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Phytoliths in Paleoecology: Analytical Considerations, Current Use, and Future Directions
Abstract
Phytoliths, microscopic plant silicaPhytoliths silica/silicon bodies, are often preserved in modern and fossil soils and sediment, as well as in archaeological contexts. They record unique characteristics of past vegetation and, unlike palynomorphs and macrofossils, are commonly found in direct association with fossil vertebrates, providing vital paleoecological data. Within pre-Quaternary paleoecologyPaleoecology , phytolith analysis has so far elucidated Cretaceous-Cenozoic grass evolution, vegetation change including the spread of grasslands, plant-animal co-evolution, and dietsDiet of extinct animals. Because deep-time phytolith analysis is a young field, many methodological aspects are not standardized, preventing comparisons among studies and calibration using published modern analogs. On the other hand, the plethora of novel approaches in recent literature points to the potential of phytolith-based paleoecology. Here, we review the present state of phytolith analysis, focusing on pre-Quaternary applications. We discuss the nature and known biases of the phytolith record, current methods, and examples of when phytoliths contributed substantially to knowledge of past ecosystems, and highlight important future avenues of research.
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The sampled terraces have been utilized for agricultural activities over an extended period.
“Consequently, it can be inferred that the sampled terraces have been utilized for agricultural activities over an extended period, as the highest phytolith concentrations in natural soils typically occur in the upper humic horizon and decrease with depth (Qader et al., 2023; Strömberg et al., 2018).”
From The impact of agriculture on tropical mountain soils in the western peruvian andes: a pedo-geoarchaeological study of terrace agricultural systems in the laramate region (14.5° S) (2024) · cites this paper as Strömberg et al., 2018
The Pe11-07 terrace might not have been used extensively for agriculture over an extended period.
“This mirrors the soil control profile Pe10-32 (Fig. 15), devoid of terracing and likely agriculture, suggesting that the Pe11-07 terrace might not have been used extensively for agriculture over an extended period (Qader et al., 2023; Strömberg et al., 2018).”
From The impact of agriculture on tropical mountain soils in the western peruvian andes: a pedo-geoarchaeological study of terrace agricultural systems in the laramate region (14.5° S) (2024) · cites this paper as Strömberg et al., 2018
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Woody cover in African savannas: the role of resources, fire and herbivory.
Sankaran, M., Ratnam, J., & Hanan, N. (2008) · Global Ecology and Biogeography · doi:10.1111/j.1466-8238.2007.00360.x · Cited by 589
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Leceta, F., Binder, C., Mader, C., Mächtle, B., Marsh, E., Dietrich, L., Reindel, M., Eitel, B., & Meister, J. (2024) · Soil · doi:10.5194/soil-10-727-2024 · Cited by 14
Allende, M. K.-G., & Samplonius, A. (2022) · Annals of Anatomy - Anatomischer Anzeiger · doi:10.1016/j.aanat.2021.151849 · Cited by 6
Metadata
- Authors
- Strömberg, C. A. E., Dunn, R. E., Crifò, C., & Harris, E. B.
- Venue
- Vertebrate Paleobiology and Paleoanthropology
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- Springer International Publishing
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- 2018
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- 235-287
- ISSN
- 1877-9077
- 1877-9085
- Cited by
- 94
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- Language
- en
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- www.springer.com/tdm (tdm)
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