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The spread of grass-dominated habitats in Turkey and surrounding areas during the Cenozoic: Phytolith evidence

Strömberg, Caroline A.E., Werdelin, Lars, Friis, Else Marie, Saraç, Gerçek·2007·Palaeogeography, Palaeoclimatology, Palaeoecology
DOI 10.1016/j.palaeo.2007.02.012
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  • Phytoliths are non-organic silica microfossils formed inside many plants that can be preserved on geological timescales, even in settings where organic matter (including pollen) is not preserved.

    “Phytoliths are non-organic silica microfossils formed inside many plants that can be preserved on geological timescales, even in settings where organic matter (including pollen) is not preserved”

    From Phytolith assemblages reflect variability in human land use and the modern environment (2024) · cites this paper as Strömberg et al. 2007

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Metadata

Authors
Strömberg, C. A. E., Werdelin, L., Friis, E. M., & Saraç, G.
Venue
Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher
Elsevier BV
Published
2007-06
Volume
250
Issue
1-4
Pages
18-49
ISSN
0031-0182
DOI
10.1016/j.palaeo.2007.02.012
Cited by
206
References
0
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)

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