GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 2010-2014  (20)
Document type
Keywords
Publisher
Years
Year
  • 1
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2013. This is the author's version of the work. It is posted here by permission of Nature Publishing Group for personal use, not for redistribution. The definitive version was published in Nature Geoscience 7 (2014):144–150, doi:10.1038/ngeo2045.
    Description: Heinrich events - surges of icebergs into the North Atlantic Ocean - punctuated the last glacial period. The events are associated with millennial-scale cooling in the Northern Hemisphere. Freshwater from the melting icebergs is thought to have interrupted the Atlantic meridional overturning circulation, thus minimizing heat transport into the northern North Atlantic. The northward flow of warm water passes through the Florida Straits and is reflected in the distribution of seawater properties in this region. Here we investigate the northward flow through this region over the past 40,000 years using oxygen isotope measurements of benthic foraminifera from two cores on either side of the Florida Straits, which allow us to estimate water density, which is related to flow via the thermal wind relation. We infer a substantial reduction of flow during Heinrich Event 1 and the Heinrich-like Younger Dryas cooling, but little change during Heinrich Events 2 and 3, which occurred during an especially cold phase of the last glacial period. We speculate that because glacial circulation was already weakened before the onset of Heinrich Events 2 and 3, freshwater forcing had little additional effect. However, low-latitude climate perturbations were observed during all events. We therefore suggest these perturbations may not have been directly caused by changes in heat transport associated with Atlantic overturning circulation as commonly assumed.
    Description: The authors acknowledge the US National Science Foundation (OCE-0096472, OCE-0648258 and OCE-1102743), a grant from the Comer Science and Education Foundation and a Rutt Bridges Undergraduate Research Fellowship to L.G.H. for funding this work. PC acknowledges the supports from the Natural Science Foundation of China (40921004 and 40930844). S.M. was funded through the DFG Research Center/Cluster of Excellence “The Ocean in the Earth System”.
    Description: 2014-07-12
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Channell, James E T; Hodell, David A; Margari, Vasiliki; Skinner, Luke C; Tzedakis, Polychronis C; Kesler, M S (2013): Biogenic magnetite, detrital hematite, and relative paleointensity in Quaternary sediments from the Southwest Iberian Margin. Earth and Planetary Science Letters, 376, 99-109, https://doi.org/10.1016/j.epsl.2013.06.026
    Publication Date: 2023-07-20
    Description: Magnetic properties of late Quaternary sediments on the SW Iberian Margin are dominated by bacterial magnetite, observed by transmission electron microscopy (TEM), with contributions from detrital titanomagnetite and hematite. Reactive hematite from eolian dust, together with low organic matter concentrations and the lack of sulfate reduction, lead to dissimilatory iron reduction and availability of Fe(II) for abundant magnetotactic bacteria. Magnetite grain-size proxies (kARM/k and ARM/IRM) and S-ratios (sensitive to hematite) vary on stadial/interstadial timescales, contain orbital power, and mimic planktic d18O. The detrital/biogenic magnetite ratio and hematite concentration are greater during stadials and glacial isotopic stages, reflecting increased detrital (magnetite) input during times of lowered sea level, coinciding with atmospheric conditions favoring hematitic dust supply. Magnetic susceptibility, on the other hand, has a very different response being sensitive to coarse detrital multidomain (MD) magnetite associated with ice-rafted debris (IRD). High susceptibility and/or magnetic grain size coarsening, mark Heinrich stadials (HS), particularly HS2, HS3, HS4, HS5, HS6 and HS7, as well as older Heinrich-like detrital layers, indicating the sensitivity of this region to fluctuations in the position of the polar front. Relative paleointensity (RPI) records have well-constrained age models based on planktic d18O correlation to ice-core chronologies, however, they differ from reference records (e.g. PISO) particularly in the vicinity of glacial maxima, mainly due to inefficient normalization of RPI records in intervals of enhanced detrital/eolian hematite input.
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2023-07-20
    Keywords: Absolute; CALYPSO; Calypso Corer; Correlation coefficient; DEPTH, sediment/rock; GEOSCIENCES, MARMARCORE; Marion Dufresne (1995); Maximum angular deviation; MD01-2444; MD123; NRM, Declination; NRM, Inclination; Slope
    Type: Dataset
    Format: text/tab-separated-values, 30720 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2023-07-20
    Keywords: Absolute; CALYPSO; Calypso Corer; Correlation coefficient; DEPTH, sediment/rock; GEOSCIENCES, MARMARCORE; Marion Dufresne (1995); Maximum angular deviation; MD01-2443; MD123; NRM, Declination; NRM, Inclination; Slope
    Type: Dataset
    Format: text/tab-separated-values, 33792 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hodell, David A; Crowhurst, Simon J; Skinner, Luke C; Tzedakis, Polychronis C; Margari, Vasiliki; Channell, James E T; Kamenov, George D; Maclachlan, Suzanne; Rothwell, Robin Guy (2013): Response of Iberian Margin sediments to orbital and suborbital forcing over the past 420 ka. Paleoceanography, 28(1), 185-199, https://doi.org/10.1002/palo.20017
    Publication Date: 2023-09-16
    Description: Here we report 420 kyr long records of sediment geochemical and color variations from the southwestern Iberian Margin. We synchronized the Iberian Margin sediment record to Antarctic ice cores and speleothem records on millennial time scales and investigated the phase responses relative to orbital forcing of multiple proxy records available from these cores. Iberian Margin sediments contain strong precession power. Sediment "redness" (a* and 570-560 nm) and the ratio of long-chain alcohols to n-alkanes (C26OH/(C26OH + C29)) are highly coherent and in-phase with precession. Redder layers and more oxidizing conditions (low alcohol ratio) occur near precession minima (summer insolation maxima). We suggest these proxies respond rapidly to low-latitude insolation forcing by wind-driven processes (e.g., dust transport, upwelling, precipitation). Most Iberian Margin sediment parameters lag obliquity maxima by 7-8 ka, indicating a consistent linear response to insolation forcing at obliquity frequencies driven mainly by high-latitude processes. Although the lengths of the time series are short (420 ka) for detecting 100 kyr eccentricity cycles, the phase relationships support those obtained by Shackleton []. Antarctic temperature and the Iberian Margin alcohol ratios (C26OH/(C26OH + C29)) lead eccentricity maxima by 6 kyr, with lower ratios (increased oxygenation) occurring at eccentricity maxima. CO2, CH4, and Iberian SST are nearly in phase with eccentricity, and minimum ice volume (as inferred from Pacific d18Oseawater) lags eccentricity maxima by 10 kyr. The phase relationships derived in this study continue to support a potential role of the Earth's carbon cycle in contributing to the 100 kyr cycle.
    Type: Dataset
    Format: application/zip, 9 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Margari, Vasiliki; Skinner, Luke C; Hodell, David A; Martrat, Belén; Toucanne, Samuel; Grimalt, Joan O; Gibbard, Philip L; Lunkka, Juha Pekka; Tzedakis, Polychronis C (2014): Land-ocean changes on orbital and millennial time scales and the penultimate glaciation. Geology, 42(3), 183-186, https://doi.org/10.1130/G35070.1
    Publication Date: 2023-09-16
    Description: Past glacials can be thought of as natural experiments in which variations in boundary conditions influenced the character of climate change. However, beyond the last glacial, an integrated view of orbital- and millennial-scale changes and their relation to the record of glaciation has been lacking. Here, we present a detailed record of variations in the land-ocean system from the Portuguese margin during the penultimate glacial and place it within the framework of ice-volume changes, with particular reference to European ice-sheet dynamics. The interaction of orbital- and millennial-scale variability divides the glacial into an early part with warmer and wetter overall conditions and prominent climate oscillations, a transitional mid-part, and a late part with more subdued changes as the system entered a maximum glacial state. The most extreme event occurred in the mid-part and was associated with melting of the extensive European ice sheet and maximum discharge from the Fleuve Manche river. This led to disruption of the meridional overturning circulation, but not a major activation of the bipolar seesaw. In addition to stadial duration, magnitude of freshwater forcing, and background climate, the evidence also points to the influence of the location of freshwater discharges on the extent of interhemispheric heat transport.
    Keywords: AGE; Alkenone, C37:4; Calculated from UK'37 (Müller et al, 1998); CALYPSO; Calypso Corer; DEPTH, sediment/rock; GEOSCIENCES, MARMARCORE; Marion Dufresne (1995); MD01-2444; MD123; Sea surface temperature, annual mean
    Type: Dataset
    Format: text/tab-separated-values, 318 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2023-09-16
    Keywords: AGE; CALYPSO; Calypso Corer; Color, a*; Color, b*; Color, L*, lightness; Color reflectance interval 560-570 nm wavelength; Depth, composite; DEPTH, sediment/rock; GEOSCIENCES, MARMARCORE; Intercore correlation; Marion Dufresne (1995); MD01-2444; MD123; SPEC; Spectrophotometer
    Type: Dataset
    Format: text/tab-separated-values, 26800 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2023-09-16
    Keywords: AGE; Alkenone, C37:4; Calculated from UK'37 (Müller et al, 1998); CALYPSO; Calypso Corer; DEPTH, sediment/rock; Event label; GEOSCIENCES, MARMARCORE; Marion Dufresne (1995); MD01-2443; MD01-2444; MD123; n-hexacosan-1-ol/(n-hexacosan-1-ol + n-nonacosane) ratio; Sea surface temperature, annual mean
    Type: Dataset
    Format: text/tab-separated-values, 4613 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2023-09-16
    Keywords: Calcium/Titanium ratio; Calcium carbonate; CALYPSO; Calypso Corer; DEPTH, sediment/rock; GEOSCIENCES, MARMARCORE; log-Titanium/Calcium ratio; Marion Dufresne (1995); MD01-2444; MD123; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 2082 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2023-09-16
    Keywords: -; AGE; COMPCORE; Composite Core; GEOSCIENCES, MARMARCORE; Marion Dufresne (1995); MD01-2444/2443; MD123
    Type: Dataset
    Format: text/tab-separated-values, 4202 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...