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  • PANGAEA  (14)
  • Elsevier  (4)
  • 2010-2014  (18)
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Year
  • 11
    Publication Date: 2024-02-29
    Keywords: Age, 14C AMS; Age, 14C calibrated; Age, dated; Age, dated standard deviation; Atlantic; BC; Box corer; Calendar age; Calendar age, standard deviation; DEPTH, sediment/rock; Elevation of event; Event label; GC; Gravity corer; INMD; INMD-111BX; INMD-113BX; INMD-115BX; Latitude of event; Longitude of event; Melville; PC; Piston corer; RC13; RC13-190; RC24; RC24-11; RC24-17; RC24-2; RC24-8GC; Reference/source; Robert Conrad; V16; V16-21; V19; V19-308; V20; V20-234; V22; V22-174; V25; V25-59; V25-60; V27; V27-161; V27-263; V27-267; V29; V29-178; V30; V30-40; V30-41; V30-96; V30-97; V32; V32-67; Vema
    Type: Dataset
    Format: text/tab-separated-values, 115 data points
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  • 12
    Publication Date: 2024-02-29
    Keywords: Atlantic; Atlantic Ocean; BC; Box corer; DEPTH, sediment/rock; Elevation of event; Event label; Globorotalia tumida, δ13C; Globorotalia tumida, δ18O; INMD; INMD-111BX; INMD-113BX; Latitude of event; Longitude of event; Mass spectrometer Fisons Optima; Melville; PC; Piston corer; RC08; RC08-18; RC08-19; RC11; RC1112; RC11-17; RC13; RC13-188; RC13-189; RC13-190; RC13-210; RC16; RC16-77; RC24; RC24-1; RC24-11; RC24-13; RC24-15; RC24-16; RC24-17; RC24-19; RC24-21; RC24-7; Robert Conrad; Sample ID; V10; V10-93; V14; V14-2; V14-5; V16; V16-203; V16-205; V16-206; V16-21; V16-22; V16-35; V16-37; V17; V17-165; V20; V20-230; V20-233; V20-234; V22; V22-169; V22-174; V22-175; V22-179; V22-182; V22-202; V22-219; V22-30; V22-31; V22-32; V25; V25-44; V25-50; V25-59; V25-60; V26; V26-102; V26-99; V27; V27-181; V27-267; V30; V30-40; V30-41; V32; V32-67; Vema
    Type: Dataset
    Format: text/tab-separated-values, 303 data points
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  • 13
    Publication Date: 2024-02-29
    Keywords: Atlantic; BC; Box corer; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; GC; Gravity corer; INMD; INMD-111BX; INMD-113BX; Latitude of event; Longitude of event; Mass spectrometer Fisons Optima; Melville; Neogloboquadrina dutertrei, δ13C; Neogloboquadrina dutertrei, δ18O; PC; Piston corer; RC11; RC1112; RC11-17; RC13; RC13-188; RC13-189; RC13-190TW; RC13-210; RC24; RC24-1; RC24-11; RC24-13; RC24-15TW; RC24-16TW; RC24-17; RC24-19TW; RC24-21TW; RC24-7; Robert Conrad; Sample ID; V14; V14-5; V16; V16-203; V16-21; V16-22; V16-35; V16-37; V20; V20-230; V20-233; V20-234; V22; V22-174; V22-175; V22-179; V22-182; V22-202; V22-30; V22-31; V22-32; V25; V25-44; V25-50; V25-59; V25-60; V26; V26-100; V26-102; V26-99; V27; V27-181; V27-267; V30; V30-40; V30-41; V32; V32-67; Vema
    Type: Dataset
    Format: text/tab-separated-values, 331 data points
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  • 14
    Publication Date: 2024-02-29
    Keywords: Atlantic; Atlantic Ocean; BC; Box corer; DEPTH, sediment/rock; Elevation of event; Event label; Globorotalia truncatulinoides dextral, δ13C; Globorotalia truncatulinoides dextral, δ18O; INMD; INMD-111BX; INMD-113BX; INMD-115BX; Latitude of event; Longitude of event; Mass spectrometer Fisons Optima; Melville; PC; Piston corer; RC08; RC08-18; RC08-19; RC08-23; RC11; RC1112; RC11-17; RC13; RC13-188; RC13-189; RC13-190; RC13-210; RC16; RC16-77; RC24; RC24-1; RC24-11; RC24-13; RC24-15; RC24-16; RC24-17; RC24-19; RC24-21; RC24-7; Robert Conrad; Sample ID; V10; V10-93; V14; V14-2; V14-5; V16; V16-203; V16-205; V16-206; V16-21; V16-22; V16-35; V16-37; V17; V17-165; V19; V19-308; V20; V20-233; V20-234; V20-244; V22; V22-169; V22-174; V22-175; V22-179; V22-182; V22-202; V22-30; V22-31; V22-32; V25; V25-44; V25-50; V25-59; V25-60; V26; V26-100; V26-102; V26-99; V27; V27-161; V27-181; V27-263; V27-267; V29; V29-178; V30; V30-40; V30-41; V30-96; V30-97; V32; V32-67; Vema
    Type: Dataset
    Format: text/tab-separated-values, 342 data points
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  • 15
    Publication Date: 2024-01-25
    Keywords: 325-M0031A; 325-M0033A; 325-M0035A; 325-M0036A; 325-M0039A; 325-M0053A; 325-M0057A; Age, dated; Age, dated standard deviation; Aragonite; Comment; DIVER; DRILL; Drilling/drill rig; Event label; Exp325; GBR-1023; GBR-1024; GBR-1108; GBR-206; GBR-219; GBR-307; GBR-318; GBR-537; GBR-947; GBR-954; Great Barrier Reef, Australia; Great Barrier Reef Environmental Changes; Greatship Maya; HYD_01CSite11; HYD_01Csite6; HYD_01CSite6; HYD_01CSite8; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Magnesium/Calcium ratio; NOG_01BSite2; NOG_01BSite6; Number; Papua New Guinea; PNG-21A; PNG-36; PNG-89B; Sample code/label; Sample comment; Sampling by diver; Site; Standard deviation; Strontium/Calcium ratio; δ13C, skeletal carbonate; δ18O, skeletal carbonate
    Type: Dataset
    Format: text/tab-separated-values, 739 data points
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  • 16
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    PANGAEA
    In:  Supplement to: Wu, Henry C; Linsley, Braddock K; Dassié, Emilie Pauline; Schiraldi, Benedetto; deMenocal, Peter B (2013): Oceanographic variability in the South Pacific Convergence Zone region over the last 210 years from multi-site coral Sr/Ca records. Geochemistry, Geophysics, Geosystems, 14(5), 1435-1453, https://doi.org/10.1029/2012GC004293
    Publication Date: 2024-02-21
    Description: In the South Pacific Convergence Zone (SPCZ), the variability in a sub-seasonally resolved microatoll Porites colony Sr/Ca record from Tonga and a previously published high-resolution record from Fiji are strongly influenced by sea surface temperature (SST) over the calibration period from 1981 to 2004 (R^2 = 0.67 - 0.68). However, the Sr/Ca-derived SST correlation to instrumental SST decreases back in time. The lower frequency secular trend (~1°C) and decadal-scale (~2 - 3°C) modes in Sr/Ca-derived SST are almost two times larger than that observed in instrumental SST. The coral Sr/Ca records suggest that local effects on SST generate larger amplitude variability than gridded SST products indicate. Reconstructed d18O of seawater (d18Osw) at these sites correlate with instrumental sea surface salinity (SSS; r = 0.64 - 0.67) but not local precipitation (r = -0.10 to - 0.22) demonstrating that the advection and mixing of different salinity water masses may be the predominant control on d18Osw in this region. The Sr/Ca records indicate SST warming over the last 100 years and appears to be related to the expansion of the western Pacific warm pool (WPWP) including an increasing rate of expansion in the last ~20 years. The reconstructed d18Osw over the last 100 years also shows surface water freshening across the SPCZ. The warming and freshening of the surface ocean in our study area suggests that the SPCZ has been shifting (expanding) southeast, possibly related to the southward shift and intensification of the South Pacific gyre over the last 50 years in response to strengthened westerly winds.
    Keywords: Age; AGE; Center for Marine Environmental Sciences; DHC; Diver-held corer; Ha afera Island, Tonga; MARUM; Strontium/Calcium ratio; Tonga_TH1
    Type: Dataset
    Format: text/tab-separated-values, 426 data points
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  • 17
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    Unknown
    PANGAEA
    In:  Supplement to: Felis, Thomas; McGregor, Helen V; Linsley, Braddock K; Tudhope, Alexander W; Gagan, Michael K; Suzuki, Atsushi; Inoue, Mayuri; Thomas, Alexander L; Esat, Tezer M; Thompson, William G; Tiwari, Manish; Potts, Donald C; Mudelsee, Manfred; Yokoyama, Yusuke; Webster, Jody M (2014): Intensification of the meridional temperature gradient in the Great Barrier Reef following the Last Glacial Maximum. Nature Communications, 5, 4102, https://doi.org/10.1038/ncomms5102
    Publication Date: 2024-04-20
    Description: Tropical south-western Pacific temperatures are of vital importance to the Great Barrier Reef (GBR), but the role of sea surface temperatures (SSTs) in the growth of the GBR since the Last Glacial Maximum remains largely unknown. Here we present records of Sr/Ca and d18O for Last Glacial Maximum and deglacial corals that show a considerably steeper meridional SST gradient than the present day in the central GBR. We find a 1-2 °C larger temperature decrease between 17° and 20°S about 20,000 to 13,000 years ago. The result is best explained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacific gyre and East Australian Current. Our findings indicate that the GBR experienced substantial meridional temperature change during the last deglaciation, and serve to explain anomalous deglacial drying of northeastern Australia. Overall, the GBR developed through significant SST change and may be more resilient than previously thought.
    Keywords: Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 18
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Earth and Planetary Science Letters 387 (2014): 240–251, doi:10.1016/j.epsl.2013.11.032.
    Description: Evidence from geologic archives suggests that there were large changes in the tropical hydrologic cycle associated with the two prominent northern hemisphere deglacial cooling events, Heinrich Stadial 1 (HS1; ∼19 to 15 kyr BP; kyr BP = 1000 yr before present) and the Younger Dryas (∼12.9 to 11.7 kyr BP). These hydrologic shifts have been alternatively attributed to high and low latitude origin. Here, we present a new record of hydrologic variability based on planktic foraminifera-derived δ18O of seawater (δ18Osw) estimates from a sediment core from the tropical Eastern Indian Ocean, and using 12 additional δ18Osw records, construct a single record of the dominant mode of tropical Eastern Equatorial Pacific and Indo-Pacific Warm Pool (IPWP) hydrologic variability. We show that deglacial hydrologic shifts parallel variations in the reconstructed interhemispheric temperature gradient, suggesting a strong response to variations in the Atlantic Meridional Overturning Circulation and the attendant heat redistribution. A transient model simulation of the last deglaciation suggests that hydrologic changes, including a southward shift in the Intertropical Convergence Zone (ITCZ) which likely occurred during these northern hemisphere cold events, coupled with oceanic advection and mixing, resulted in increased salinity in the Indonesian region of the IPWP and the eastern tropical Pacific, which is recorded by the δ18Osw proxy. Based on our observations and modeling results we suggest the interhemispheric temperature gradient directly controls the tropical hydrologic cycle on these time scales, which in turn mediates poleward atmospheric heat transport.
    Description: ThisworkwasfundedbytheNationalScienceFoundation;theOceanandClimateChangeInstituteandtheAcademicProgramsOfficeatWoodsHoleOceano-graphicInstitution;BMBF(PABESIA);andDFG(He3412/15-1)
    Keywords: Indo-Pacific ; Eastern Equatorial Pacific ; δ18O of seawater ; Deglaciation ; Heat transport
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Format: application/msword
    Format: text/plain
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