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  • AGE; DEPTH, sediment/rock; Foraminifera; foraminifera oxygen isotopes. Late Quaternary; Giant piston corer; Globigerinoides ruber, Magnesium/Calcium ratio; Globigerinoides ruber, δ18O; GPC; KX22-4; KX97322-4; Mg/Ca paleothermometry; Neogloboquadrina dutertrei, Magnesium/Calcium ratio; Neogloboquadrina dutertrei, δ18O; Sea sub-surface salinity; Sea sub-surface temperature; Sea surface salinity; Sea surface salinity, difference; Sea surface temperature; Temperature, difference; West Pacific Warm Pool; δ18O, seawater, reconstructed; δ18O, seawater, reconstructed, difference; δ18O, seawater, reconstructed, residual  (1)
  • AWI_Paleo; Biomarker; Japan Sea; Last Glacial; LV53-19-1; North Pacific; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; paleo-oceanography; PC; Piston corer; sea-level; SST; TEX86; UK'37; upper ocean  (1)
  • OMEXII-9K_2; Tropical North Atlantic  (1)
Document type
Keywords
Publisher
Years
  • 1
    Publication Date: 2023-03-30
    Description: We obtained Core KX97322-4 (00°01.73′S, 159°14.66′E, 2362 m) from the Ontong Java Plateau in the central WPWP using a giant piston corer on the Science-1 vessel during the Warm Pool Subject Cruise executed in 2008. The sedimentation rate is 0.39–4.95 cm kyr^-1^, with an average time resolution of 0.57 kyr cm^-1^. The age model was established based on downcore stable oxygen isotope measurements on the benthic foraminifer Cibicidoides wuellerstorfi (〉500 μm) correlated with the reference benthic stack LR04 using Match 2.3.1 software, combined with five accelerator mass spectrometry radiocarbon (^14^C) dates on the planktonic foraminifer Trilobatus sacculifer (with a sac) (350–500 μm) measured at the National Ocean Sciences Accelerator Mass Spectrometry facility, Woods Hole Oceanographic Institution, USA. We measured stable oxygen isotope and Mg/Ca ratio of planktic foraminifera Globigerinoides ruber and Neogloboquadrina dutertrei at the Institute of Oceanology, Chinese Academy of Sciences (IOCAS), using GV IsoPrime mass spectrometer and inductively coupled plasma-optical emission spectrometry (ICP-OES, Thermo-Fisher, iCAP6300 radial) to rebuild paleo-temperature and salinity of the central western Pacific warm pool during the last 360, 000 years, aiming to probe paleo-ENSO progress in late Quaternary.
    Keywords: AGE; DEPTH, sediment/rock; Foraminifera; foraminifera oxygen isotopes. Late Quaternary; Giant piston corer; Globigerinoides ruber, Magnesium/Calcium ratio; Globigerinoides ruber, δ18O; GPC; KX22-4; KX97322-4; Mg/Ca paleothermometry; Neogloboquadrina dutertrei, Magnesium/Calcium ratio; Neogloboquadrina dutertrei, δ18O; Sea sub-surface salinity; Sea sub-surface temperature; Sea surface salinity; Sea surface salinity, difference; Sea surface temperature; Temperature, difference; West Pacific Warm Pool; δ18O, seawater, reconstructed; δ18O, seawater, reconstructed, difference; δ18O, seawater, reconstructed, residual
    Type: Dataset
    Format: text/tab-separated-values, 9271 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-06-27
    Description: Paleoceanographic evidence commonly indicates that Last Glacial Maximum surface temperatures in the Japan Sea were comparable to modern conditions, in striking difference to colder neighboring regions. Here, based on a core from the central Japan Sea, our results show similar UK′37- and TEXL86-derived temperatures between 24.7-16.3 ka BP, followed by an abrupt divergence at ~16.3 ka BP and a weakening of divergence after ~ 8.7 ka BP. We attribute this process to a highly stratified glacial upper ocean controlled by the East Asian Summer Monsoon, increasing thermal gradient between surface and subsurface layers during the deglaciation and the intrusion of Tsushima Warm Current since the mid Holocene, respectively. Therefore, we suggest threshold-like changes in upper-ocean temperatures linked to sea-level rise and monsoon dynamics, rather than just sea surface temperatures, play a critical role in shaping the thermal and ventilation history of this NW Pacific marginal sea.
    Keywords: AWI_Paleo; Biomarker; Japan Sea; Last Glacial; LV53-19-1; North Pacific; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; paleo-oceanography; PC; Piston corer; sea-level; SST; TEX86; UK'37; upper ocean
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Hendry, Katharine R; Gong, Xun; Knorr, Gregor; Pike, Jennifer; Hall, Ian R (2016): Deglacial diatom production in the tropical North Atlantic driven by enhanced silicic acid supply. Earth and Planetary Science Letters, 438, 122-129, https://doi.org/10.1016/j.epsl.2016.01.016
    Publication Date: 2024-02-08
    Description: This data release contains stable silicon isotope data from sponge spicules isolated from sediment core OMEXII-9K off the Iberian Margin, from 0 to 336cm, and an updated age model.
    Keywords: OMEXII-9K_2; Tropical North Atlantic
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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