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  • 1
    Monograph available for loan
    Monograph available for loan
    Amsterdem
    Call number: G 6040 / Regal 13
    Type of Medium: Monograph available for loan
    Pages: 104 S. : graph. Darst., Kt.
    Note: Amsterdam, Univ., Diss., 1933
    Location: Magazine - must be ordered
    Branch Library: GFZ Library
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  • 2
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Cell Differentiation and Development 32 (1990), S. 189-202 
    ISSN: 0922-3371
    Keywords: Adhesion ; Cancer ; Extracellular Matrix ; Integrins ; Receptors
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 210 (1966), S. 1017-1019 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] RECENT investigations1-5 suggest that adenosine-Jtv S^S'-monophosphate (cyclic AMP) acts as a cellular mediator involved in the tissue response to a number of hormones, including catecholamines, glucagon, adreno-corticotrophic hormone and vasopressin. It is clear that cyclic AMP may produce ...
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 1966-06-01
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Published by Springer Nature
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  • 5
    Publication Date: 2022-05-27
    Description: © The Author(s), 2021. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Drake, H. F., Rivest, R. L., Edelman, A., & Deutch, J. A simple model for assessing climate control trade-offs and responding to unanticipated climate outcomes. Environmental Research Letters, 16(10), (2021): 104012, https://doi.org/10.1088/1748-9326/ac243e.
    Description: Persistent greenhouse gas (GHG) emissions threaten global climate goals and have prompted consideration of climate controls supplementary to emissions mitigation. We present MARGO, an idealized model of optimally-controlled climate change, which is complementary to both simpler conceptual models and more complicated Integrated Assessment Models. The four methods of controlling climate damage—mitigation, carbon dioxide removal (CDR), adaptation, and solar radiation modification (SRM)—are not interchangeable, as they enter at different stages of the causal chain that connects GHG emissions to climate damages. Early and aggressive mitigation is necessary to stabilize GHG concentrations below a tolerable level. While the most cost-beneficial and cost-effective pathways to reducing climate suffering include deployments of all four controls, the quantitative trade-offs between the different controls are sensitive to value-driven parameters and poorly-known future costs and damages. Static policy optimization assumes perfect foresight and obscures the active role decision-makers have in shaping a climate trajectory. We propose an explicit policy response process wherein climate control policies are re-adjusted over time in response to unanticipated outcomes. We illustrate this process in two 'storyline' scenarios: (a) near-term increases in mitigation and CDR are deficient, such that climate goals are expected to slip out of reach; (b) SRM is abruptly terminated after 40 years of successful deployment, causing an extremely rapid warming which is amplified by an excess of GHGs due to deterred mitigation. In both cases, an optimized policy response yields substantial benefits relative to continuing the original policy. The MARGO model is intentionally designed to be as simple, transparent, customizable, and accessible as possible, addressing concerns about previous climate-economic modelling approaches and enabling a more diverse set of stakeholders to engage with these essential and timely topics.
    Description: This material is based upon work supported by the National Science Foundation Graduate Research Fellowship Program under Grant No. 174530.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 6
    Publication Date: 2023-03-03
    Keywords: Communality; DEPTH, sediment/rock; Factor 1; Factor 2; Factor 3; Factor 4; Factor analysis; GeoTü; M5/2; M5/2_91MC; Meteor (1986); MUC; MultiCorer; Paleoceanography at Tübingen University
    Type: Dataset
    Format: text/tab-separated-values, 70 data points
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  • 7
    Publication Date: 2023-03-03
    Keywords: Communality; DEPTH, sediment/rock; Factor 1; Factor 2; Factor 3; Factor 4; Factor analysis; GeoTü; M5/2; M5/2_93MC; Meteor (1986); MUC; MultiCorer; Paleoceanography at Tübingen University
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 8
    Publication Date: 2023-03-03
    Keywords: Communality; DEPTH, sediment/rock; Factor 1; Factor 2; Factor 3; Factor 4; Factor analysis; GeoTü; M5/2; M5/2_98MC; Meteor (1986); MUC; MultiCorer; Paleoceanography at Tübingen University
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Edelman-Furstenberg, Yael; Scherbacher, Maria; Hemleben, Christoph; Almogi-Labin, Ahuva (2001): Deep-sea benthic foraminifera from the central Red Sea. Journal of Foraminiferal Research, 31(1), 48-59, https://doi.org/10.2113/0310048
    Publication Date: 2023-05-12
    Description: The distribution of living (Rose Bengal-stained), dead and fossil benthic foraminifera was investigated in six short cores (multicores, 30-32 cm total length) recovered from the central Red Sea. The ecological preferences as well as the relationship between the live and dead/fossil assemblages (preserved down-core) were examined. The sites, located along a W-E profile and between the depth of 366 and 1782 m, extend from the center of the oxygen minimum zone (OMZ, ~200-650 m), through its margin at ~600 m, and down to the well-aerated deep-water environment. Live (Rose-Bengal stained) and coexisting dead foraminifera were studied in the upper 5 cm of each of the sites, and the fossil record was studied down to ~32 cm. Q-mode Principal Component Analysis was used and four distinct foraminiferal fossil assemblages were determined. These assemblages follow different water mass properties. In the center of the OMZ, where the organic carbon content is highest and the oxygen concentration is lowest (〈=0.5 ml O2/l), the Bolivina persiensis-Bulimina marginata-Discorbinella rhodiensis assemblage dominates. The slightly more aerated and lower organic-carbon-content seafloor, at the margin of the OMZ, is characterized by the Neouvigerina porrecta-Gyroidinoides cf. G. soldanii assemblage. The transitional environment, between 900-1200 m, with its well-aerated and oligotrophic seafloor, is dominated by the Neouvigerina ampullacea-Cibicides mabahethi assemblage. The deeper water (〉1500 m), characterized by the most oxygenated and oligotrophic seafloor conditions, is associated with the Astrononion sp. A-Hanzawaia sp. A assemblage. Throughout the Red Sea extremely high values of temperature and salinity are constant below ~200 m depth, but the flux of organic matter to the sea floor varies considerably with bathymetry and appears to be the main controlling factor governing the distribution pattern of the benthic foraminifera. Comparison between live and the dead/fossil assemblages reveals a large difference between the two. Processes that may control this difference include species-specific high turnover rates, and preferential predation and loss of fragile taxa (either by chemical or microbial processes). Significant variations in the degree of loss of the organic-cemented agglutinants were observed down core. This group is preserved down to 5-10 cm at the shallow OMZ sites and down to greater depths at well-aerated and oligotrophic sites. The lower rate of disintegration of these forms, in the deeper locations of the Red Sea, may be related to low microbial activity. This results in the preservation of increasing numbers of organic-cemented shells down-core.
    Keywords: GeoTü; M5/2; M5/2_100MC; M5/2_107MC; M5/2_88MC; M5/2_91MC; M5/2_93MC; M5/2_98MC; Meteor (1986); MUC; MultiCorer; Paleoceanography at Tübingen University
    Type: Dataset
    Format: application/zip, 29 datasets
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  • 10
    Publication Date: 2023-03-03
    Keywords: Communality; DEPTH, sediment/rock; Factor 1; Factor 2; Factor 3; Factor 4; Factor analysis; GeoTü; M5/2; M5/2_88MC; Meteor (1986); MUC; MultiCorer; Paleoceanography at Tübingen University
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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