaks in abundance of various calcareous and agglutinated recolonizers. These observations suggest that synergistic stressors, including deepwater CaCO3 corrosiveness, low oxygenation, and high environmental instability caused the extinction. Combined faunal and biomarker data (BIT index, higher plant n-alkane average chain length) and the high abundance of the mineral chlorite suggest that erosion and weathering increased strongly at the onset of the PETM, due to an overall wet climate with invigorated hydrological cycle, which led to storm flood events carrying massive sediment discharge into the Belluno Basin. This interval was followed by the core of the PETM, characterized by four precessionally paced cycles in CaCO3 %, hematite %, δ13C, abundant occurrence of opportunistic benthic foraminiferal taxa, and calcareous nannofossil and planktonic foraminiferal taxa typical of high-productivity environments, radiolarians, and lower δDn-alkanes. We interpret these cycles as reflecting alternation between an overall arid climate, characterized by strong winds and intense upwelling, and an overall humid climate, with abundant rains and high sediment delivery (including refractory organic carbon) from land. Precessionally paced marl–limestone couplets occur throughout the recovery interval of the carbon isotope excursion (CIE) and up to 10 m above it, suggesting that these wet–dry cycles persisted, though at declining intensity, after the peak PETM. Enhanced climate extremes at mid-latitudes might have been a direct response to the massive CO2 input in the ocean atmosphere system at the Paleocene–Eocene transition, and may have had a primary role in restoring the Earth system to steady state." @default.
• W2260892310 created "2016-06-24" @default.
• W2260892310 creator A5064740314 @default.
• W2260892310 creator A5076759446 @default.
• W2260892310 creator A5082968355 @default.
• W2260892310 date "2016-02-09" @default.
• W2260892310 modified "2023-10-16" @default.
• W2260892310 title "Variability in climate and productivity during the Paleocene–Eocene Thermal Maximum in the western Tethys (Forada section)" @default.
• W2260892310 cites W1481261509 @default.
• W2260892310 cites W1507246280 @default.
• W2260892310 cites W1508364750 @default.
• W2260892310 cites W1548303926 @default.
• W2260892310 cites W1553208841 @default.
• W2260892310 cites W1553861208 @default.
• W2260892310 cites W1554688948 @default.
• W2260892310 cites W1580683189 @default.
• W2260892310 cites W1582909710 @default.
• W2260892310 cites W1584064745 @default.
• W2260892310 cites W1587430167 @default.
• W2260892310 cites W1598075842 @default.
• W2260892310 cites W1598314256 @default.
• W2260892310 cites W1632286192 @default.
• W2260892310 cites W178456859 @default.
• W2260892310 cites W1802793573 @default.
• W2260892310 cites W1829730549 @default.
• W2260892310 cites W1877298222 @default.
• W2260892310 cites W1964116684 @default.
• W2260892310 cites W1964126829 @default.
• W2260892310 cites W1965072994 @default.
• W2260892310 cites W1965472552 @default.
• W2260892310 cites W1965811169 @default.
• W2260892310 cites W1966360142 @default.
• W2260892310 cites W1967025504 @default.
• W2260892310 cites W1968409576 @default.
• W2260892310 cites W1968620739 @default.
• W2260892310 cites W1975122465 @default.
• W2260892310 cites W1975256453 @default.
• W2260892310 cites W1976215537 @default.
• W2260892310 cites W1976550053 @default.
• W2260892310 cites W1978894916 @default.
• W2260892310 cites W1980257118 @default.
• W2260892310 cites W1980265204 @default.
• W2260892310 cites W1981818426 @default.
• W2260892310 cites W1983360446 @default.
• W2260892310 cites W1983794578 @default.
• W2260892310 cites W1985294064 @default.
• W2260892310 cites W1985654786 @default.
• W2260892310 cites W1986363924 @default.
• W2260892310 cites W1987162112 @default.
• W2260892310 cites W1987710402 @default.
• W2260892310 cites W1987869680 @default.
• W2260892310 cites W1988054149 @default.
• W2260892310 cites W1989241939 @default.
• W2260892310 cites W1989279896 @default.
• W2260892310 cites W1989728222 @default.
• W2260892310 cites W1990366259 @default.
• W2260892310 cites W1991143586 @default.
• W2260892310 cites W1993332262 @default.
• W2260892310 cites W1994271054 @default.
• W2260892310 cites W1996417990 @default.
• W2260892310 cites W1998378984 @default.
• W2260892310 cites W1999583990 @default.
• W2260892310 cites W2000246025 @default.
• W2260892310 cites W2002027097 @default.
• W2260892310 cites W2002615691 @default.
• W2260892310 cites W2002706814 @default.
• W2260892310 cites W2004318778 @default.
• W2260892310 cites W2004782345 @default.
• W2260892310 cites W2004861625 @default.
• W2260892310 cites W2006828330 @default.
• W2260892310 cites W2006926850 @default.
• W2260892310 cites W2008450675 @default.
• W2260892310 cites W2010350484 @default.
• W2260892310 cites W2014080039 @default.
• W2260892310 cites W2014746345 @default.
• W2260892310 cites W2015891195 @default.
• W2260892310 cites W2016225258 @default.
• W2260892310 cites W2017212463 @default.
• W2260892310 cites W2017922709 @default.
• W2260892310 cites W2018445931 @default.
• W2260892310 cites W2018732069 @default.
• W2260892310 cites W2019142165 @default.
• W2260892310 cites W2019433019 @default.
• W2260892310 cites W2019600437 @default.
• W2260892310 cites W2021408515 @default.
• W2260892310 cites W2022508325 @default.
• W2260892310 cites W2023021226 @default.
• W2260892310 cites W2024597018 @default.
• W2260892310 cites W2026051854 @default.
• W2260892310 cites W2026823059 @default.
• W2260892310 cites W2027177856 @default.
• W2260892310 cites W2028745742 @default.
• W2260892310 cites W2033052384 @default.
• W2260892310 cites W2037528795 @default.
• W2260892310 cites W2038285860 @default.
• W2260892310 cites W2046619810 @default.
• W2260892310 cites W2047899760 @default.
• W2260892310 cites W2048005816 @default.

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