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  • 1
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 434 (2005), S. 1118-1121 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Massive iceberg discharges from the Northern Hemisphere ice sheets, ‘Heinrich events’, coincided with the coldest periods of the last ice age. There is widespread evidence for Heinrich events and their profound impact on the climate and circulation of the North Atlantic Ocean, ...
    Type of Medium: Electronic Resource
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  • 2
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    PANGAEA
    In:  Supplement to: Atwood, Alyssa R; Sachs, Julian P (2014): Separating ITCZ- and ENSO-related rainfall changes in the Galápagos over the last 3 kyr using D/H ratios of multiple lipid biomarkers. Earth and Planetary Science Letters, 404, 408-419, https://doi.org/10.1016/j.epsl.2014.07.038
    Publication Date: 2023-01-13
    Description: We present a 3000-yr rainfall reconstruction from the Galápagos Islands that is based on paired biomarker records from the sediment of El Junco Lake. Located in the eastern equatorial Pacific, the climate of the Galápagos Islands is governed by movements of the Intertropical Convergence Zone (ITCZ) and the El Niño-Southern Oscillation (ENSO). We use a novel method for reconstructing past ENSO- and ITCZ-related rainfall changes through analysis of molecular and isotopic biomarker records representing several types of plants and algae that grow under differing climatic conditions. We propose that dD values of dinosterol, a sterol produced by dinoflagellates, record changes in mean rainfall in El Junco Lake, while dD values of C34 botryococcene, a hydrocarbon unique to the green alga Botryococcus braunii, record changes in rainfall associated with moderate-to-strong El Niño events. We use these proxies to infer changes in mean rainfall and El Niño-related rainfall over the past 3000 yr. During periods in which the inferred change in El Niño-related rainfall opposed the change in mean rainfall, we infer changes in the amount of ITCZ-related rainfall. Simulations with an idealized isotope hydrology model of El Junco Lake help illustrate the interpretation of these proxy reconstructions. Opposing changes in El Niño- and ITCZ-related rainfall appear to account for several of the largest inferred hydrologic changes in El Junco Lake. We propose that these reconstructions can be used to infer changes in frequency and/or intensity of El Niño events and changes in the position of the ITCZ in the eastern equatorial Pacific over the past 3000 yr. Comparison with El Junco Lake sediment grain size records indicates general agreement of inferred rainfall changes over the late Holocene.
    Keywords: COMPCORE; Composite Core; EJ7-MW1_EJ-N-1; Pacific Ocean
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 3
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    PANGAEA
    In:  Supplement to: Leduc, Guillaume; Sachs, Julian P; Kawka, Orest E; Schneider, Ralph R (2013): Holocene changes in eastern equatorial Atlantic salinity as estimated by water isotopologues. Earth and Planetary Science Letters, 362, 151-162, https://doi.org/10.1016/j.epsl.2012.12.003
    Publication Date: 2023-01-13
    Description: The isotopic composition of surface seawater is widely used to infer past changes in sea surface salinity using paired foraminiferal Mg/Ca and d18O from marine sediments. At low latitudes, paleosalinity reconstructions using this method have largely been used to document changes in the hydrological cycle. This method usually assumes that the modern seawater d18O (d18Osw)/salinity relationship remained constant through time. Modelling studies have shown that such assumptions may not be valid because large-scale atmospheric circulation patterns linked to global climate changes can alter the seawater d18Osw/salinity relationship locally. Such processes have not been evidenced by paleo-data so far because there is presently no way to reconstruct past changes in the seawater d18Osw/salinity relationship. We have addressed this issue by applying a multi-proxy salinity reconstruction from a marine sediment core collected in the Gulf of Guinea. We measured hydrogen isotopes in C37:2 alkenones (dDa) to estimate changes in seawater dD. We find a smooth, long-term increase of ~10 per mil in dDa between 10 and 3 kyr BP, followed by a rapid decrease of ~10 per mil in dDa between 3 kyr BP and core top to values slightly lighter than during the early Holocene. Those features are inconsistent with published salinity estimations based on d18Osw and foraminiferal Ba/Ca, as well as nearby continental rainfall history derived from pollen analysis. We combined dDa and d18Osw values to reconstruct a Holocene record of salinity and compared it to a Ba/Ca-derived salinity record from the same sedimentary sequence. This combined method provides salinity trends that are in better agreement with both the Ba/Ca-derived salinity and the regional precipitation changes as inferred from pollen records. Our results illustrate that changes in atmospheric circulation can trigger changes in precipitation isotopes in a counter-intuitive manner that ultimately impacts surface salinity estimates based on seawater isotopic values. Our data suggest that the trends in Holocene rainfall isotopic values at low latitudes may not uniquely result from changes in local precipitation associated with the amount effect.
    Keywords: AGE; Alkenone C37:2, δD; Gas chromatography - Isotope ratio mass spectrometer (GC-IRMS); MD03-2707; PC; Piston corer; Salinity, standard error; Sea surface salinity; SSS calculated from d18O and d2H (Rohling, 2007); δ Deuterium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 112 data points
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  • 4
    Publication Date: 2023-02-07
    Keywords: AGE; Age, error; COMPCORE; Composite Core; Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EJ7-MW1_EJ-N-1; Error; Index; Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 575 data points
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  • 5
    Publication Date: 2023-02-07
    Keywords: AGE; COMPCORE; Composite Core; Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EJ7-MW1_EJ-N-1; Index; Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 68 data points
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  • 6
    Publication Date: 2023-02-08
    Keywords: AGE; Age, error; Biomarker; COMPCORE; Composite Core; Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EJ7-MW1_EJ-N-1; Logarithm; Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 418 data points
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  • 7
    Publication Date: 2023-02-08
    Keywords: AGE; Age, error; COMPCORE; Composite Core; Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EJ7-MW1_EJ-N-1; Pacific Ocean; δ Deuterium; δ Deuterium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 478 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Anderson, Robert F; Barker, Stephen; Fleisher, Martin Q; Gersonde, Rainer; Goldstein, Steven L; Kuhn, Gerhard; Mortyn, P Graham; Pahnke, Katharina; Sachs, Julian P (2014): Biological response to millennial variability of dust and nutrient supply in the Subantarctic South Atlantic Ocean. Philosophical Transactions of the Royal Society A-Mathematical Physical and Engineering Sciences, 372(2019), 20130054, https://doi.org/10.1098/rsta.2013.0054
    Publication Date: 2023-03-16
    Description: Fluxes of lithogenicmaterial and fluxes of three palaeo productivity proxies (organic carbon, biogenic opal and alkenones) over the past 100,000 years were determined using the 230Th-normalization method in three sediment cores from the Subantarctic South Atlantic Ocean. Features in the lithogenic flux record of each core correspond to similar features in the record of dust deposition in the EPICA Dome C ice core. Biogenic fluxes correlate with lithogenic fluxes in each sediment core. Our preferred interpretation is that South American dust, most probably from Patagonia, constitutes a major source of lithogenic material in Subantarctic South Atlantic sediments, and that past biological productivity in this region responded to variability in the supply of dust, probably due to biologically available iron carried by the dust. Greater nutrient supply as well as greater nutrient utilization (stimulated by dust) contributed to Subantarctic productivity during cold periods, in contrast to the region south of the Antarctic Polar Front (APF), where reduced nutrient supply during cold periods was the principal factor limiting productivity. The anti-phased patterns of productivity on opposite sides of the APF point to shifts in the physical supply of nutrients and to dust as cofactors regulating productivity in the Southern Ocean.
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
    Publication Date: 2023-06-21
    Keywords: 14-methyl pentadecanol; 4alpha,23,24-Trimethyl-5alpha-cholest-22E-en-3beta-ol; Archaeol; Center for Marine Environmental Sciences; Cholestanol; Cholesterol; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diplopterol; Docosanol; Docosenol; Dotricontanol; Eicosanol; Eicosenol; Ergosta-7,22-dien-3b-ol; Ergostanol; Ergosterol; Farnesol; Gas chromatography; HAND; Heneicosanol; Heptacosanol; Heptadecadienol; Heptadecanol; Heptadecenol; Hexacosanol; Hexadecanol; Hopanoid, unknown; Hydroxycholesterol; Kiritimati Island; Kiritimati-Island_Lake-2A; MARUM; Nonacosanol; Nonadecadienol; Nonadecanol; Nondecenol; Octadecanol; Octadecenol; Octasanol; Pentacosanol; Pentadecanol; Sample code/label; Sampling by hand; Sito-dien-sterol; Sitostanol; Sitosterol; Sum; Tetracosanol; Tricontanol; Tricosanol
    Type: Dataset
    Format: text/tab-separated-values, 192 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Keigwin, Lloyd D; Sachs, Julian P; Rosenthal, Yair; Boyle, Edward A (2005): The 8200 year B.P. event in the slope water system, western subpolar North Atlantic. Paleoceanography, 20(2), PA2003, https://doi.org/10.1029/2004PA001074
    Publication Date: 2023-05-12
    Description: Stable isotope, trace metal, alkenone paleothermometry, and radiocarbon methods have been applied to sediment cores in the western subpolar North Atlantic between Hudson Strait and Cape Hatteras to reveal the history of climate in that region over the past ~11 kyr. We focus on cores from the Laurentian Fan, which is known to have rapid and continuous accumulation of hemipelagic sediment. Although results among our various proxy data are not always in agreement, the weight of the evidence (alkenone sea surface temperature (SST), d18O and abundance of Globigerinoides ruber) indicates a continual cooling of surface waters over Laurentian Fan, from about 18°C in the early Holocene to about 8°C today. Alternatively, Mg/Ca data on planktonic foraminifera indicate no systematic change in Holocene SST. The inferred long-term decrease in SST was probably driven by decreasing seasonality of Northern Hemisphere insolation. Two series of proxy data show the gradual cooling was interrupted by a two-step cold pulse that began 8500 years ago, and lasted about 700 years. Although this event is associated with the final deglaciation of Hudson Bay, there is no d18O minimum anywhere in the Labrador Sea, yet there is some evidence for it as far south as Cape Hatteras. Finally, although the 8200 year B.P. event has been implicated in decreasing North Atlantic ventilation, and hence widespread temperature depression on land and at sea, we find inconsistent evidence for a change at that time in deep ocean nutrient content at ~4 km water depth.
    Keywords: Age, 14C AMS; Age, dated; Age, dated material; Age, dated standard error; Age, maximum/old; Age, minimum/young; Calendar age; CH07-98-GGC19; DEPTH, sediment/rock; Elevation of event; Event label; GGC; Giant gravity corer; HU96-29-69; Laboratory code/label; Latitude of event; Longitude of event; MUC; MultiCorer; North Atlantic; OCE326-GGC14; OCE326-GGC26; OCE326-MC13; OCE326-MC25; PC; Piston corer; TC; Trigger corer
    Type: Dataset
    Format: text/tab-separated-values, 298 data points
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