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    <subfield code="a">10.1017/qua.2022.68</subfield>
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    <subfield code="a">Turu, V.</subfield>
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    <subfield code="a">Glacial–interglacial cycles in the south-central and southeastern Pyrenees since ~180 ka (NE Spain–Andorra–S France)</subfield>
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    <subfield code="c">2023</subfield>
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    <subfield code="a">This study uses luminescence and 14C accelerator mass spectrometry procedures to date relevant glaciofluvial and glacial deposits from the south-central and southeastern Pyrenees (Andorra–France–Spain). We distinguish two types of end-moraine complexes: (1) those in which at least a far-flung moraine exists beyond a frequently nested end-moraine complex (the most common) and (2) those in which a close-nested end moraine encompasses at least two glacial cycles. Both types formed within six distinctive glacial intervals: (1) A penultimate glacial cycle during Marine Oxygen Isotope Stage (MIS) 6 and older glaciofluvial terraces occurred beyond the range of the luminescence dating method. (2) An early glacial advance in MIS 5d (~97 −15/+19 ka) was followed by glacial retreat during MIS 5c (&lt; 91 ± 9 ka). (3) The last maximum ice extent (LMIE) was in early MIS 4 (~74 ± 4.5 ka). (4) Unexpectedly, glaciers thinned during the second half of MIS 3 (~39 −6/+11 ka). (5) During the MIS 3–2 transition, glaciers subsequently fluctuated behind the LMIE limits. (6) The global last glacial maximum (LGM) started as early as ~26.6 ± 0.365 ka b2k, and the corresponding end moraines were built behind the LMIE limits or merged with it, forming close-nested moraines.</subfield>
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    <subfield code="b">38 / 65 = 0.585</subfield>
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    <subfield code="b">155 / 254 = 0.61</subfield>
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  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Peña-Monné, J. L.</subfield>
    <subfield code="u">Universidad de Zaragoza</subfield>
    <subfield code="0">(orcid)0000-0003-4067-8222</subfield>
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  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Cunha, P. P.</subfield>
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    <subfield code="a">Jalut, G.</subfield>
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    <subfield code="a">Buylaert, J. P.</subfield>
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    <subfield code="a">Murray, A. S.</subfield>
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  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Oliva, M.</subfield>
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    <subfield code="a">Carrasco, R. M.</subfield>
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    <subfield code="a">Ros, X.</subfield>
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    <subfield code="a">Turu-Font, L.</subfield>
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    <subfield code="a">Ventura Roca, J.</subfield>
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    <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="773" ind1=" " ind2=" ">
    <subfield code="g">113 (2023), [28 pp.]</subfield>
    <subfield code="p">Quat. res.</subfield>
    <subfield code="t">Quaternary Research (United States)</subfield>
    <subfield code="x">0033-5894</subfield>
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