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  • 1
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    A Stratigraphical Basis for the Anthropocene (2014)
    London : The Geological Society
    Details
    Keywords: Anthropocene ; stratigraphy
    Description / Table of Contents: 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
    Pages: Online-Ressource (VI, 321 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781862396715
    URL: https://sp.lyellcollection.org/content/395/1
    Language: English
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    E-BOOK
  • 2
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    Reconstruction of past storminess and storm track position, evidence from Pedrido Bog, Galicia, Spain (2021)
    PANGAEA
    Details
    Publication Date: 2023-01-30
    Description: 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.
    Keywords: Europe; Holocene; North Atlantic Oscillation; storminess; storm track
    Type: Dataset
    Format: application/zip, 2 datasets
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    DATA PANGAEA
  • 3
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    Sand-based storminess proxies from Pedrido Bog, Galicia, Spain (2021)
    PANGAEA
    Details
    Publication Date: 2023-02-07
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 968 data points
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    DATA PANGAEA
  • 4
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    Sand-based storminess proxies from a coastal peatland Struban Bog, Outer Hebrides, Scotland (2021)
    PANGAEA
    Details
    Publication Date: 2023-02-08
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1132 data points
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  • 5
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    North-south storm track index reconstruction for western Europe from Pedrido Bog, Galicia, Spain (2021)
    PANGAEA
    Details
    Publication Date: 2023-02-07
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 192 data points
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  • 6
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    Sand-based storminess proxies from a coastal peatland Hill Top Bog, Outer Hebrides, Scotland (2021)
    PANGAEA
    Details
    Publication Date: 2023-02-07
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1286 data points
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  • 7
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    Complex coastlines responding to climate change : do shoreline shapes reflect present forcing or “remember” the distant past? (2017)
    Copernicus Publications on behalf of the European Geosciences Union
    Details
    Publication Date: 2022-05-26
    Description: © 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.
    Description: 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.
    Description: This work was funded by NERC national capability core funding to the British Geological Survey.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 8
    Electronic Resource
    Electronic Resource
    Thermal rearrangement of cyclopropylimines. III. Total synthesis of pyridine alkaloids (1968)
    s.l. : American Chemical Society
    Journal of the American Chemical Society 90 (1968), S. 5576-5579 
    Details
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/ja01022a047
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    Paper (German National Licenses)
    Fulltext
  • 9
    Electronic Resource
    Electronic Resource
    HLA class II haplotype and sequence analysis support a role for DQ in narcolepsy (1997)
    Springer
    Immunogenetics 46 (1997), S. 410-417 
    Details
    ISSN: 1432-1211
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Notes: Abstract  A systematic haplotype and sequencing analysis of the HLA-DR and -DQ region in patients with narcolepsy was performed. Five new (CA)n microsatellite markers were generated and positioned on the physical map across the HLA-DQB1-DQA1-DRB1 interval. Haplotypes for these new markers and the three HLA loci were established using somatic cell hybrids generated from patients. A four-marker haplotype surrounding the DQB1 * 0602 gene was found in all narcolepsy patients, and was identical to haplotypes observed on random chromosomes harboring the DQB1 * 0602 allele. Eighty-six kilobases of contiguous genomic sequence across the region did not reveal new genes, and analysis of this sequence for single nucleotide polymorphisms did not reveal sequence variation among DQB1 * 0602 chromosomes. These results are consistent with other studies, suggesting that the HLA-DQ genes themselves are among the predisposing factors in narcolepsy.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s002510050295
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  • 10
    Electronic Resource
    Electronic Resource
    Modeling of Dry Sliding Wear Using a Systematic Approach (2006)
    s.l. ; Stafa-Zurich, Switzerland
    Key engineering materials Vol. 324-325 (Nov. 2006), p. 967-970 
    Details
    ISSN: 1013-9826
    Source: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Virtual life testing is becoming a widely accepted methodology for predicting the lifespan of products. In this method, reliable models are important to predict different aspects of designperformance, one of which is wear. Wear and has been a subject of numerous scientific andempirical investigations. Due to the complex and dynamic nature of the phenomena, there is nogeneral wear model, which can be adopted for all wear problems. A systematic approach to themodelling of dry sliding wear using analytical time domain models is presented in this paper. Giventhe sliding distance, the model is capable of predicting wear status in transient (running-in) andsteady-state operating conditions. The validity of the modelling approach is demonstrated bycomparing the predicted results of wear experiments, with that actually measured. For simplicity,the model is based on sliding distance as input variable, while other factors like temperature, load,surface conditions are treated as constant. A simple geometry of sliding polymer-based contacts isused for establishing of wear model
    Type of Medium: Electronic Resource
    URL: http://www.tib-hannover.de/fulltexts/2011/0528/01/52/transtech_doi~10.4028%252Fwww.scientific.net%252FKEM.324-325.967.pdf
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