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PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Accumulation rates of biogenic components of ODP Hole 154-926B
The multi-proxies (BAR, bio-SiO2 MAR, and CaCO3 MAR) of productivity in Ocean Drilling Program (ODP) Leg 154 Site 926 Hole B (3°43'N, 42°54'W) during the late Miocene. Based on... -
PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Accumulation rates of biogenic components of ODP Hole 121-758A
The multi-proxies (BAR, bio-SiO2 MAR, and CaCO3 MAR) of productivity in Ocean Drilling Program (ODP) Leg 121 Site 758 Hole A (5°23.05'N, 90°21.67'E) during the late Miocene.... -
PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Carbonate mass accumulation rates from IODP Hole 371-U1506A
This dataset has no description
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PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Major element composition of IODP Site U1501 in the South China Sea from 5.2 ...
IODP Site U1501 (18°53.09′N, 115°45.95′E, water depth: 2846 m) is situated on the west side of Pearl River Canyon. The length for hole C at IODP Site U1501 is up to 461.8 m,... -
PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Late Miocene model boundary condtions
Here we present Late Miocene (~11-7 Ma) model boundary conditions used by Knorr et al. [2011] in two files (Paleogeography.nc and Surface_conditions.nc). These boundary... -
PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Multi-proxy reconstructions of productivity during the late Miocene
The Late Miocene Biogenic Bloom (LMBB), marked by notable increases in biogenic components in marine sediments, provides insights into the response of the biological pump to... -
PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Accumulation rates of benthic foraminifera from IODP Hole 371-U1506A
This dataset has no description
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PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Stable isotope (δ¹³C) of Trilobatus sacculifer from IODP Hole 371-U1506A
This dataset has no description
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PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Stable isotope (δ¹³C, δ¹⁸O) of Cibicides mundulus from IODP Hole 371-U1506A
This dataset has no description
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PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Relative group abundance of benthic foraminifera from IODP Hole 371-U1506A
This dataset has no description
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PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Relative cluster abundance of benthic foraminifera from IODP Hole 371-U1506A
This dataset has no description
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PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Oxygenated bottom water conditions on Broken Ridge (central Indian Ocean) in ...
The late Miocene and early Pliocene were marked by widespread oxygen depletion in the Pacific and Indian Oceans in conjunction with the so-called "Late Miocene Biogenic Bloom"... -
PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Benthic foraminifera relative abundance and enhanced benthic foraminifera oxy...
Relative abundance of benthic foraminifera genera from IODP Site U1488, western equatorial Pacific Ocean. The dataset spans the Late Miocene-Early Pliocene interval, from 8.7 to... -
PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Late Pleistocene δ¹¹B based carbon dioxide levels from ODP Site 154-926
Earth's climate cooled markedly during the Late Miocene from 12 to 5 million years ago, with far-reaching consequences for global ecosystems. However, the driving forces of... -
PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Mg/Ca ratios measured on planktic foraminifera species and reconstructed Sea ...
During the late Miocene, global cooling occurred alongside the establishment of near-modern terrestrial and marine ecosystems. Significant (3 to 5 °C) sea surface cooling from... -
PANGAEA (Data Publisher for Earth & Environmental Science)
Imported
Opal contents at IODP U1417 (Gulf of Alaska) during Late Miocne to Early Plei...
International Ocean Discovery Program Site U1417 in the Surveyor (Gulf of Alaska) preserves the hemi-pelagic sediments influenced by the glacial and fluvi-al depositional from...
