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  • Articles  (1)
  • Data  (15)
  • 1995-1999  (16)
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  • 1
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Evidence for abrupt climate changes on millennial and shorter timescales is widespread in marine and terrestrial climate records. Rapid reorganization of ocean circulation is considered to exert some control over these changes, as are shifts in the concentrations of atmospheric greenhouse ...
    Type of Medium: Electronic Resource
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  • 2
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    In:  Supplement to: Diester-Haass, Lieselotte; Zahn, Rainer (1996): Eocene-Oligocene transition in the Southern Ocean: History of water mass circulation and biological productivity. Geology, 24(2), 163-166, https://doi.org/10.1130/0091-7613(1996)024%3C0163:EOTITS%3E2.3.CO;2
    Publication Date: 2024-01-09
    Description: High-resolution records of carbon and oxygen isotopes and benthic foraminiferal accumulation rates for the Eocene-Oligocene section at Ocean Drilling Program Site 689 (Maud Rise, Weddell Sea; paleodepth about 1500 m) were used to infer variations in paleoproductivity in relation to changes in climate and ventilation of the deeper-water column. The benthic foraminiferal abundance and isotope records show short-term fluctuations at periodicities of 100 and 400 ka, implying orbitally driven climatic variations. Both records suggest that intermediate-depth water chemistry and primary productivity changed in response to climate. During the Eocene, productivity increased during cold periods and during cold-to-warm transitions, possibly as a result of increased upwelling of nutrient-rich waters. In the Oligocene, in contrast, productivity maxima occurred during intervals of low delta18O values (presumably warmer periods), when a proto–polar front moved to the south of the location of Site 689. This profound transition in climate-productivity patterns occurred around 37 Ma, coeval with rapid changes toward increasing variability of the oxygen and carbon isotope and benthic abundance records and toward larger-amplitude delta18O fluctuations. Therefore, we infer that, at this time, temperature fluctuations increased and a proto–polar front formed in conjunction with the first distinct pulsations in size of the Antarctic ice sheet. We speculate that this major change might have resulted from an initial opening of the Drake Passage at 37 Ma, at least for surface- and intermediate-water circulation.
    Keywords: 113-689; Accumulation rate, mass; Calculated; Calculated (Herguera and Berger, 1991); COMPCORE; Composite Core; Counting 〉150 µm fraction; DEPTH, sediment/rock; Foraminifera, benthic; Foraminifera, benthic, flux; Joides Resolution; Leg113; Ocean Drilling Program; ODP; Paleoproductivity as carbon; South Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 1748 data points
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  • 3
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    In:  Supplement to: Zahn, Rainer; Schönfeld, Joachim; Kudrass, Hermann-Rudolph; Park, M-H; Erlenkeuser, Helmut; Grootes, Pieter Meiert (1997): Thermohaline instability in the North Atlantic during meltwater events: Stable isotope and ice-rafted detritus records from core SO75-26KL, Portuguese margin. Paleoceanography, 12(5), 696-710, https://doi.org/10.1029/97PA00581
    Publication Date: 2024-06-26
    Description: A benthic isotope record has been measured for core SO75-26KL from the upper Portuguese margin (1099 m water depth) to monitor the response of thermohaline overturn in the North Atlantic during Heinrich events. Evaluating benthic delta18O in TS diagrams in conjunction with equilibrium deltac fractionation implies that advection of Mediterranean outflow water (MOW) to the upper Portuguese margin was significantly reduced during the last glacial (〈 15% compared to 30% today). The benthic isotope record along core SO75-26KL therefore primarily monitors variability of glacial North Atlantic conveyor circulation. The 14C-accelerator mass spectrometry ages of 13.54±.07 and 20.46±.12 ka for two ice-rafted detritus (IRD) layers in the upper core section and an interpolated age of 36.1 ka for a third IRD layer deeper in the core are in the range of published 14C ages for Heinrich events H1, H2, and H4. Marked depletion of benthic delta13C by 0.7-1.1 per mil during the Heinrich events suggests reduced thermohaline overturn in the North Atlantic during these events. Close similarity between meltwater patterns (inferred from planktonic delta18O) at Site 609 and ventilation patterns (inferred from benthic delta13C) in core SO75-26KL implies coupling between thermohaline overturn and surface forcing, as is also suggested by ocean circulation models. Benthic delta13C starts to decrease 1.5-2.5 kyr before Heinrich events Hl and H4, fully increased values are reached 1.5-3 kyr after the events, indicating a successive slowdown of thermohaline circulation well before the events and resumption of the conveyor's full strength well after the events. Benthic delta13C changes in the course of the Heinrich events show subtle maxima and minima suggesting oscillatory behavior of thermohaline circulation, a distinct feature of thermohaline instability in numerical models. Inferrred gradual spin-up of thermohaline circulation after Hl and H4 is in contrast to abrupt wanning in the North Atlantic region that is indicated by sudden increases in Greenland ice core delta18O and in marine faunal records from the northern North Atlantic. From this we infer that thermohaline circulation can explain only in part the rapid climatic oscillations seen in glacial sections of the Greenland ice core record.
    Keywords: KL; off Portugal; Piston corer (BGR type); SO75/3; SO75/3_26KL; Sonne
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
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    In:  Supplement to: Rühlemann, Carsten; Mulitza, Stefan; Müller, Peter J; Wefer, Gerold; Zahn, Rainer (1999): Warming of the tropical Atlantic Ocean and slowdown of thermohaline circulation during the last deglaciation. Nature, 402(6761), 511-514, https://doi.org/10.1038/990069
    Publication Date: 2024-06-26
    Description: Evidence for abrupt climate changes on millennial and shorter timescales is widespread in marine and terrestrial climate records (Dansgard et al., 1993, doi:10.1038/364218a0; Bond et al., 1993, doi:10.1038/365143a0; Charles et al., 1996, doi:10.1016/0012-821X(96)00083-0, Bard et al., 1997, doi:10.1038/385707a0). Rapid reorganization of ocean circulation is considered to exert some control over these changes (Broecker et al., 1985, doi:10.1038/315021a0), as are shifts in the concentrations of atmospheric greenhouse gases (Broecker, 1994, doi:10.1038/372421a0). The response of the climate system to these two influences is fundamentally different: slowing of thermohaline overturn in the North Atlantic Ocean is expected to decrease northward heat transport by the ocean and to induce warming of the tropical Atlantic (Crowley, 1992, doi:10.1029/92PA01058; Manabe and Stouffer, 1997, doi:10.1029/96PA03932), whereas atmospheric greenhouse forcing should cause roughly synchronous global temperature changes (Manabe et al., 1991, doi:10.1175/1520-0442(1991)004〈0785:TROACO〉2.0.CO;2). So these two mechanisms of climate change should be distinguishable by the timing of surface-water temperature variations relative to changes in deep-water circulation. Here we present a high-temporal-resolution record of sea surface temperatures from the western tropical North Atlantic Ocean which spans the past 29,000 years, derived from measurements of temperature-sensitive alkenone unsaturation in sedimentary organic matter. We find significant warming is documented for Heinrich event H1 (16,900-15,400 calendar years bp) and the Younger Dryas event (12,900-11,600 cal. yr bp), which were periods of intense cooling in the northern North Atlantic. Temperature changes in the tropical and high-latitude North Atlantic are out of phase, suggesting that the thermohaline circulation was the important trigger for these rapid climate changes.
    Keywords: Gravity corer (Kiel type); M35/1; M35003-4; Meteor (1986); SL
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 5
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    In:  Supplement to: Thomson, John; Nixon, S; Summerhayes, Colin P; Schönfeld, Joachim; Zahn, Rainer; Grootes, Pieter Meiert (1999): Implications for sedimentation changes on the Iberian margin over the last two glacial/interglacial transitions from (230Th-excess)0 systematics. Earth and Planetary Science Letters, 165(3-4), 255-270, https://doi.org/10.1016/S0012-821X(98)00265-9
    Publication Date: 2024-06-26
    Description: The Portuguese margin is well-suited for studies of the contrasts in North Atlantic circulation during glacial and interglacial times because of its rapid sediment accumulation rate. This paper reports a (230Thexcess)0-based study of sediment accumulation over the past 140 ky, a period which includes the last two glacial/interglacial transitions, in two cores at 2.4 and 3.5 km water depth on a slope transect at 40°N. Although the independently-determined mean sediment accumulation fluxes over the past 140 ky are unequivocally high with means of 13.2 and 10.5 g cm**-2 ky**-1 in the two cores, conventional application of the (230Thexcess)0 method yields consistently lower fluxes with means of 3.5 and 3.8 g cm**-2 ky**-1. These (230Thexcess)0 estimates are interpreted as representations of the regional depositional flux through time. This (230Thexcess)0 regional flux is composed of a carbonate flux of 〈1 g cm**-2 ky**-1and a larger and variable clay input which indicates the importance of the sea level control on the clay input to the basin. Clay flux dominates the regional sediment accumulation which has a total flux of ~2 g cm**-2 ky**-1and a CaCO3 content up to 50% in interglacial times, and a total flux up to ~5 g cm**-2 ky**-1and a CaCO3 content down to 10% in glacial times. This pattern of change of sediment composition through time is also typical of the NE Atlantic, and sediment focusing (contourite formation) appears responsible for the high actual fluxes observed in glacial compared with interglacial times on the Iberian margin. The inventories of (230Thexcess)0 exceed those which could have been supplied from the overlying water column alone over 140 ky by factors of *3.2 and *4.0 in the two cores. This is ascribed to preferential current focusing of fine sedimentary material in glacial times as a result of a systematic change in deep ocean circulation in response to climatic forcing. The presence of Heinrich events in the sediments is clearly evident, but at this southerly latitude they produce muted regional increases in accumulation flux (〈2 g cm**-2 ky**-1), apart from the large Heinrich event 4 which introduced an additional 10-20 g cm cm**-2 ky**-1 over ambient background levels.
    Keywords: CALYPSO; Calypso Corer; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); MD101; MD952039; MD95-2039; MD952040; MD95-2040; Porto Seamount
    Type: Dataset
    Format: application/zip, 8 datasets
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  • 6
    Publication Date: 2024-06-26
    Keywords: CALYPSO; Calypso Corer; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; DEPTH, sediment/rock; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); Mass spectrometer Finnigan MAT 251; MD101; MD952039; MD95-2039; Porto Seamount
    Type: Dataset
    Format: text/tab-separated-values, 504 data points
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  • 7
    Publication Date: 2024-06-26
    Keywords: CALYPSO; Calypso Corer; Carbonates; DEPTH, sediment/rock; Element analysis coulometric; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); MD101; MD952040; MD95-2040; Porto Seamount
    Type: Dataset
    Format: text/tab-separated-values, 211 data points
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  • 8
    Publication Date: 2024-06-26
    Keywords: CALYPSO; Calypso Corer; DEPTH, sediment/rock; Grain size, sieving; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); MD101; MD952039; MD95-2039; Porto Seamount; Sand; Sand, mass netto
    Type: Dataset
    Format: text/tab-separated-values, 738 data points
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  • 9
    Publication Date: 2024-06-26
    Keywords: AGE; Alpha spectrometry, total dissolution; Calculated; CALYPSO; Calypso Corer; DEPTH, sediment/rock; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); MD101; MD952039; MD95-2039; Porto Seamount; Sea level; Sedimentation rate; see reference(s); Thorium-230, supported, uncorrected; Thorium-230, supported, uncorrected standard deviation; Thorium-230/Thorium-232 activity ratio; Thorium-230/Thorium-232 activity ratio, standard deviation; Thorium-232; Thorium-232, standard deviation; Uranium-234; Uranium-234, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; Uranium-238; Uranium-238, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 1583 data points
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  • 10
    Publication Date: 2024-06-26
    Keywords: Calculated from mass/volume; CALYPSO; Calypso Corer; Density, dry bulk; Density, wet bulk; DEPTH, sediment/rock; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); Mass, brutto; Mass, netto; Mass, tara; MD101; MD952039; MD95-2039; Porosity; Porto Seamount; Sample volume; Water content, wet mass, brutto
    Type: Dataset
    Format: text/tab-separated-values, 2952 data points
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