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  • 2020-2024
  • 2010-2014  (6)
  • 1980-1984
  • 2013  (6)
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  • 2020-2024
  • 2010-2014  (6)
  • 1980-1984
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  • 1
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    AGU (American Geophysical Union) | Wiley
    In:  Eos, Transactions American Geophysical Union, 94 (10). p. 100.
    Publication Date: 2016-08-05
    Description: AGU Chapman Conference: The Agulhas System and Its Role in Changing Ocean Circulation, Climate, and Marine Ecosystems; Stellenbosch, South Africa, 8–12 October 2012
    Type: Article , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-03-02
    Keywords: Age, comment; Age, error; Age, maximum/old; Age, minimum/young; Age model; CALYPSO; Calypso Corer; Comment; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Marion Dufresne (1995); MD02-2588; MD02-2588Q; MD128; Southern Ocean; SWAF
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Marino, Gianluca; Zahn, Rainer; Ziegler, Martin; Purcell, Conor; Knorr, Gregor; Hall, Ian R; Ziveri, Patrizia; Elderfield, Henry (2013): Agulhas salt-leakage oscillations during abrupt climate changes of the Late Pleistocene. Paleoceanography, 28(3), 599-606, https://doi.org/10.1002/palo.20038
    Publication Date: 2023-01-13
    Description: An ensemble of new, high-resolution records of surface ocean hydrography from the Indian-Atlantic oceanic gateway, south of Africa, demonstrates recurrent and high-amplitude salinity oscillations in the Agulhas Leakage area during the penultimate glacial-interglacial cycle. A series of millennial-scale salinification events, indicating strengthened salt leakage into the South Atlantic, appear to correlate with abrupt changes in the North Atlantic climate and Atlantic Meridional Overturning Circulation (AMOC). This interhemispheric coupling, which plausibly involved changes in the Hadley Cell and midlatitude westerlies that impacted the interocean transport at the tip of Africa, suggests that the Agulhas Leakage acted as a source of negative buoyancy for the perturbed AMOC, possibly aiding its return to full strength. Our finding points to the Indian-to-Atlantic salt transport as a potentially important modulator of the AMOC during the abrupt climate changes of the Late Pleistocene.
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Rodriguez-Sanz, Laura; Mortyn, P Graham; Herguera, Juan-Carlos; Zahn, Rainer (2013): Hydrographic changes in the tropical and extratropical Pacific during the last deglaciation. Paleoceanography, 28(3), 529-538, https://doi.org/10.1002/palo.20049
    Publication Date: 2023-06-27
    Description: Fine-scale, paired Mg/Ca-d18O profiles (Globigerinoides ruber white, sensu lato) from the San Lázaro Basin (SLB) at 25°N in the Northeast Pacific reveal a transition from a predominant presence of tropical/subtropical waters during the last glacial termination (T1) to an increasing influence of fresh and cold California Current waters toward the Holocene. Changing atmospheric circulation patterns over the Northeast Pacific in step with the demise of the Northern Hemisphere ice sheets and/or with a shift from El Niño- to La Niña-like conditions toward the Holocene are prime candidates to explain this water mass change. d18OSW-IVC increases of ~0.5-0.7 per mil during the Younger Dryas (YD) and Heinrich stadial 1 (HS1) at the SLB are observed in a number of d18OSW-IVC records from the tropical Pacific, more directly influenced by changes in the position of the Intertropical Convergence Zone (ITCZ). Conditioning by ITCZ migration of the tropical Pacific Ocean towards salinity increase during YD and HS1, and the subsequent advection of those water masses as far north as 25°N likely accounted for the reconstructed hydrographical changes at the SLB. A larger influence of tropical water masses as far north as 25°N plausibly contributed to changes in the atmospheric moisture transports to western North America and affected the regional hydrological cycle across T1. Finally, the fine-scale resolution of our d18OSW-IVC record allows pinpointing a shift from relative salty to fresh surface conditions at ~16.2 ka, signaling that the two-phase structure of HS1 is plausibly a ubiquitous feature of the northern tropical to extratropical ocean-atmosphere dynamics.
    Keywords: Age, 14C AMS; Age, 14C calibrated, CALIB 6.0 and Marine09 (Reimer et al., 2009); Age, dated; Age, dated standard deviation; Calendar age; Calendar age, standard deviation; DEPTH, sediment/rock; Giant piston corer; GPC; IMAGES VIII - MONA; Marion Dufresne (1995); MD022505; MD02-2505; MD126; San Lazaro
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2023-06-27
    Keywords: Age, comment; Age, error; Age, maximum/old; Age, minimum/young; Age model; CALYPSO; Calypso Corer; Comment; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; IMAGES II; Marion Dufresne (1995); MD105; MD96-2080; MD962080, ABS; Southern Agulhas Bank
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
    Location Call Number Limitation Availability
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  • 6
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    PANGAEA
    In:  Supplement to: Jonkers, Lukas; van Heuven, Steven; Zahn, Rainer; Peeters, Frank J C (2013): Seasonal patterns of shell flux, d18O and d13C of small and large N. pachyderma (s) and G. bulloides in the subpolar North Atlantic. Paleoceanography, 28(1), 164-174, https://doi.org/10.1002/palo.20018
    Publication Date: 2024-02-17
    Description: Past water column stratification can be assessed through comparison of the d18O of different planktonic foraminiferal species. The underlying assumption is that different species form their shells simultaneously, but at different depths in the water column. We evaluate this assumption using a sediment trap time-series of Neogloboquadrina pachyderma (s) and Globigerina bulloides from the NW North Atlantic. We determined fluxes, d18O and d13C of shells from two size fractions to assess size-related effects on shell chemistry and to better constrain the underlying causes of isotopic differences between foraminifera in deep-sea sediments. Our data indicate that in the subpolar North Atlantic differences in the seasonality of the shell flux, and not in depth habitat or test size, determine the interspecies Delta d18O. N. pachyderma (s) preferentially forms from early spring to late summer, whereas the flux ofG. bulloides peaks later in the season and is sustained until autumn. Likewise, seasonality influences large and small specimens differently, with large shells settling earlier in the season. The similarity of the seasonal d18O patterns between the two species indicates that they calcify in an overlapping depth zone close to the surface. However, their d13C patterns are markedly different (〉1 per mil). Both species have a seasonally variable offset from d13CDIC that appears to be governed primarily by temperature, with larger offsets associated with higher temperatures. The variable offset from d13CDIC implies that seasonality of the flux affects the fossil d13C signal, which has implications for reconstruction of the past oceanic carbon cycle.
    Keywords: Calculated; DATE/TIME; Date/time end; DEPTH, water; Event label; Globigerina bulloides, flux; Globigerina bulloides, δ13C; Globigerina bulloides, δ18O; IRM_1; IRM_3; IRM_4; Mass spectrometer, Finnigan, MAT 253; Neogloboquadrina pachyderma sinistral, flux; Neogloboquadrina pachyderma sinistral, δ13C; Neogloboquadrina pachyderma sinistral, δ18O; North Atlantic; Sample code/label; Trap, sediment; TRAPS; Turborotalita quinqueloba, flux; Turborotalita quinqueloba, δ13C; Turborotalita quinqueloba, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 668 data points
    Location Call Number Limitation Availability
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