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  • 1
    Schlagwort(e): Anthropocene ; stratigraphy
    Beschreibung / Inhaltsverzeichnis: An introduction to the Anthropocene: case for and against a new epoch --- A stratigraphical basis for the Anthropocene? / Colin N. Waters, Jan A. Zalasiewicz, Mark Williams, Michael A. Ellis and Andrea M. Snelling / Geological Society, London, Special Publications, 395, 1-21, 24 March 2014, https://doi.org/10.1144/SP395.18 --- The ‘Anthropocene’ as a ratified unit in the ICS International Chronostratigraphic Chart: fundamental issues that must be addressed by the Task Group / S. C. Finney / Geological Society, London, Special Publications, 395, 23-28, 24 October 2013, https://doi.org/10.1144/SP395.9 --- The term ‘Anthropocene’ in the context of formal geological classification / P. L. Gibbard and M. J. C. Walker / Geological Society, London, Special Publications, 395, 29-37, 25 October 2013, https://doi.org/10.1144/SP395.1 --- Can an Anthropocene Series be defined and recognized? / Jan Zalasiewicz, Mark Williams and Colin N. Waters / Geological Society, London, Special Publications, 395, 39-53, 10 March 2014, https://doi.org/10.1144/SP395.16 --- The nature of anthropogenic deposits and landscape modification --- An assessment of lithostratigraphy for anthropogenic deposits / J. R. Ford, S. J. Price, A. H. Cooper and C. N. Waters / Geological Society, London, Special Publications, 395, 55-89, 8 April 2014, https://doi.org/10.1144/SP395.12 --- The relationship between archaeological stratigraphy and artificial ground and its significance in the Anthropocene / M. Edgeworth / Geological Society, London, Special Publications, 395, 91-108, 25 October 2013, https://doi.org/10.1144/SP395.3 --- The mineral signature of the Anthropocene in its deep-time context / Jan Zalasiewicz, Ryszard Kryza and Mark Williams / Geological Society, London, Special Publications, 395, 109-117, 19 December 2013, https://doi.org/10.1144/SP395.2 --- Geomagnetic and mineral magnetic characterization of the Anthropocene / Ian Snowball, Mark W. Hounslow and Andreas Nilsson / Geological Society, London, Special Publications, 395, 119-141, 19 December 2013, https://doi.org/10.1144/SP395.13 --- A biostratigraphical signature for the Anthropocene --- Is the fossil record of complex animal behaviour a stratigraphical analogue for the Anthropocene? / M. Williams, J. A. Zalasiewicz, C. N. Waters and E. Landing / Geological Society, London, Special Publications, 395, 143-148, 25 October 2013, https://doi.org/10.1144/SP395.8 --- Palaeontological evidence for defining the Anthropocene / Anthony D. Barnosky / Geological Society, London, Special Publications, 395, 149-165, 24 October 2013, https://doi.org/10.1144/SP395.6 --- Coral reefs in the Anthropocene: persistence or the end of the line? / O. Hoegh-Guldberg / Geological Society, London, Special Publications, 395, 167-183, 20 March 2014, https://doi.org/10.1144/SP395.17 --- Microbiotic signatures of the Anthropocene in marginal marine and freshwater palaeoenvironments / I. P. Wilkinson, C. Poirier, M. J. Head, C. D. Sayer and J. Tibby / Geological Society, London, Special Publications, 395, 185-219, 31 January 2014, https://doi.org/10.1144/SP395.14 --- Geochemical signatures and catastrophic events --- Assessing the Anthropocene with geochemical methods / Agnieszka Gałuszka, Zdzisław M. Migaszewski and Jan Zalasiewicz / Geological Society, London, Special Publications, 395, 221-238, 24 October 2013, https://doi.org/10.1144/SP395.5 --- Definition of the Anthropocene: a view from the underworld / Ian J. Fairchild and Silvia Frisia / Geological Society, London, Special Publications, 395, 239-254, 24 October 2013, https://doi.org/10.1144/SP395.7 --- Ice Sheets and the Anthropocene / Eric W. Wolff / Geological Society, London, Special Publications, 395, 255-263, 25 November 2013, https://doi.org/10.1144/SP395.10 --- The release and persistence of radioactive anthropogenic nuclides / Gary J. Hancock, Stephen G. Tims, L. Keith Fifield and Ian T. Webster / Geological Society, London, Special Publications, 395, 265-281, 28 February 2014, https://doi.org/10.1144/SP395.15 --- Volcanic markers for dating the onset of the Anthropocene / Victoria C. Smith / Geological Society, London, Special Publications, 395, 283-299, 21 November 2013, https://doi.org/10.1144/SP395.11 --- The technosphere concept --- Technology as a geological phenomenon: implications for human well-being / P. K. Haff / Geological Society, London, Special Publications, 395, 301-309, 24 October 2013, https://doi.org/10.1144/SP395.4
    Seiten: Online-Ressource (VI, 321 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781862396715
    Sprache: Englisch
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2023-01-30
    Beschreibung: Over annual to decadal timescales changes in the storm track influences regional climate in Europe, however little is known about how the storm track varies over centennial and millennial timescales. We here present two datasets. The first is a reconstruction of storminess from northwest Spain spanning the period 4600-0 cal yrs BP, which was developed by measuring aeolian sand deposits in a peat core from Pedrido Bog, Galicia, Spain. Samples of equal volume (5 cm3) from 1 cm contiguous intervals along the core were processed using the loss-on-ignition method (Heiri et al. 2001), leaving the ignition residue, which was sieved to establish the weight of the 120-180 and 〉180 micron sand fractions. The ignition residue and sand fractions reflect the past amount of sand deposition, which can be used as proxies for storminess. The second dataset is a North-South storm track index reconstruction for western Europe spanning the period 3940-120 cal yrs BP. To create the storm track index, the above described storminess record from Spain was subtracted from a storminess record from Scotland, derived by averaging the results of two storminess reconstructions from the Outer Hebrides, Scotland (Orme et al., 2016). Each record was sampled to the same 20 year temporal resolution and standardised prior to this.
    Schlagwort(e): Europe; Holocene; North Atlantic Oscillation; storminess; storm track
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2023-02-07
    Beschreibung: Over annual to decadal timescales changes in the storm track influences regional climate in Europe, however little is known about how the storm track varies over centennial and millennial timescales. We here present two datasets. The first is a reconstruction of storminess from northwest Spain spanning the period 4600-0 cal yrs BP, which was developed by measuring aeolian sand deposits in a peat core from Pedrido Bog, Galicia, Spain. Samples of equal volume (5 cm3) from 1 cm contiguous intervals along the core were processed using the loss-on-ignition method (Heiri et al. 2001), leaving the ignition residue, which was sieved to establish the weight of the 120-180 and 〉180 micron sand fractions. The ignition residue and sand fractions reflect the past amount of sand deposition, which can be used as proxies for storminess. The second dataset is a North-South storm track index reconstruction for western Europe spanning the period 3940-120 cal yrs BP. To create the storm track index, the above described storminess record from Spain was subtracted from a storminess record from Scotland, derived by averaging the results of two storminess reconstructions from the Outer Hebrides, Scotland (Orme et al., 2016). Each record was sampled to the same 20 year temporal resolution and standardised prior to this.
    Schlagwort(e): After Heiri et al., (2001); AGE; Density, organic matter; DEPTH, sediment/rock; Europe; Grain size, sieving; Holocene; Ignition residue; North Atlantic Oscillation; PEATC; Peat corer; Pedrido_Bog; Size fraction 〉 0.180 mm; Size fraction 0.18-0.12 mm; Spain; storminess; storm track
    Materialart: Dataset
    Format: text/tab-separated-values, 968 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 2023-02-08
    Beschreibung: Storminess in northern Europe varies over annual and decadal timescales, however little is known about how storminess varies over centennial and millennial timescales. In this project two storminess reconstructions were developed from the Outer Hebrides, Scotland. Peat cores were sampled using a Russian corer from a peatbog Struban Bog (57°33'35''N; 7°20'45''W). Samples of equal volume (5 cm3) from 1 cm contiguous intervals along the core were processed using the loss-on-ignition method (Heiri et al. 2001), leaving the ignition residue, which was sieved to establish the weight of the 120-180 and 〉180 micron sand fractions. The ignition residue and sand fractions reflect the past amount of sand deposition, which can be used as a proxies for storminess. Chronological constraints were provided by AMS radiocarbon dates; with 6 dates. The reconstruction from Struban Bog spans the period 4200-180 cal yrs BP.
    Schlagwort(e): After Heiri et al., (2001); AGE; Density, organic matter; DEPTH, sediment/rock; Europe; Grain size, sieving; Holocene; Ignition residue; North Atlantic Oscillation; Outer Hebrides, Scotland; PEATC; Peat corer; Size fraction 〉 0.180 mm; Size fraction 0.18-0.12 mm; storminess; STR; Struban_Bog
    Materialart: Dataset
    Format: text/tab-separated-values, 1132 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Publikationsdatum: 2023-02-07
    Beschreibung: To create the storm track index, the above described storminess record from Spain was subtracted from a storminess record from Scotland, derived by averaging the results of two storminess reconstructions from the Outer Hebrides, Scotland (Orme et al., 2016). Each record was sampled to the same 20 year temporal resolution and standardised prior to this.
    Schlagwort(e): DEPTH, sediment/rock; Europe; Hill_Top_Bog; Holocene; North Atlantic Oscillation; North-south storm track index; Outer Hebrides, Scotland; PEATC; Peat corer; Pedrido_Bog; Spain; storminess; storm track; STR; Struban_Bog
    Materialart: Dataset
    Format: text/tab-separated-values, 192 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Publikationsdatum: 2023-02-07
    Beschreibung: Storminess in northern Europe varies over annual and decadal timescales, however little is known about how storminess varies over centennial and millennial timescales. In this project two storminess reconstructions were developed from the Outer Hebrides, Scotland. Peat cores were sampled using a Russian corer from a peatbog Hill Top Bog (57°10'5''N; 7°20'52W). Samples of equal volume (5 cm3) from 1 cm contiguous intervals along the core were processed using the loss-on-ignition method (Heiri et al. 2001), leaving the ignition residue, which was sieved to establish the weight of the 120-180 and 〉180 micron sand fractions. The ignition residue and sand fractions reflect the past amount of sand deposition, which can be used as a proxies for storminess. Chronological constraints were provided by AMS radiocarbon dates; with 8 dates on the Hill Top Bog core. The reconstruction from Hill Top Bog spans the period 3940-0 cal yrs BP.
    Schlagwort(e): After Heiri et al., (2001); AGE; Density, organic matter; DEPTH, sediment/rock; Europe; Grain size, sieving; Hill_Top_Bog; Holocene; Ignition residue; North Atlantic Oscillation; Outer Hebrides, Scotland; PEATC; Peat corer; Size fraction 〉 0.180 mm; Size fraction 0.18-0.12 mm; storminess
    Materialart: Dataset
    Format: text/tab-separated-values, 1286 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
    Publikationsdatum: 2022-05-26
    Beschreibung: © The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Earth Surface Dynamics 4 (2016): 871-884, doi:10.5194/esurf-4-871-2016.
    Beschreibung: A range of planform morphologies emerge along sandy coastlines as a function of offshore wave climate. It has been implicitly assumed that the morphological response time is rapid compared to the timescales of wave climate change, meaning that coastal morphologies simply reflect the extant wave climate. This assumption has been explored by focussing on the response of two distinctive morphological coastlines – flying spits and cuspate capes – to changing wave climates, using a coastline evolution model. Results indicate that antecedent conditions are important in determining the evolution of morphologies, and that sandy coastlines can demonstrate hysteresis behaviour. In particular, antecedent morphology is particularly important in the evolution of flying spits, with characteristic timescales of morphological adjustment on the order of centuries for large spits. Characteristic timescales vary with the square of aspect ratios of capes and spits; for spits, these timescales are an order of magnitude longer than for capes (centuries vs. decades). When wave climates change more slowly than the relevant characteristic timescales, coastlines are able to adjust in a quasi-equilibrium manner. Our results have important implications for the management of sandy coastlines where decisions may be implicitly and incorrectly based on the assumption that present-day coastlines are in equilibrium with current conditions.
    Beschreibung: This work was funded by NERC national capability core funding to the British Geological Survey.
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
    Digitale Medien
    Digitale Medien
    s.l. : American Chemical Society
    Journal of the American Chemical Society 90 (1968), S. 5576-5579 
    ISSN: 1520-5126
    Quelle: ACS Legacy Archives
    Thema: Chemie und Pharmazie
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    facet.materialart.
    Unbekannt
    Washington, D.C., etc. : Periodicals Archive Online (PAO)
    The Journal of economic education. 10:2 (1979:Spring) 49 
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    Digitale Medien
    Digitale Medien
    [s.l.] : Macmillan Magazines Ltd
    Nature 387 (1997), S. 67-70 
    ISSN: 1476-4687
    Quelle: Nature Archives 1869 - 2009
    Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik
    Notizen: [Auszug] Rheological layering in wax, including a continuous transition between brittle and ductile behaviour, may be made by generating a vertical temperature gradient giving a transition from brittle to ductile behaviour at some depth. Previous ...
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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