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2 results for “International Ocean Discovery Program”

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zenodo32/100

First record of oceanic anoxic event 1d at southern high latitudes: Sedimentary and geochemical evidence from International Ocean Discovery Program Expedition 369

<p>Oceanic anoxic event&nbsp;1d (OAE 1d) has been well studied&nbsp;at northern low&nbsp;latitudes (i.e., in Tethys and&nbsp;the&nbsp;North&nbsp;Atlantic); however,&nbsp;the paleoenvironmental response associated with this event at high latitudes&nbsp;has not been documented and the trigger mechanism&nbsp;remains unknown. Here, we&nbsp;address both of these shortcomings by&nbsp;presenting&nbsp;the first detailed sedimentary and geochemical multi-proxy records of the OAE 1d at southern high latitudes (60-62&deg;S), obtained from sediments at Site U1513, IODP Expedition 369.&nbsp;In particular, the record of sedimentary mercury proxy reveals that OAE 1d is associated with the Central Kerguelen large igneous province volcanism.&nbsp;Furthermore, the significant increase in continental runoff and consequent terrigenous input&nbsp;for&nbsp;southwestern Australia&nbsp;in the southeastern proto-India Ocean&nbsp;might&nbsp;have resulted regionally in weakened bottom-water oxygenation and strengthened organic matter burial during OAE 1d. Oceanic anoxic event&nbsp;1d (OAE 1d) has been well studied&nbsp;at northern low&nbsp;latitudes (i.e., in Tethys and&nbsp;the&nbsp;North&nbsp;Atlantic); however,&nbsp;the paleoenvironmental response associated with this event at high latitudes&nbsp;has not been documented and the trigger mechanism&nbsp;remains unknown. Here, we&nbsp;address both of these shortcomings by&nbsp;presenting&nbsp;the first detailed sedimentary and geochemical multi-proxy records of the OAE 1d at southern high latitudes (60-62&deg;S), obtained from sediments at Site U1513, IODP Expedition 369.&nbsp;In particular, the record of sedimentary mercury proxy reveals that OAE 1d is associated with the Central Kerguelen large igneous province volcanism.&nbsp;Furthermore, the significant increase in continental runoff and consequent terrigenous input&nbsp;for&nbsp;southwestern Australia&nbsp;in the southeastern proto-India Ocean&nbsp;might&nbsp;have resulted regionally in weakened bottom-water oxygenation and strengthened organic matter burial during OAE 1d.</p>

opencc-by-4.0Mar 2022View details →
zenodo28/100

Complete supplementary data related to palynological research of International Ocean Discovery Program (IODP) Expedition 364

<p>Supplemental data relating to Vann Smith&#39;s 2020 dissertation at Louisiana State University</p>

opencc-by-4.0Apr 2020View details →

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