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1 - 10 of 13 search results for KA :PC53 24 |u:www.inqua-seqs.org where 0 match all words and 13 match some words.
  1. Results that match 2 of 3 words

  2. 21 Dec 2016: Hrazdan valley is thought to have been active around 700 ka and produced obsidian outcrops close. ... landscapes. Subsequent downcutting since 193 ka has exposed the sedimentary stack in the valley.
  3. Conference abstracts_1

    https://www.inqua-seqs.org/wp-content/uploads/SEQS2008AbstractsRennes.pdf
    31 Oct 2011: environmental variability during the Late Quaternary (10 – 30 cal ka), we studied fluvial archives of. ... ka BP (Oldest Dryas, H1 event), solid and liquid discharges decrease whereas aeolian processes.
  4. GeoEcoMar – Bucharest, 2013 INQUA – Section on European ...

    https://www.inqua-seqs.org/files/Book_of_Abstracts.pdf
    7 Oct 2013: Palaeoclimate and palaeoenvironmental responses in the western Mediterranean over the last 140 ka: evidence from Mallorca, Spain. ... Coarse quartz in samples collected from the L1 yielded ages of 11 ka to 53 ka.
  5. Volume of abstracts

    https://www.inqua-seqs.org/wp-content/uploads/SEQS2002AbstractsUfa.pdf
    31 Oct 2011: 24. Erbajeva Margarita, Alexeeva Nadezhda, Khenzykhenova Fedora and Yazykov Alexander. Biostratigraphy of the South-Eastern Siberia. ... data. The most known of them is the problem of the 100-ka Pleistocene climatic periodicity.
  6. INQUA SEQS 2021 Conference Proceedings Wrocław, Poland, 13th December …

    https://www.inqua-seqs.org/files/SEQS2021_Abstracts_Wroclaw_Poland.pdf
    15 Dec 2021: biological adaptations to the tundra-steppe and forest-tundra habitats. The climatically mild mid-Last Glacial interstadial (60/55–24 ka BP) is considered to be the. ... end of the mid-last glacial (30–24 ka BP) within the mammoth steppe (Ukraintseva,
  7. ISBN-13: 978-84-692-5903-0 DEPÓSITO LEGAL: GR 2957-2009 2009 SEQS…

    https://www.inqua-seqs.org/wp-content/uploads/SEQS2009AbstractsOrce.pdf
    31 Oct 2011: 10-100 ka climatic shifts throughout the Earth's history would have caused the. ... Their. formation ranges between 120 and 18 Ka. They consequently span between OIS 5c-d.
  8. Foreword

    https://www.inqua-seqs.org/files/SEQS2006_Abstracts_Milano.pdf
    20 Jun 2017: Quaternary Science Reviews, 24: 1861-1872. Graf H.R. (1993) - Die Deckenschotter der zentralen Nordschweiz. ... A combination of 10Be and paleomagnetic measurement suggests ages < 62ka, 450-980 ka and app.
  9. INQUA SEQS International Union for Quaternary Research (INQUA)Section …

    https://www.inqua-seqs.org/wp-content/uploads/SEQS2010absractsrostov.pdf
    31 Oct 2011: MammaliaInsectivora. 3 Blarinoides sp. 24 cf. Drepanosorex sp. 15 Talpa minor 9.
  10. Po sto jna , 20 18 IN QU A ...

    https://www.inqua-seqs.org/files/SEQS2018_Abstracts_Guide_Postojna_Slovenia.pdf
    31 Oct 2018: The U-series dating and age-depth modeling allowed to determine the time of growth of the stalagmite between 323 and 232 ka, during the MIS 9 - MIS 7 (Marine Isotope ... Stage) and also allowed to distinguish two breaks in the deposition of the
  11. Quaternary Stratigraphy – palaeoenvironment, sediments, palaeofauna…

    https://www.inqua-seqs.org/files/SEQS2020_Abstracts_Wroclaw_Poland.pdf
    26 Sep 2020: Quaternary Stratigraphy – palaeoenvironment, sediments, palaeofauna and human migrations across Central Europe. Edited by. Artur SobczykUrszula Ratajczak-SkrzatekMarek KasprzakAdam KotowskiAdrian MarciszakKrzysztof Stefaniak. INQUA SEQS

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