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  • 1
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    PANGAEA
    In:  Supplement to: Winckler, Gisela; Anderson, Robert F; Schlosser, Peter (2005): Equatorial Pacific productivity and dust flux during the mid-Pleistocene climate transition. Paleoceanography, 20(4), PA4025, https://doi.org/10.1029/2005PA001177
    Publication Date: 2023-09-15
    Description: We present a helium isotope record for core TT013-114PC from the central equatorial Pacific (140°W, 4°N, 4432 m water depth) spanning a period of 1 million years. We focus on the time interval from 560 to 800 kyr, largely coinciding with the mid-Pleistocene climate transition (MPT) when the dominant period of the Earth's climate variability shifted from 41 kyr to 100 kyr. The terrigenous 4He concentrations from our study correlate very well with published titanium concentrations in this core strongly supporting the use of terrigenous 4He as a monitor of continental dust. Normalizing titanium and terrigenous 4He concentrations to 3He suggests that the dust supply during the MPT was approximately 30% lower compared to the subsequent period (560-100 kyr). The 3He-normalized barium, aluminum and phosphorus concentrations, trace elements with a predominantly biogenic source in these sediments, are relatively constant. This is in contrast to previous studies that reported an apparent rise of titanium-normalized productivity proxies. Rather than a significant increase in productivity during the MPT, we conclude that the dust flux to the central equatorial Pacific was reduced and that the export productivity was approximately constant during this period of climate reorganization.
    Keywords: 11291231 Pistoncore13; AGE; Comment; DEPTH, sediment/rock; Equatorial Pacific; Helium-3; Helium-3, standard deviation; Helium-3/Helium-4; Helium-3/Helium-4, standard deviation; Helium-4, terrestrial; Helium-4, terrestrial, standard deviation; Isotope ratio mass spectrometry; Normalized; PC; Piston corer; Thomas G. Thompson; TT013; TT013_114
    Type: Dataset
    Format: text/tab-separated-values, 225 data points
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Marcantonio, Franco; Anderson, Robert F; Higgins, Sean M; Stute, Martin; Schlosser, Peter; Kubik, Peter W (2001): Sediment focusing in the central equatorial Pacific Ocean. Paleoceanography, 16(3), 260-267, https://doi.org/10.1029/2000PA000540
    Publication Date: 2023-09-23
    Description: At four sites in the central equatorial Pacific Ocean the flux of extraterrestrial 3He, determined using the excess 230Th profiling method, is 8 * 10**-13 cm**3 STP/cm**2/ka. This supply rate is constant to within 30%. At these same sites, however, the burial rate of 3He, determined using chronostratigraphic accumulation rates, varies by more than a factor of 3. The lowest burial rates, which occur north of the equator at 1°N, 139°W are lower than the global average rate of supply of extraterrestrial 3He by 20% and indicate that sediment winnowing may have occurred. The highest burial rates, which are recorded at the equator and at 2°S, are higher than the rate of supply of extraterrestrial 3He by 100%, and these provide evidence for sediment focusing. By analyzing several proxies measured in core PC72 sediments spanning the past 450 kyr we demonstrate that periods of maximum burial rates of 230Th, 3He, 10Be, Ti, and barite, with a maximum peak-to-trough amplitude of a factor of 6, take place systematically during glacial time. However, the ratio of any one proxy to another is constant to within 30% over the entire length of the records. Given that each proxy represents a different source (234U decay in seawater, interplanetary dust, upper atmosphere, continental dust, or upper ocean), our preferred interpretation for the covariation is that the climate-related changes in burial rates are driven by changes in sediment focusing.
    Keywords: AGE; DEPTH, sediment/rock; Event label; GC; Gravity corer; Helium-3, flux; Helium-3/Helium-4; MANOP; MANOP_B18; MANOP_B25; Thorium-230 excess
    Type: Dataset
    Format: text/tab-separated-values, 173 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-09-23
    Keywords: AGE; Calculated; DEPTH, sediment/rock; ICP-MS, VG-Plasma-Quad 2; PC; Piston corer; RC17; RC17-177; Robert Conrad; Thorium-230; Thorium-230, standard deviation; Thorium-230 excess; Thorium-230 excess, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 184 data points
    Location Call Number Limitation Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Winckler, Gisela; Anderson, Robert F; Stute, Martin; Schlosser, Peter (2004): Does interplanetary dust control 100 kyr glacial cycles? Quaternary Science Reviews, 23(18-19), 1873-1878, https://doi.org/10.1016/j.quascirev.2004.05.007
    Publication Date: 2024-01-09
    Description: The cause of the 100 kyr glacial–interglacial cycles during the past 800 kyr is one of the fundamental puzzles in paleoclimatology. The widely accepted Milankovitch theory, relating earth's climate cycles to variations in insolation caused by periodic changes in orbital parameters, has difficulties to explain the predominant 100 kyr rhythm. Although earth's eccentricity varies with a period of 100 kyr, the resulting change in insolation is too small to produce the corresponding climate cycle by direct forcing (Imbrie et al., 1993; doi:10.1029/93PA02751. In order to solve the '100 kyr problem', Muller and MacDonald (1995, doi:10.1038/377107b0; 1997, doi:10.1126/science.277.5323.215; Proc. Nat. Acad. Sci. USA 94 (1997b) 8329) proposed an alternative orbital but non-Milankovitch mechanism attributing the glacial cycles to regular variations in the accretion of interplanetary dust particles (IDP) caused by 100 kyr cycles in the orbital inclination of the earth. To test this controversial hypothesis, we study the IDP accumulation in deep-sea sediments from a period in the early Pleistocene. We find apparent 41 kyr cycles but no 100 kyr periodicity in the IDP accumulation rate. As there is no known mechanism to produce 41 kyr cycles in IDP supply from space, we conclude that the 41 kyr cycles are caused by the dynamics of sediment accumulation, and that changes in the IDP flux do not drive the Pleistocene glacial cycles.
    Keywords: 138-849; Accumulation rate, mass; AGE; Calcium carbonate; Calculated; Comment; COMPCORE; Composite Core; Coulometry; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Helium-3; Helium-3, standard deviation; Helium-3/Helium-4; Helium-3/Helium-4, standard deviation; Joides Resolution; Leg138; Mass spectrometer MAP215-50; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 333 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-01-09
    Keywords: 130-806B; AGE; Calculated; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; ICP-MS, VG-Plasma-Quad 2; Joides Resolution; Leg130; North Pacific Ocean; Ocean Drilling Program; ODP; Sample comment; Thorium-230; Thorium-230, standard deviation; Thorium-230 excess; Thorium-230 excess, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 110 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-01-09
    Keywords: 130-806C; AGE; Calculated; DEPTH, sediment/rock; DRILL; Drilling/drill rig; ICP-MS, VG-Plasma-Quad 2; Joides Resolution; Leg130; North Pacific Ocean; Ocean Drilling Program; ODP; Thorium-230; Thorium-230, standard deviation; Thorium-230 excess; Thorium-230 excess, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 232 data points
    Location Call Number Limitation Availability
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Higgins, Sean M; Anderson, Robert F; Marcantonio, Franco; Schlosser, Peter; Stute, Martin (2002): Sediment focusing creates 100-ka cycles in interplanetary dust accumulation on the Ontong Java Platea. Earth and Planetary Science Letters, 203(1), 383-397, https://doi.org/10.1016/S0012-821X(02)00864-6
    Publication Date: 2024-01-09
    Description: The accumulation of extraterrestrial 3He, a tracer for interplanetary dust particles (IDPs), in sediments from the Ontong Java Plateau (OJP; western equatorial Pacific Ocean) has been shown previously to exhibit a regular cyclicity during the late Pleistocene, with a period of ~100 ka. Those results have been interpreted to reflect periodic variability in the global accretion of IDPs that, in turn, has been linked to changes in the inclination of Earth's orbit with respect to the invariable plane of the solar system. Here we show that the accumulation in OJP sediments of authigenic 230Th, produced by radioactive decay of 234U in seawater, exhibits a 100-ka cyclicity similar in phase and amplitude to that evident in the 3He record. We interpret the similar patterns of 230Th and 3He accumulation to reflect a common origin within the ocean-climate system. Comparing spatial and temporal patterns of sediment accumulation against regional patterns of biological productivity and against the well-established pattern of CaCO3 dissolution in the deep Pacific Ocean leads to the further conclusion that a common 100-ka cycle in accumulation of biogenic, authigenic and extraterrestrial constituents in OJP sediments reflects the influence of climate-related changes in sediment focusing, rather than changes in the rate of production or supply of sedimentary constituents.
    Keywords: 130-806B; 130-806C; DRILL; Drilling/drill rig; Joides Resolution; Leg130; North Pacific Ocean; Ocean Drilling Program; ODP; PC; Piston corer; RC17; RC17-177; Robert Conrad
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-04-20
    Description: This data set includes noble gas measurements and modeled recharge temperatures from 32 separate groundwater studies, each analyzed using the same consistent framework and set of noble gas temperature models (CE, PR, and OD models). Along with noble gas data and modeled temperatures are site information (coordinates, recharge elevation), groundwater age data, modern recharge temperatures, other model outputs (excess air, fractionation), and uncertainties for all variables of interest. These data were used to estimate LGM-Late Holocene temperature differences from each site and, together, for the large-scale low-latitude, low-elevation land surface.
    Keywords: Arizona_LGM; Brazil_LGM; Bunter-Sandstone-Aquifer_LGM; Dakota_LGM; France_LGM; Georgia_LGM; Great-Hungarian-Plain_LGM; Kalahari_LGM; Minqin-Basin_LGM; Mojave-Desert_LGM; MULT; Multiple investigations; New-Zealand_LGM; North-China-Plain_LGM; Pannonian-Basin_LGM; Sahel_LGM; San-Diego_LGM; San-Juan-Basin_LGM; Switzerland_LGM
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 766.1 kBytes
    Location Call Number Limitation Availability
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