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1 - 4 of 4 search results for KA :PC53 24 |u:www.inqua-seqs.org where 0 match all words and 4 match some words.

  1. Results that match 2 of 3 words

  2. 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.

  3. 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.

  4. 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.

  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.

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