THE PIONEERING CONTRIBUTIONS AND LEGACY OF WALDO H. ZAGWIJN (1928-2018)
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Authors
Gibbard, PL
Suc, Jean-Pierre
Popescu, Speranta Maria
Bertini, Adele
Head, Martin
Diniz, Filomena
Journal Title
Alpine and Mediterranean Quaternary
ISSN
2279-7327
Publisher
AIQUA - Associazione Italiana per lo Studio del Quaternario
Volume
31
Issue
1
Pages
iii-viii
Type
Article
This Version
AM
Metadata
Show full item recordCitation
Gibbard, P., Suc, J., Popescu, S. M., Bertini, A., Head, M., & Diniz, F. THE PIONEERING CONTRIBUTIONS AND LEGACY OF WALDO H. ZAGWIJN (1928-2018). Alpine and Mediterranean Quaternary, 31 (1), iii-viii. https://doi.org/10.26382/AMQ.2018.16
Abstract
Professor Dr. Waldo H. Zagwijn passed away on 26 June, 2018, in his ninetieth year. His thesis research (Zagwijn, 1960) stimulated palynological investigations into the Pliocene and early Quaternary, and caused a fundamental shift in our under-standing of the transition from the warm and relatively stable climate of the late Neogene to the extreme glacial-interglacial oscilla-tions of the early Quaternary. Distinct in several aspects from the usual methodologies of that time, Zagwijn’s approach can be summarized as:
focusing on establishing the botanical identification of pollen grains, following the guiding approach of his supervisor F. Flor-schütz, using botanical nomenclature to highlight these identifications and clarifying relationships between botany and the ear-lier artificial pollen nomenclature;
comprehensive and continuous attention to plant macroremains (fruits, seeds, etc.; Zagwijn, 1990) as a mean of integrating classical palaeobotany with modern palynology;
palaeoenvironmental interpretations informed by a deep understanding of modern plant ecology and associations;
leading investigations in the field, and paying special attention to stratigraphic correlations between (onshore and offshore) boreholes and exposed sections in quarries, using a range of available proxies including heavy mineral analysis.
Waldo H. Zagwijn was a visionary in realizing how modern palynology can be used for vegetational and climatic reconstructions in the Neogene, and indeed as far back as Paleogene times.
Keywords
Pollen analysis, Palaeovegetation, Climatostratigraphy, Pliocene-Pleistocene boundary, Glacials-Interglacials
Identifiers
External DOI: https://doi.org/10.26382/AMQ.2018.16
This record's URL: https://www.repository.cam.ac.uk/handle/1810/288342
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