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  • Digital Humanities and Cultural Heritage
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  • 15. Life on land
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  • Publikationer från Umeå universitet
  • Digital Humanities and Cultural Heritage

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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Kanbar, Hussein; Kanbar, Hussein Jaafar; Tran Le, Thai; Olajos, Fredrik; +2 Authors

    AbstractPurposeIntact lake sediments reflect the development of terrestrial ecosystems. This development can be understood by decoding mineral and geochemical information of sedimentary archives. Therefore, we characterized a Holocene lake sediment core and revealed bulk to micro-scale variations via a combination of geochemical techniques and statistical methods.MethodsA 2.3 m sediment core was collected from Hotagen, a lake in west-central Sweden; a sediment sample was collected every 5 cm. A part of each sediment sample was kept untreated (named bulk) and another part was size-fractionated into < 4, 4–16, 16–64, and > 64 µm subsamples. Characterization was then made with respect to grain size distribution (GSD), physico-chemical parameters, geochemical properties, organic composition, and mineralogy. The sediments were investigated at bulk, micro-, and elemental scales using powder X-ray diffraction (XRD), diffuse reflectance infrared Fourier transform spectroscopy (DRIFT), and scanning electron microscopy coupled to energy-dispersive X-ray spectroscopy (SEM–EDX).ResultsThe deepest sediment was identified as glacial till dating back to the Late Pleistocene. The bulk sediments showed a clear distinction between 0–195 cm (unit 1, U1) and 200–225 cm (unit 2, U2) depths. Quartz and feldspar minerals decreased and organic matter and clay minerals increased from the till towards the lower limit of U1. The development in the sedimentary properties marked the transformation of the terrestrial ecosystem from glacier-covered land to vegetated areas. This development was also well reflected by the appearance of X-ray amorphous materials and the formation of distinct organo-mineral aggregates; chlorite was the predominant clay mineral in these aggregates. The geochemical variation between U2 and U1 sediments was further established by resolving the DRIFT spectral components through multivariate curve resolution alternating least square (MCR-ALS). The U1 sediments settled over a period of ~ 7500 years and showed comparable mineral, geochemical, and organic composition. However, the size-fractionated sediments, mainly < 4 µm, showed diverse mineral and geochemical composition. Indeed, these sediments were distinct by containing relatively higher amounts of X-ray amorphous materials and clay minerals, the latter had variable Na, Mg, and K contents.ConclusionThe combined use of geochemical and statistical approaches used in this study followed the mineral and geochemical development of sediments that had settled during the Late Pleistocene and Early Holocene Epochs. Finally, the U2 sediments marked the terrestrial ecosystem development that occurred during the late glaciation, deglaciation, and post-glaciation periods.Graphical abstract

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Publikationer från U...arrow_drop_down
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    Journal of Soils and Sediments
    Article . 2021 . Peer-reviewed
    License: CC BY
    Data sources: Crossref
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    Journal of Soils and Sediments
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    License: CC BY
    Data sources: UnpayWall
    Hal-Diderot
    Article . 2021
    Data sources: Hal-Diderot
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Publikationer från U...arrow_drop_down
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      Journal of Soils and Sediments
      Article . 2021 . Peer-reviewed
      License: CC BY
      Data sources: Crossref
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Journal of Soils and Sediments
      Article
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      Hal-Diderot
      Article . 2021
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Kathleen D. Morrison; Emily Hammer; Oliver Boles; Marco Madella; +60 Authors

    In the 12,000 years preceding the Industrial Revolution, human activities led to significant changes in land cover, plant and animal distributions, surface hydrology, and biochemical cycles. Earth system models suggest that this anthropogenic land cover change influenced regional and global climate. However, the representation of past land use in earth system models is currently oversimplified. As a result, there are large uncertainties in the current understanding of the past and current state of the earth system. In order to improve representation of the variety and scale of impacts that past land use had on the earth system, a global effort is underway to aggregate and synthesize archaeological and historical evidence of land use systems. Here we present a simple, hierarchical classification of land use systems designed to be used with archaeological and historical data at a global scale and a schema of codes that identify land use practices common to a range of systems, both implemented in a geospatial database. The classification scheme and database resulted from an extensive process of consultation with researchers worldwide. Our scheme is designed to deliver consistent, empirically robust data for the improvement of land use models, while simultaneously allowing for a comparative, detailed mapping of land use relevant to the needs of historical scholars. To illustrate the benefits of the classification scheme and methods for mapping historical land use, we apply it to Mesopotamia and Arabia at 6 kya (c. 4000 BCE). The scheme will be used to describe land use by the Past Global Changes (PAGES) LandCover6k working group, an international project comprised of archaeologists, historians, geographers, paleoecologists, and modelers. Beyond this, the scheme has a wide utility for creating a common language between research and policy communities, linking archaeologists with climate modelers, biodiversity conservation workers and initiatives. Fil: Morrison, Kathleen D.. University of Pennsylvania; Estados Unidos Fil: Hammer, Emily. University of Pennsylvania; Estados Unidos Fil: Boles, Oliver. University of Pennsylvania; Estados Unidos Fil: Madella, Marco. University of the Witwatersrand; Sudáfrica. Universitat Pompeu Fabra; España Fil: Whitehouse, Nicola. University of Glasgow; Reino Unido Fil: Gaillard, Marie-Jose. Linnaeus University; Suecia Fil: Bates, Jennifer. University of Pennsylvania; Estados Unidos Fil: Linden, Marc Vander. Bournemouth University; Sudáfrica Fil: Merlo, Stefania. University of the Witwatersrand; Sudáfrica Fil: Yao, Alice. University of Chicago; Estados Unidos Fil: Popova, Laura. Arizona State University; Estados Unidos Fil: Hill, Austin Chad. University of Pennsylvania; Estados Unidos Fil: Antolin, Ferran. Universiat Basel; Suiza Fil: Bauer, Andrew. University of Stanford; Estados Unidos Fil: Biagetti, Stefano. University of the Witwatersrand; Sudáfrica. Universitat Pompeu Fabra; España Fil: Bishop, Rosie R.. University of Stavanger; Noruega Fil: Buckland, Phillip. Universidad de Umea; Suecia Fil: Cruz, Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Unidad Ejecutora en Ciencias Sociales Regionales y Humanidades. Universidad Nacional de Jujuy. Unidad Ejecutora en Ciencias Sociales Regionales y Humanidades; Argentina Fil: Dreslerová, Dagmar. Institute Of Archaeology Of The Academy Of Sciences Of The Czech Republic; Hungría Fil: Dusseldorp, Gerrit. Leiden University; Países Bajos Fil: Ellis, Erle C.. University of Maryland; Estados Unidos. University Of Johannesburg; Sudáfrica Fil: Filipovich, Ruben Eduardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina Fil: Foster, Thomas. University of Tulsa; Estados Unidos Fil: Hannaford, Matthew J.. Lincoln University.; Nueva Zelanda Fil: Harrison, Sandy P.. University of Reading; Reino Unido Fil: Hazarika, Manjil. Cotton University; India Fil: Herold, Hajnalka. University of Exeter; Reino Unido Fil: Hilpert, Johanna. Universitat zu Köln; Alemania Fil: Kaplan, Jed O.. The University Of Hong Kong; Hong Kong Fil: Kay, Andrea. Max Planck Institute For The Science Of Human History; Alemania Fil: Goldewijk, Kees Klein. Utrecht University; Países Bajos Fil: Kolár, Jan. Masaryk University; República Checa Fil: Kyazike, Elizabeth. Kyambogo University; Uganda Fil: Laabs, Julian. University of Bern; Suiza Fil: Lancelotti, Carla. Universitat Pompeu Fabra; España Fil: Lane, Paul. University of the Witwatersrand; Sudáfrica. University of Cambridge; Estados Unidos Fil: Lawrence, Dan. University of Durham; Reino Unido Fil: Lewis, Krista. University of Arkansas; Estados Unidos Fil: Lombardo, Umberto. University of Bern; Suiza Fil: Lucarini, Giulio. Consiglio Nazionale delle Ricerche; Italia. University of Naples; Italia Fil: Arroyo Kalin, Manuel. Colegio Universitario de Londres; Reino Unido Fil: Marchant, Rob. University of York; Reino Unido Fil: Mayle, Francis. University of Reading; Reino Unido Fil: McClatchie, Meriel. University College; Irlanda Fil: McLeester, Madeleine. Dartmouth College; Estados Unidos Fil: Mooney, Scott. Unsw Sydney; Australia Fil: Moskal-Del Hoyo, Magdalena. Wladyslaw Szafer Institute Of Botany Of The Polish Academy Of Sciences; Polonia Fil: Navarrete, Vanessa. Universitat Autònoma de Barcelona; España Fil: Ndiema, Emmanuel. National Museums Of Kenya; Kenia Fil: Neves, Eduardo Góes. Universidade de Sao Paulo; Brasil Fil: Nowak, Marek. Jagiellonian University; Polonia Fil: Out, Welmoed A.. Moesgaard Museum; Dinamarca Fil: Petrie, Cameron. Universitat Pompeu Fabra; España. University of Cambridge; Estados Unidos Fil: Phelps, Leanne N.. Royal Botanic Gardens; Reino Unido. University of Edinburgh; Reino Unido Fil: Szakonyi, Zsolt. Eötvös University; Hungría Fil: Rostain, Stéphen. Centre National de la Recherche Scientifique; Francia Fil: Russell, Thembi. University of the Witwatersrand; Sudáfrica Fil: Sluyter, Andrew. Louisiana State University; Estados Unidos Fil: Styring, Amy K.. University of Oxford; Reino Unido Fil: Tamanaha, Eduardo. The Mamirauá Sustainable Development Institute; Brasil Fil: Thomas, Evert. The Alliance of Bioversity International and CIAT; Perú Fil: Veerasamy, Selvakumar. Tamil University; India Fil: Welton, Lynn. University of the Witwatersrand; Sudáfrica Fil: Zanon, Marco. Institute of Pre- and Protohistoric Archaeology; Alemania

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    Europe PubMed Central
    Article . 2021
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    Article . 2021
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    Durham Research Online
    Article . 2021 . Peer-reviewed
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    Apollo
    Article . 2021
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    Article . 2021 . Peer-reviewed
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    https://doi.org/10.5451/unibas...
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    Apollo
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      Europe PubMed Central
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      NARCIS
      Article . 2021
      Data sources: NARCIS
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      Durham Research Online
      Article . 2021 . Peer-reviewed
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      UiS Brage
      Article . 2021
      Data sources: UiS Brage
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      Apollo
      Article . 2021
      License: CC BY
      Data sources: Datacite
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      edoc
      Article . 2021 . Peer-reviewed
      Data sources: edoc
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      PLoS ONE
      Article . 2021
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      Oxford University Research Archive
      Other literature type . 2022
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      MPG.PuRe
      Article . 2021
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      UPF Digital Repository
      Article . 2021
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      PLoS ONE
      Article
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      Apollo
      Other literature type . 2021
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      OPUS Augsburg
      Article . 2021
      License: CC BY
      Data sources: OPUS Augsburg
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      Apollo
      Other literature type . 2021
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      https://doi.org/10.5451/unibas...
      Other literature type . 2021
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      Apollo
      Article . 2021
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    Authors: Pálsson, Gísli;

    Domination, Subsistence, and Interdependence : Tracing Resource Claim Networks across Iceland's Post-Reformation Landscape

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    Human Ecology
    Article
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    Human Ecology
    Article . 2019 . Peer-reviewed
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      Human Ecology
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      Human Ecology
      Article . 2019 . Peer-reviewed
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    Authors: Pearce, Danni M.; Mair, Douglas W. F.; Rea, Brice R.; Lea, James M.; +3 Authors

    The Greenland Ice Sheet (GrIS) is known to have experienced widespread retreat over the last century. Information on outlet glacier dynamics, prior to this, are limited due to both a lack of observations and a paucity of mapped or mappable deglacial evidence which restricts our understanding of centennial to millennial timescale dynamics of the GrIS. Here we present glacial geomorphological mapping, for upper Godthåbsfjord, covering 5800 km2 at a scale of 1:92,000, using a combination of ASTER GDEM V2, a medium-resolution DEM (error <10 m horizontal and <6 m vertical accuracy), panchromatic orthophotographs and ground truthing. This work provides a detailed geomorphological assessment for the area, compiled as a single map, comprising of moraines, meltwater channels, streamlined bedrock, sediment lineations, ice-dammed lakes, trimlines, terraces, gullied sediment and marine limits. Whilst some of the landforms have been previously identified, the new information presented here improves our understanding of ice margin behaviour and can be used for future numerical modelling and landform dating programmes. Data also form the basis for palaeoglaciological reconstructions and contribute towards understanding of the centennial to millennial timescale record of this sector of the GrIS.

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    CORE (RIOXX-UK Aggregator)
    Article . 2018
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    Journal of Maps
    Article . 2018 . Peer-reviewed
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    Journal of Maps
    Article
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    Other literature type . 2018
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    Data sources: Datacite
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Other literature type . 2018
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    Journal of Maps
    Article . 2018
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      CORE (RIOXX-UK Aggregator)
      Article . 2018
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      Journal of Maps
      Article . 2018 . Peer-reviewed
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      Journal of Maps
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      Other literature type . 2018
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      figshare
      Other literature type . 2018
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      Data sources: Datacite
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      Journal of Maps
      Article . 2018
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    Authors: Chapligin, B; Meyer, H; Swann, GEA; Meyer-Jacob, Carsten; +1 Authors

    In 2003 sediment core Lz1024 was drilled at Lake El'gygytgyn, far east Russian Arctic, in an area of the Northern Hemisphere which has not been glaciated for the last 3.6 Ma. Biogenic silica was used for analysing the oxygen isotope composition (&delta;<sup>18</sup>O<sub>diatom</sub>) in the upper 13 m long section dating back about 250 ka with samples dominated by one taxa in the <10 &mu;m fraction (<i>Cyclotella ocellata</i>). Downcore variations in &delta;<sup>18</sup>O values show that glacial-interglacial cycles are present throughout the core and &delta;<sup>18</sup>O<sub>diatom</sub>-values are mainly controlled by &delta;<sup>18</sup>O<sub>precipitation</sub>. Changes reflect the Holocene Thermal Maximum, the Last Glacial Maximum (LGM) and the interglacial periods corresponding to MIS 5.5 and MIS 7 with a peak-to-peak amplitude between LGM and MIS 5.5 of &Delta;<sup>18</sup>O = 5.3&permil;. This corresponds to a mean annual air temperature difference of about 9 °C. Our record is the first continuous &delta;<sup>18</sup>O<sub>diatom</sub> record from an Arctic lake sediment core directly responding to precipitation and dating back more than 250 ka and correlates well with the stacked marine &delta;<sup>18</sup>O LR04 (<i>r</i> = 0.58) and &delta;D EPICA Dome-C record (<i>r</i> = 0.69). With &delta;<sup>18</sup>O results indicating strong links to both marine and ice-core records, records from Lake El'gygytgyn can be used to further investigate the sensitivity of the Arctic climate to both past and future global climatic changes.

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    Climate of the Past
    Article . 2012
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    https://doi.org/10.5194/cpd-8-...
    Preprint . 2012
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    Climate of the Past (CP)
    Article . Preprint
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    Climate of the Past (CP)
    Article . 2012 . Peer-reviewed
    License: CC BY
    Data sources: Crossref
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Publikationer från U...arrow_drop_down
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Climate of the Past
      Article . 2012
      Data sources: DOAJ-Articles
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      https://doi.org/10.5194/cpd-8-...
      Preprint . 2012
      License: CC BY
      Data sources: Crossref
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Climate of the Past (CP)
      Article . Preprint
      License: CC BY
      Data sources: UnpayWall
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Climate of the Past (CP)
      Article . 2012 . Peer-reviewed
      License: CC BY
      Data sources: Crossref
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5 Research products
  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Kanbar, Hussein; Kanbar, Hussein Jaafar; Tran Le, Thai; Olajos, Fredrik; +2 Authors

    AbstractPurposeIntact lake sediments reflect the development of terrestrial ecosystems. This development can be understood by decoding mineral and geochemical information of sedimentary archives. Therefore, we characterized a Holocene lake sediment core and revealed bulk to micro-scale variations via a combination of geochemical techniques and statistical methods.MethodsA 2.3 m sediment core was collected from Hotagen, a lake in west-central Sweden; a sediment sample was collected every 5 cm. A part of each sediment sample was kept untreated (named bulk) and another part was size-fractionated into < 4, 4–16, 16–64, and > 64 µm subsamples. Characterization was then made with respect to grain size distribution (GSD), physico-chemical parameters, geochemical properties, organic composition, and mineralogy. The sediments were investigated at bulk, micro-, and elemental scales using powder X-ray diffraction (XRD), diffuse reflectance infrared Fourier transform spectroscopy (DRIFT), and scanning electron microscopy coupled to energy-dispersive X-ray spectroscopy (SEM–EDX).ResultsThe deepest sediment was identified as glacial till dating back to the Late Pleistocene. The bulk sediments showed a clear distinction between 0–195 cm (unit 1, U1) and 200–225 cm (unit 2, U2) depths. Quartz and feldspar minerals decreased and organic matter and clay minerals increased from the till towards the lower limit of U1. The development in the sedimentary properties marked the transformation of the terrestrial ecosystem from glacier-covered land to vegetated areas. This development was also well reflected by the appearance of X-ray amorphous materials and the formation of distinct organo-mineral aggregates; chlorite was the predominant clay mineral in these aggregates. The geochemical variation between U2 and U1 sediments was further established by resolving the DRIFT spectral components through multivariate curve resolution alternating least square (MCR-ALS). The U1 sediments settled over a period of ~ 7500 years and showed comparable mineral, geochemical, and organic composition. However, the size-fractionated sediments, mainly < 4 µm, showed diverse mineral and geochemical composition. Indeed, these sediments were distinct by containing relatively higher amounts of X-ray amorphous materials and clay minerals, the latter had variable Na, Mg, and K contents.ConclusionThe combined use of geochemical and statistical approaches used in this study followed the mineral and geochemical development of sediments that had settled during the Late Pleistocene and Early Holocene Epochs. Finally, the U2 sediments marked the terrestrial ecosystem development that occurred during the late glaciation, deglaciation, and post-glaciation periods.Graphical abstract

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Publikationer från U...arrow_drop_down
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Journal of Soils and Sediments
    Article . 2021 . Peer-reviewed
    License: CC BY
    Data sources: Crossref
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Journal of Soils and Sediments
    Article
    License: CC BY
    Data sources: UnpayWall
    Hal-Diderot
    Article . 2021
    Data sources: Hal-Diderot
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Publikationer från U...arrow_drop_down
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Journal of Soils and Sediments
      Article . 2021 . Peer-reviewed
      License: CC BY
      Data sources: Crossref
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Journal of Soils and Sediments
      Article
      License: CC BY
      Data sources: UnpayWall
      Hal-Diderot
      Article . 2021
      Data sources: Hal-Diderot
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Kathleen D. Morrison; Emily Hammer; Oliver Boles; Marco Madella; +60 Authors

    In the 12,000 years preceding the Industrial Revolution, human activities led to significant changes in land cover, plant and animal distributions, surface hydrology, and biochemical cycles. Earth system models suggest that this anthropogenic land cover change influenced regional and global climate. However, the representation of past land use in earth system models is currently oversimplified. As a result, there are large uncertainties in the current understanding of the past and current state of the earth system. In order to improve representation of the variety and scale of impacts that past land use had on the earth system, a global effort is underway to aggregate and synthesize archaeological and historical evidence of land use systems. Here we present a simple, hierarchical classification of land use systems designed to be used with archaeological and historical data at a global scale and a schema of codes that identify land use practices common to a range of systems, both implemented in a geospatial database. The classification scheme and database resulted from an extensive process of consultation with researchers worldwide. Our scheme is designed to deliver consistent, empirically robust data for the improvement of land use models, while simultaneously allowing for a comparative, detailed mapping of land use relevant to the needs of historical scholars. To illustrate the benefits of the classification scheme and methods for mapping historical land use, we apply it to Mesopotamia and Arabia at 6 kya (c. 4000 BCE). The scheme will be used to describe land use by the Past Global Changes (PAGES) LandCover6k working group, an international project comprised of archaeologists, historians, geographers, paleoecologists, and modelers. Beyond this, the scheme has a wide utility for creating a common language between research and policy communities, linking archaeologists with climate modelers, biodiversity conservation workers and initiatives. Fil: Morrison, Kathleen D.. University of Pennsylvania; Estados Unidos Fil: Hammer, Emily. University of Pennsylvania; Estados Unidos Fil: Boles, Oliver. University of Pennsylvania; Estados Unidos Fil: Madella, Marco. University of the Witwatersrand; Sudáfrica. Universitat Pompeu Fabra; España Fil: Whitehouse, Nicola. University of Glasgow; Reino Unido Fil: Gaillard, Marie-Jose. Linnaeus University; Suecia Fil: Bates, Jennifer. University of Pennsylvania; Estados Unidos Fil: Linden, Marc Vander. Bournemouth University; Sudáfrica Fil: Merlo, Stefania. University of the Witwatersrand; Sudáfrica Fil: Yao, Alice. University of Chicago; Estados Unidos Fil: Popova, Laura. Arizona State University; Estados Unidos Fil: Hill, Austin Chad. University of Pennsylvania; Estados Unidos Fil: Antolin, Ferran. Universiat Basel; Suiza Fil: Bauer, Andrew. University of Stanford; Estados Unidos Fil: Biagetti, Stefano. University of the Witwatersrand; Sudáfrica. Universitat Pompeu Fabra; España Fil: Bishop, Rosie R.. University of Stavanger; Noruega Fil: Buckland, Phillip. Universidad de Umea; Suecia Fil: Cruz, Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Unidad Ejecutora en Ciencias Sociales Regionales y Humanidades. Universidad Nacional de Jujuy. Unidad Ejecutora en Ciencias Sociales Regionales y Humanidades; Argentina Fil: Dreslerová, Dagmar. Institute Of Archaeology Of The Academy Of Sciences Of The Czech Republic; Hungría Fil: Dusseldorp, Gerrit. Leiden University; Países Bajos Fil: Ellis, Erle C.. University of Maryland; Estados Unidos. University Of Johannesburg; Sudáfrica Fil: Filipovich, Ruben Eduardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina Fil: Foster, Thomas. University of Tulsa; Estados Unidos Fil: Hannaford, Matthew J.. Lincoln University.; Nueva Zelanda Fil: Harrison, Sandy P.. University of Reading; Reino Unido Fil: Hazarika, Manjil. Cotton University; India Fil: Herold, Hajnalka. University of Exeter; Reino Unido Fil: Hilpert, Johanna. Universitat zu Köln; Alemania Fil: Kaplan, Jed O.. The University Of Hong Kong; Hong Kong Fil: Kay, Andrea. Max Planck Institute For The Science Of Human History; Alemania Fil: Goldewijk, Kees Klein. Utrecht University; Países Bajos Fil: Kolár, Jan. Masaryk University; República Checa Fil: Kyazike, Elizabeth. Kyambogo University; Uganda Fil: Laabs, Julian. University of Bern; Suiza Fil: Lancelotti, Carla. Universitat Pompeu Fabra; España Fil: Lane, Paul. University of the Witwatersrand; Sudáfrica. University of Cambridge; Estados Unidos Fil: Lawrence, Dan. University of Durham; Reino Unido Fil: Lewis, Krista. University of Arkansas; Estados Unidos Fil: Lombardo, Umberto. University of Bern; Suiza Fil: Lucarini, Giulio. Consiglio Nazionale delle Ricerche; Italia. University of Naples; Italia Fil: Arroyo Kalin, Manuel. Colegio Universitario de Londres; Reino Unido Fil: Marchant, Rob. University of York; Reino Unido Fil: Mayle, Francis. University of Reading; Reino Unido Fil: McClatchie, Meriel. University College; Irlanda Fil: McLeester, Madeleine. Dartmouth College; Estados Unidos Fil: Mooney, Scott. Unsw Sydney; Australia Fil: Moskal-Del Hoyo, Magdalena. Wladyslaw Szafer Institute Of Botany Of The Polish Academy Of Sciences; Polonia Fil: Navarrete, Vanessa. Universitat Autònoma de Barcelona; España Fil: Ndiema, Emmanuel. National Museums Of Kenya; Kenia Fil: Neves, Eduardo Góes. Universidade de Sao Paulo; Brasil Fil: Nowak, Marek. Jagiellonian University; Polonia Fil: Out, Welmoed A.. Moesgaard Museum; Dinamarca Fil: Petrie, Cameron. Universitat Pompeu Fabra; España. University of Cambridge; Estados Unidos Fil: Phelps, Leanne N.. Royal Botanic Gardens; Reino Unido. University of Edinburgh; Reino Unido Fil: Szakonyi, Zsolt. Eötvös University; Hungría Fil: Rostain, Stéphen. Centre National de la Recherche Scientifique; Francia Fil: Russell, Thembi. University of the Witwatersrand; Sudáfrica Fil: Sluyter, Andrew. Louisiana State University; Estados Unidos Fil: Styring, Amy K.. University of Oxford; Reino Unido Fil: Tamanaha, Eduardo. The Mamirauá Sustainable Development Institute; Brasil Fil: Thomas, Evert. The Alliance of Bioversity International and CIAT; Perú Fil: Veerasamy, Selvakumar. Tamil University; India Fil: Welton, Lynn. University of the Witwatersrand; Sudáfrica Fil: Zanon, Marco. Institute of Pre- and Protohistoric Archaeology; Alemania

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    CORE (RIOXX-UK Aggregator)
    Article . 2021
    License: CC BY
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    Europe PubMed Central
    Article . 2021
    Data sources: PubMed Central
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    NARCIS
    Article . 2021
    Data sources: NARCIS
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    CORE (RIOXX-UK Aggregator)
    Article . 2021
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    NARCIS
    Article . 2021
    Data sources: NARCIS
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    Durham Research Online
    Article . 2021 . Peer-reviewed
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    UiS Brage
    Article . 2021
    Data sources: UiS Brage
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    Apollo
    Article . 2021
    License: CC BY
    Data sources: Datacite
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    edoc
    Article . 2021 . Peer-reviewed
    Data sources: edoc
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    PLoS ONE
    Article . 2021
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    Oxford University Research Archive
    Other literature type . 2022
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    MPG.PuRe
    Article . 2021
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    Data sources: MPG.PuRe
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    UPF Digital Repository
    Article . 2021
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    PLoS ONE
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    Apollo
    Other literature type . 2021
    Data sources: Apollo
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    OPUS Augsburg
    Article . 2021
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    Apollo
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    https://doi.org/10.5451/unibas...
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      Europe PubMed Central
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      Durham Research Online
      Article . 2021 . Peer-reviewed
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      UiS Brage
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      Apollo
      Article . 2021
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      edoc
      Article . 2021 . Peer-reviewed
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      PLoS ONE
      Article . 2021
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      Oxford University Research Archive
      Other literature type . 2022
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      Apollo
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      Apollo
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      image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
      https://doi.org/10.5451/unibas...
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      Article . 2021
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Pálsson, Gísli;

    Domination, Subsistence, and Interdependence : Tracing Resource Claim Networks across Iceland's Post-Reformation Landscape

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    Human Ecology
    Article
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    Human Ecology
    Article . 2019 . Peer-reviewed
    License: CC BY
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      Human Ecology
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      Human Ecology
      Article . 2019 . Peer-reviewed
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    Authors: Pearce, Danni M.; Mair, Douglas W. F.; Rea, Brice R.; Lea, James M.; +3 Authors

    The Greenland Ice Sheet (GrIS) is known to have experienced widespread retreat over the last century. Information on outlet glacier dynamics, prior to this, are limited due to both a lack of observations and a paucity of mapped or mappable deglacial evidence which restricts our understanding of centennial to millennial timescale dynamics of the GrIS. Here we present glacial geomorphological mapping, for upper Godthåbsfjord, covering 5800 km2 at a scale of 1:92,000, using a combination of ASTER GDEM V2, a medium-resolution DEM (error <10 m horizontal and <6 m vertical accuracy), panchromatic orthophotographs and ground truthing. This work provides a detailed geomorphological assessment for the area, compiled as a single map, comprising of moraines, meltwater channels, streamlined bedrock, sediment lineations, ice-dammed lakes, trimlines, terraces, gullied sediment and marine limits. Whilst some of the landforms have been previously identified, the new information presented here improves our understanding of ice margin behaviour and can be used for future numerical modelling and landform dating programmes. Data also form the basis for palaeoglaciological reconstructions and contribute towards understanding of the centennial to millennial timescale record of this sector of the GrIS.

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    Article . 2018
    License: CC BY
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    Journal of Maps
    Article . 2018 . Peer-reviewed
    Data sources: Crossref
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    Journal of Maps
    Article
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    Other literature type . 2018
    License: CC BY
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