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    <subfield code="2">doi</subfield>
    <subfield code="a">10.1007/s12665-022-10547-x</subfield>
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    <subfield code="2">sideral</subfield>
    <subfield code="a">130165</subfield>
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    <subfield code="a">ART-2022-130165</subfield>
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  <datafield tag="041" ind1=" " ind2=" ">
    <subfield code="a">eng</subfield>
  </datafield>
  <datafield tag="100" ind1=" " ind2=" ">
    <subfield code="a">Peña Monné, José Luis</subfield>
    <subfield code="u">Universidad de Zaragoza</subfield>
    <subfield code="0">(orcid)0000-0003-4067-8222</subfield>
  </datafield>
  <datafield tag="245" ind1=" " ind2=" ">
    <subfield code="a">Late Quaternary palaeoenvironmental controls on concentric talus evolution in the Central Ebro Basin (NE Spain)</subfield>
  </datafield>
  <datafield tag="260" ind1=" " ind2=" ">
    <subfield code="c">2022</subfield>
  </datafield>
  <datafield tag="506" ind1="0" ind2=" ">
    <subfield code="a">Access copy available to the general public</subfield>
    <subfield code="f">Unrestricted</subfield>
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  <datafield tag="520" ind1="3" ind2=" ">
    <subfield code="a">The polyphasic evolution of the testimonial buttes in the central area of the Ebro basin (Los Monegros) is analysed. This is a semiarid area that favours high erosion rates. An evolutionary model of the Jubierre hills is presented that shows the environmental cycles represented by aggradational and degradative processes on the slopes that resulted in the present arrangement of talus flatiron rings. In the four studied cases, talus relicts are composed of detritic material from a disappeared caprock pediment. Four slope stages (S4 to S1) that formed under stable climate conditions are identified. Older stages (S4 and S3) are estimated by comparison with other talus flatirons in the region. The S2 stage contains Bronze Age archaeological remains and the radiocarbon age obtained was 1608-1446 years cal BC (2 sigma), while S1 is younger. A palaeoenvironmental interpretation was made for these aggradational stages (S4 to S1). The active erosion of these hills led to a relief inversion, and talus flatirons remain as the only features revealing the presence of the relict hills and past human occupations.</subfield>
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    <subfield code="9">info:eu-repo/grantAgreement/ES/MINECO/HAR2014-59042-P</subfield>
    <subfield code="9">info:eu-repo/grantAgreement/ES/MINECO/HAR2015-65620-P</subfield>
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    <subfield code="9">info:eu-repo/semantics/openAccess</subfield>
    <subfield code="a">by</subfield>
    <subfield code="u">http://creativecommons.org/licenses/by/3.0/es/</subfield>
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    <subfield code="a">2.8</subfield>
    <subfield code="b">2022</subfield>
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    <subfield code="a">GEOSCIENCES, MULTIDISCIPLINARY</subfield>
    <subfield code="b">95 / 202 = 0.47</subfield>
    <subfield code="c">2022</subfield>
    <subfield code="d">Q2</subfield>
    <subfield code="e">T2</subfield>
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  <datafield tag="591" ind1=" " ind2=" ">
    <subfield code="a">WATER RESOURCES</subfield>
    <subfield code="b">45 / 103 = 0.437</subfield>
    <subfield code="c">2022</subfield>
    <subfield code="d">Q2</subfield>
    <subfield code="e">T2</subfield>
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  <datafield tag="591" ind1=" " ind2=" ">
    <subfield code="a">ENVIRONMENTAL SCIENCES</subfield>
    <subfield code="b">162 / 275 = 0.589</subfield>
    <subfield code="c">2022</subfield>
    <subfield code="d">Q3</subfield>
    <subfield code="e">T2</subfield>
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  <datafield tag="592" ind1=" " ind2=" ">
    <subfield code="a">0.599</subfield>
    <subfield code="b">2022</subfield>
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  <datafield tag="593" ind1=" " ind2=" ">
    <subfield code="a">Soil Science</subfield>
    <subfield code="c">2022</subfield>
    <subfield code="d">Q2</subfield>
  </datafield>
  <datafield tag="593" ind1=" " ind2=" ">
    <subfield code="a">Earth-Surface Processes</subfield>
    <subfield code="c">2022</subfield>
    <subfield code="d">Q2</subfield>
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  <datafield tag="593" ind1=" " ind2=" ">
    <subfield code="a">Geology</subfield>
    <subfield code="c">2022</subfield>
    <subfield code="d">Q2</subfield>
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  <datafield tag="593" ind1=" " ind2=" ">
    <subfield code="a">Water Science and Technology</subfield>
    <subfield code="c">2022</subfield>
    <subfield code="d">Q2</subfield>
  </datafield>
  <datafield tag="593" ind1=" " ind2=" ">
    <subfield code="a">Pollution</subfield>
    <subfield code="c">2022</subfield>
    <subfield code="d">Q2</subfield>
  </datafield>
  <datafield tag="593" ind1=" " ind2=" ">
    <subfield code="a">Environmental Chemistry</subfield>
    <subfield code="c">2022</subfield>
    <subfield code="d">Q3</subfield>
  </datafield>
  <datafield tag="593" ind1=" " ind2=" ">
    <subfield code="a">Global and Planetary Change</subfield>
    <subfield code="c">2022</subfield>
    <subfield code="d">Q3</subfield>
  </datafield>
  <datafield tag="594" ind1=" " ind2=" ">
    <subfield code="a">5.2</subfield>
    <subfield code="b">2022</subfield>
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    <subfield code="a">info:eu-repo/semantics/article</subfield>
    <subfield code="v">info:eu-repo/semantics/publishedVersion</subfield>
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  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Sampietro Vattuone, María Marta</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Picazo Millán, Jesús, V.</subfield>
    <subfield code="u">Universidad de Zaragoza</subfield>
    <subfield code="0">(orcid)0000-0002-4726-819X</subfield>
  </datafield>
  <datafield tag="710" ind1="2" ind2=" ">
    <subfield code="1">3006</subfield>
    <subfield code="2">430</subfield>
    <subfield code="a">Universidad de Zaragoza</subfield>
    <subfield code="b">Dpto. Geograf. Ordenac.Territ.</subfield>
    <subfield code="c">Área Geografía Física</subfield>
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  <datafield tag="710" ind1="2" ind2=" ">
    <subfield code="1">3000</subfield>
    <subfield code="2">695</subfield>
    <subfield code="a">Universidad de Zaragoza</subfield>
    <subfield code="b">Dpto. Ciencias de la Antigüed.</subfield>
    <subfield code="c">Área Prehistoria</subfield>
  </datafield>
  <datafield tag="773" ind1=" " ind2=" ">
    <subfield code="g">81, 422 (2022), 19</subfield>
    <subfield code="p">Environ. earth sci.</subfield>
    <subfield code="t">Environmental Earth Sciences</subfield>
    <subfield code="x">1866-6280</subfield>
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  <datafield tag="856" ind1="4" ind2=" ">
    <subfield code="s">15498261</subfield>
    <subfield code="u">http://zaguan.unizar.es/record/118979/files/texto_completo.pdf</subfield>
    <subfield code="y">Versión publicada</subfield>
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    <subfield code="u">http://zaguan.unizar.es/record/118979/files/texto_completo.jpg?subformat=icon</subfield>
    <subfield code="x">icon</subfield>
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