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  • 2020-2024  (56)
  • 2000-2004  (11)
  • 1990-1994  (1)
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  • 1
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The carbon-isotope signature of terrestrial organic matter (OM) offers a valuable tool to develop stratigraphic correlations for near-shore deposits. A mid-Cretaceous coastal succession of the western Algarve Basin, Portugal, displays a marked negative δ13C excursion ranging from − 21.2‰ to − 27.8‰ in the Early Aptian followed by two shifts towards higher values (up to − 19.3‰) during the Early and Late Aptian, respectively. The dominance of cuticle and leaf debris in the bulk OM fraction is confirmed by optical studies, Rock-Eval pyrolysis and by comparison with the δ13C signature of four different types of fossilized land-plant particles. Correlation of two terrestrial δ13Cbulk OM records from different study sites leads to a significant enhancement of the intrabasinal stratigraphic correlation within the Algarve Basin. Three prominent excursions in the Portuguese records can be correlated with existing δ13C curves from pelagic and terrestrial environments. The general carbon-isotope pattern is superimposed by small-scale fluctuations which can be explained by compositional variations within the OM.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    BIT 30 (1990), S. 2-16 
    ISSN: 1572-9125
    Keywords: E.2 ; F.2.1 ; G.4 ; I.1.2 ; Matrix transposition ; mixed radix notation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mathematics
    Notes: Abstract An algorithm is developed and described for transposing a matrix larger than available working storage. If an (n×m)-matrix is stored in row-major order, and blocks ofn elements may be transferred to and from working storage at a time, the algorithm needsw=(5[m/n]+8)·n elements to be present in working storage at a time and requires [log2(2mn/w)] passages over the matrix. The algorithm is as efficient as earlier methods but needs no extra backing storage space. An algebra for mixed radix notation and a generalization of mixed radix notation is introduced for the description and verification of transposition algorithms, and earlier algorithms are briefly certified or disproved.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2023-02-08
    Description: The Labrador Sea is important for the modern global thermohaline circulation system through the formation of intermediate Labrador Sea Water (LSW) that has been hypothesized to stabilize the modern mode of North Atlantic deep-water circulation. The rate of LSW formation is controlled by the amount of winter heat loss to the atmosphere, the expanse of freshwater in the convection region and the inflow of saline waters from the Atlantic. The Labrador Sea, today, receives freshwater through the East and West Greenland currents (EGC, WGC) and the Labrador Current (LC). Several studies have suggested the WGC to be the main supplier of freshwater to the Labrador Sea, but the role of the southward flowing LC in Labrador Sea convection is still debated. At the same time, many paleoceanographic reconstructions from the Labrador Shelf focussed on late deglacial to early Holocene meltwater run-off from the Laurentide Ice Sheet (LIS), whereas little information exists about LC variability since the final melting of the LIS about 7000 years ago. In order to enable better assessment of the role of the LC in deep-water formation and its importance for Holocene climate variability in Atlantic Canada, this study presents high-resolution middle to late Holocene records of sea surface and bottom water temperatures, freshening, and sea ice cover on the Labrador Shelf during the last 6000 years. Our records reveal that the LC underwent three major oceanographic phases from the mid- to late Holocene. From 6.2 to 5.6 ka, the LC experienced a cold episode that was followed by warmer conditions between 5.6 and 2.1 ka, possibly associated with the late Holocene thermal maximum. While surface waters on the Labrador Shelf cooled gradually after 3 ka in response to the neoglaciation, Labrador Shelf subsurface or bottom waters show a shift to warmer temperatures after 2.1 ka. Although such an inverse stratification by cooling of surface and warming of subsurface waters on the Labrador Shelf would suggest a diminished convection during the last 2 millennia compared to the mid-Holocene, it remains difficult to assess whether hydrographic conditions in the LC have had a significant impact on Labrador Sea deep-water formation.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2023-03-25
    Description: We present stable hydrogen isotope (dD) and carbon isotope (d13C) of sedimentary terrestrial leaf wax, namely n-alkanes, from marine sediment core SO 188-17286-1 (Bay of Bengal, 19°44.58′N, 89°52.76′E, 1428 m water depth) for the last ~130 kyr. There are four different homologues (n-C27, n-C29, n-C31 and n-C33). The concentration data of each homologues are also present here. Identification and quantification (concentration) of the individual compounds was carried out with an Agilent 6890 Gas Chromatograph (GC) with a flame ionization detector in the Geoscience, University of Kiel. The d13C and dD values of n-alkanes were then analyzed at the Leibniz Laboratory for Radiometric Dating and Stable Isotope Research in Kiel University using an Agilent 6890 GC coupled with a Thermo Finnigan MAT 253 isotope ratio mass (IRMS).
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 5
    Publication Date: 2023-01-30
    Description: The Mozambique Channel is a conduit of trade wind-driven throughflow that is a key component of the Agulhas Current and Agulhas leakage, a flux of warm and salty water from the tropical Indo-Pacific to the Atlantic Ocean. Agulhas leakage is thought to modulate Atlantic meridional overturning circulation variability. Previous studies from the Cape Basin suggest that enhanced Agulhas leakage played an important role in accelerating glacial terminations. The southern African monsoon response to abrupt climate changes associated with meltwater-induced reorganizations of the North Atlantic meridional overturning circulation, and its impact on the Mozambique Channel throughflow and, by extension, on the Agulhas leakage is not well understood. Here we present a high-resolution 26,000 year-long hydroclimate record of northern Madagascar, a core region of the southern hemisphere monsoon domain, and a mixed layer temperature reconstruction using sediment cores collected from the runoff-influenced eastern Mozambique Channel. The record indicates precipitation increases centered at 11.7-12.5 thousand years before present (kyr BP), 14.5-19 kyr BP, 23-24 kyr BP, 25-26 kyr BP. Considering age model uncertainties, this is the first strong evidence for southern African monsoon strengthening in response to meltwater-induced northern high latitude climate instabilities during the Younger Dryas (YD), Heinrich Stadial 1 (HS1), HS2 and the HS-like event prior to HS2, in agreement with the results of transient climate simulations. Furthermore, our study shows a reversal of the mixed layer temperature gradient between the western and eastern Mozambique Channel during Heinrich event 1 (HE1). We posit that the gradient reversal indicates a weakening of the trade wind-driven South Equatorial Current and Mozambique Channel throughflow that likely weakened the Agulhas leakage, potentially creating a feedback that may have contributed to the sustained weakening of the AMOC during HE1 by reducing the amount of heat and salt leakage into the Atlantic.
    Keywords: Agulhas Leakage; marine sediments; Mozambique Channel; Mozambique Channel throughflow; oxygen isotope data; SST
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 6
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    PANGAEA
    Publication Date: 2023-02-24
    Keywords: ANT-VII/5; Calculated; Calculated from UK'37 (Prahl et al., 1988); DATE/TIME; Date/time end; DEPTH, water; Duration, number of days; GeoB; Geosciences, University of Bremen; Polarstern; PS14; Sample code/label; Sea surface temperature, annual mean; Trap; TRAP; Walvis Ridge, Southeast Atlantic Ocean; WR2_trap
    Type: Dataset
    Format: text/tab-separated-values, 78 data points
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  • 7
    Publication Date: 2023-06-27
    Keywords: AGE; Age, 14C; Age, uncertainty; Agulhas Leakage; Calendar age; Calendar age, error to older; Calendar age, error to younger; Core; Date/Time of event; DEPTH, sediment/rock; Event label; GIK16163-2; GIK16164-2; GIK16166-2; Gravity corer (Kiel type); Laboratory code/label; Latitude of event; Longitude of event; M75/3; M75/3_143-2; M75/3_144-2; M75/3_146-2; marine sediments; Meteor (1986); Mozambique Channel; Mozambique Channel throughflow; oxygen isotope data; Sample material; SL; SST
    Type: Dataset
    Format: text/tab-separated-values, 217 data points
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  • 8
    Publication Date: 2023-06-27
    Keywords: AGE; Agulhas Leakage; Calculated; Core; Date/Time of event; DEPTH, sediment/rock; Event label; GIK16163-2; GIK16164-2; GIK16166-2; Globigerinoides ruber white, Magnesium/Calcium ratio; Gravity corer (Kiel type); Latitude of event; Longitude of event; M75/3; M75/3_143-2; M75/3_144-2; M75/3_146-2; marine sediments; Meteor (1986); Mozambique Channel; Mozambique Channel throughflow; oxygen isotope data; SL; SST
    Type: Dataset
    Format: text/tab-separated-values, 522 data points
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  • 9
    Publication Date: 2023-06-27
    Keywords: AGE; Agulhas Leakage; Core; Date/Time of event; DEPTH, sediment/rock; Error; Event label; GIK16163-2; GIK16164-2; GIK16166-2; Globigerinoides ruber white, δ18O; Globigerinoides ruber white, δ18O standard deviation; Gravity corer (Kiel type); Latitude of event; Longitude of event; M75/3; M75/3_143-2; M75/3_144-2; M75/3_146-2; marine sediments; Meteor (1986); Mozambique Channel; Mozambique Channel throughflow; oxygen isotope data; Sea water temperaure & ice volume effects corrected; SL; SST
    Type: Dataset
    Format: text/tab-separated-values, 1908 data points
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  • 10
    Publication Date: 2023-06-27
    Keywords: AGE; Agilent 6890 GC coupled with a Thermo Finnigan MAT 253 isotope ratio mass (IRMS); Bay of Bengal; Bengal Sea Level; DEPTH, sediment/rock; GIK17286-1; Gravity corer (Kiel type); n-Alkane C27, δD; n-Alkane C27, δD, standard error; n-Alkane C29, δD; n-Alkane C29, δD, standard error; n-Alkane C31, δD; n-Alkane C31, δD, standard error; n-Alkane C33, δD; n-Alkane C33, δD, standard error; SL; SO188/1; Sonne
    Type: Dataset
    Format: text/tab-separated-values, 1050 data points
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