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  • 11
    Online Resource
    Online Resource
    Wiley ; 2013
    In:  Journal of Quaternary Science Vol. 28, No. 1 ( 2013-01), p. 95-102
    In: Journal of Quaternary Science, Wiley, Vol. 28, No. 1 ( 2013-01), p. 95-102
    Type of Medium: Online Resource
    ISSN: 0267-8179
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2013
    detail.hit.zdb_id: 2031875-3
    SSG: 13
    SSG: 14
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  • 12
    In: Sedimentology, Wiley, Vol. 66, No. 3 ( 2019-04), p. 781-807
    Abstract: Carbonate sediments in non‐vegetated habitats on the north‐east Adriatic shelf are dominated by shells of molluscs. However, the rate of carbonate molluscan production prior to the 20th century eutrophication and overfishing on this and other shelves remains unknown because: (i) monitoring of ecosystems prior to the 20th century was scarce; and (ii) ecosystem history inferred from cores is masked by condensation and mixing. Here, based on geochronological dating of four bivalve species, carbonate production during the Holocene is assessed in the Gulf of Trieste, where algal and seagrass habitats underwent a major decline during the 20th century. Assemblages of sand‐dwelling Gouldia minima and opportunistic Corbula gibba are time‐averaged to 〉 1000 years and Corbula gibba shells are older by 〉 2000 years than shells of co‐occurring Gouldia minima . This age difference is driven by temporally disjunct production of two species coupled with decimetre‐scale mixing. Stratigraphic unmixing shows that Corbula gibba declined in abundance during the highstand phase and increased again during the 20th century. In contrast, one of the major contributors to carbonate sands – Gouldia minima – increased in abundance during the highstand phase, but declined to almost zero abundance over the past two centuries. Gouldia minima and herbivorous gastropods associated with macroalgae or seagrasses are abundant in the top‐core increments but are rarely alive. Although Gouldia minima is not limited to vegetated habitats, it is abundant in such habitats elsewhere in the Mediterranean Sea. This live–dead mismatch reflects the difference between highstand baseline communities (with soft‐bottom vegetated zones and hard‐bottom Arca beds) and present‐day oligophotic communities with organic‐loving species. Therefore, the decline in light penetration and the loss of vegetated habitats with high molluscan production traces back to the 19th century. More than 50% of the shells on the sea floor in the Gulf of Trieste reflect inactive production that was sourced by heterozoan carbonate factory in algal or seagrass habitats.
    Type of Medium: Online Resource
    ISSN: 0037-0746 , 1365-3091
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2019
    detail.hit.zdb_id: 2020955-1
    detail.hit.zdb_id: 206889-8
    SSG: 13
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  • 13
    Online Resource
    Online Resource
    Wiley ; 2008
    In:  Boreas Vol. 19, No. 3 ( 2008-01-16), p. 226-239
    In: Boreas, Wiley, Vol. 19, No. 3 ( 2008-01-16), p. 226-239
    Type of Medium: Online Resource
    ISSN: 0300-9483
    Language: English
    Publisher: Wiley
    Publication Date: 2008
    detail.hit.zdb_id: 2028632-6
    detail.hit.zdb_id: 185110-X
    SSG: 14
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  • 14
    In: Hydrological Processes, Wiley, Vol. 34, No. 19 ( 2020-09-15), p. 3910-3927
    Abstract: Seasonal suspended sediment transfer in glaciated catchments is responsive to meteorological, geomorphological, and glacio‐fluvial conditions, and thus is a useful indicator of environmental system dynamics. Knowledge of multifaceted fluvial sediment‐transfer processes is limited in the Alaskan Arctic – a region sensitive to contemporary environmental change. For two glaciated sub‐catchments at Lake Peters, northeast Brooks Range, Alaska, we conducted a two‐year endeavour to monitor the hydrology and meteorology, and used the data to derive multiple‐regression models of suspended sediment load. Statistical selection of the best models shows that incorporating meteorological or temporal explanatory variables improves performances of turbidity‐ and discharge‐based sediment models. The resulting modelled specific suspended sediment yields to Lake Peters are: 33 (20–60) t km −2 yr −1 in 2015, and 79 (50–140) t km −2 yr −1 in 2016 (95% confidence band estimates). In contrast to previous studies in Arctic Alaska, fluvial suspended sediment transfer to Lake Peters was primarily influenced by rainfall, and secondarily influenced by temperature‐driven melt processes associated with clockwise diurnal hysteresis. Despite different sub‐catchment glacier coverage, specific yields were the same order of magnitude from the two primary inflows to Lake Peters, which are Carnivore Creek (128 km 2 ; 10% glacier coverage) and Chamberlin Creek (8 km 2 ; 23% glacier coverage). Seasonal to longer‐term sediment exhaustion and/or contrasting glacier dynamics may explain the lower than expected relative specific sediment yield from the more heavily glacierized Chamberlin Creek catchment. Absolute suspended sediment yield (t yr −1 ) from Carnivore Creek to Lake Peters was 27 times greater than from Chamberlin Creek, which we attribute to catchment size and sediment supply differences. Our results provide a foundational understanding of the current sediment transfer regime and are useful for predicting changes in fluvial sediment transport in glaciated Alaskan Arctic catchments.
    Type of Medium: Online Resource
    ISSN: 0885-6087 , 1099-1085
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2020
    detail.hit.zdb_id: 1479953-4
    SSG: 14
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  • 15
    In: Journal of Quaternary Science, Wiley, Vol. 29, No. 4 ( 2014-05), p. 393-400
    Type of Medium: Online Resource
    ISSN: 0267-8179
    Language: English
    Publisher: Wiley
    Publication Date: 2014
    detail.hit.zdb_id: 2031875-3
    SSG: 13
    SSG: 14
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  • 16
    In: Journal of Quaternary Science, Wiley, Vol. 35, No. 1-2 ( 2020-01), p. 81-92
    Abstract: Glass composition‐based correlations of volcanic ash (tephra) traditionally rely on extensive manual plotting. Many previous statistical methods for testing correlations are limited by using geochemical means, masking diagnostic variability. We suggest that machine learning classifiers can expedite correlation, quickly narrowing the list of likely candidates using well‐trained models. Eruptives from Alaska's Aleutian Arc‐Alaska Peninsula and Wrangell volcanic field were used as a test environment for 11 supervised classification algorithms, trained on nearly 2000 electron probe microanalysis measurements of glass major oxides, representing 10 volcanic sources. Artificial neural networks and random forests were consistently among the top‐performing learners (accuracy and kappa 〉 0.96). Their combination as an average ensemble effectively improves their performance. Using this combined model on tephras from Eklutna Lake, south‐central Alaska, showed that predictions match traditional methods and can speed correlation. Although classifiers are useful tools, they should aid expert analysis, not replace it. The Eklutna Lake tephras are mostly from Redoubt Volcano. Besides tephras from known Holocene‐active sources, Holocene tephra geochemically consistent with Pleistocene Emmons Lake Volcanic Center (Dawson tephra), but from a yet unknown source, is evident. These tephras are mostly anchored by a highly resolved varved chronology and represent new important regional stratigraphic markers.
    Type of Medium: Online Resource
    ISSN: 0267-8179 , 1099-1417
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2020
    detail.hit.zdb_id: 2031875-3
    SSG: 13
    SSG: 14
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  • 17
    In: Transfusion, Wiley, Vol. 53, No. 9 ( 2013-09), p. 2069-2077
    Abstract: How Rh immune globulin ( RhIG ) prevents sensitization to D antigen is unclear. If RhIG Fc delivers a nonspecific immunosuppressive signal, then RhIG may inhibit sensitization to antigens other than D . HLA antibody prevalence was compared in previously pregnant D– versus D+ women to investigate whether RhIG suppresses HLA sensitization. Study Design and Methods In the L eukocyte A ntibody P revalence S tudy ( LAPS ), 7920 volunteer blood donors were screened for anti‐ HLA and surveyed about prior pregnancies and transfusions. A secondary analysis of the LAPS database was performed. Results D– women not more than 40 years old (presumed to have received antenatal with or without postpartum RhIG in all pregnancies) had a significantly lower HLA sensitization rate than D+ women (relative risk, 0.58; 95% confidence interval [ CI ], 0.40‐0.83). When stratified by deliveries (one, two, three, or four or more), D– women not older than 40 were HLA sensitized less often than D+ women in every case. In contrast, a clear relationship between D type and HLA sensitization was not seen in older previously pregnant women whose childbearing years are presumed to have preceded the use of routine RhIG prophylaxis. In a multivariable logistic regression model, D– women not more than 40 years old remained significantly less likely to be HLA sensitized compared with D+ women after adjusting for parity, time from last pregnancy, lost pregnancies, and transfusions (odds ratio [ OR ], 0.55; 95% CI , 0.34‐0.88). Conclusion Consistent with a nonspecific immunosuppressive effect of RhIG , younger previously pregnant D– women were less likely than previously pregnant D+ women to be HLA sensitized.
    Type of Medium: Online Resource
    ISSN: 0041-1132 , 1537-2995
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2013
    detail.hit.zdb_id: 2018415-3
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