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  • Cambridge University Press (CUP)  (4)
  • 1
    In: Quaternary Research, Cambridge University Press (CUP), Vol. 44, No. 3 ( 1995-11), p. 303-316
    Materialart: Online-Ressource
    ISSN: 0033-5894
    RVK:
    Sprache: Englisch
    Verlag: Cambridge University Press (CUP)
    Publikationsdatum: 1995
    ZDB Id: 1471589-2
    ZDB Id: 205711-6
    SSG: 13
    SSG: 14
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Online-Ressource
    Online-Ressource
    Cambridge University Press (CUP) ; 1999
    In:  Quaternary Research Vol. 51, No. 1 ( 1999-01), p. 83-93
    In: Quaternary Research, Cambridge University Press (CUP), Vol. 51, No. 1 ( 1999-01), p. 83-93
    Kurzfassung: Marine sediment cores from the continental slope off mid-latitude Chile (33°S) were studied with regard to grain-size distributions and clay mineral composition. The data provide a 28,000-yr 14 C accelerator mass spectrometry-dated record of variations in the terrigenous sediment supply reflecting modifications of weathering conditions and sediment source areas in the continental hinterland. These variations can be interpreted in terms of the paleoclimatic evolution of mid-latitude Chile and are compared to existing terrestrial records. Glacial climates (28,000–18,000 cal yr B.P.) were generally cold–humid with a cold–semiarid interval between 26,000 and 22,000 cal yr B.P. The deglaciation was characterized by a trend toward more arid conditions. During the middle Holocene (8000–4000 cal yr B.P.), comparatively stable climatic conditions prevailed with increased aridity in the Coastal Range. The late Holocene (4000–0 cal yr B.P.) was marked by more variable paleoclimates with generally more humid conditions. Variations of rainfall in mid-latitude Chile are most likely controlled by shifts of the latitudinal position of the Southern Westerlies. Compared to the Holocene, the southern westerly wind belt was located significantly farther north during the last glacial maximum. Less important variations of the latitudinal position of the Southern Westerlies also occurred on shorter time scales.
    Materialart: Online-Ressource
    ISSN: 0033-5894 , 1096-0287
    RVK:
    Sprache: Englisch
    Verlag: Cambridge University Press (CUP)
    Publikationsdatum: 1999
    ZDB Id: 1471589-2
    ZDB Id: 205711-6
    SSG: 13
    SSG: 14
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Online-Ressource
    Online-Ressource
    Cambridge University Press (CUP) ; 2006
    In:  Quaternary Research Vol. 65, No. 3 ( 2006-05), p. 519-525
    In: Quaternary Research, Cambridge University Press (CUP), Vol. 65, No. 3 ( 2006-05), p. 519-525
    Kurzfassung: A geochemical and paleontological reconstruction of paleoproductivity, upwelling intensity and sea surface temperature (SST) off central Chile at 35°S (GeoB3359-3) reveals marked changes from the Last Glacial Maximum (LGM) through the Early Holocene. Surface-water productivity was determined by the interaction between the atmospheric (the Southern Westerlies) and oceanographic (the Antarctic Circumpolar Current, ACC) systems from the LGM through early Termination I (TI). The northward shift of the climate zones during the LGM brought the ACC, as the main macronutrient source, closer to the GeoB3359-3, SST lowered, and surface water productivity and accumulation rates of biogenic components enhanced. With the poleward return of the Southern Westerlies and the ACC, the subtropical high-pressure system became the dominant atmospheric component southward till 35°S during the late TI and Early Holocene and caused surface water productivity to increase through enhanced upwelling.
    Materialart: Online-Ressource
    ISSN: 0033-5894 , 1096-0287
    RVK:
    Sprache: Englisch
    Verlag: Cambridge University Press (CUP)
    Publikationsdatum: 2006
    ZDB Id: 1471589-2
    ZDB Id: 205711-6
    SSG: 13
    SSG: 14
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Online-Ressource
    Online-Ressource
    Cambridge University Press (CUP) ; 2005
    In:  Journal of the Marine Biological Association of the United Kingdom Vol. 85, No. 2 ( 2005-04), p. 233-245
    In: Journal of the Marine Biological Association of the United Kingdom, Cambridge University Press (CUP), Vol. 85, No. 2 ( 2005-04), p. 233-245
    Kurzfassung: A quantitative study of macrobenthos was carried out on three transects on the shelf and continental slope off Chile (22° to 42°S; from 100 to 2000 m water depth) within and beneath the oxygen minimum zone (OMZ). Macrobenthos mean densities ranged from 104 to 13 808 ind m −2 , with highest values off Concepción (∼36°S), where highest chloroplastic pigment equivalents were also measured. Polychaetes were the numerically dominant group in all transects and depths, followed by peracarid crustaceans. Species richness and diversity correlated with observed changes in bottom-water oxygen concentrations and sediment-bound pigments. Our results show that the shelf macrobenthic communities were negatively affected by low oxygen. The non-metric multidimensional scaling (nMDS) analysis evidenced depth-related station groups which may be related to the different environments provided by the water masses involved. Indeed, the depth ranges of stations groups with their specific species inventories coincide quite well with the boundaries of the three important water masses in the region, the Equatorial Subsurface Water (∼50 m to ∼400 m depth), the Antarctic Intermediate Water (∼400 to ∼1200 m depth), and the Pacific Deep Water ( 〉 1200 m depth).
    Materialart: Online-Ressource
    ISSN: 0025-3154 , 1469-7769
    RVK:
    Sprache: Englisch
    Verlag: Cambridge University Press (CUP)
    Publikationsdatum: 2005
    ZDB Id: 1491269-7
    ZDB Id: 281325-7
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
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