Sub-Milankovich millennial cycles in proxy (UK37) sea surface temperatures for the Okinawa trough, W Mediterranean Sea, NW Atlantic Ocean and Southern Ocean
Sea surface paleo-temperatures for the Holocene deduced using the UK37 proxy are studied for four sites; the Okinawa trough (IODP hole 1202B); western Mediterranean Sea (Core 293G); NW Atlantic ocean (off-shore Portugal Core MD95-2042); Southern Ocean (off-shore S Australia, Murray Canyon, core MD03...
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Format: | Conference Object |
Language: | English |
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2018
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Online Access: | https://research.monash.edu/en/publications/7470eeb9-1576-4db3-ae2f-986afa4181bc https://researchmgt.monash.edu/ws/files/263378165/259296541_oa.pdf https://meetingorganizer.copernicus.org/EGU2018/EGU2018-12541.pdf |