English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Solid deposits of amorphous hydrated silica are formed at specific intracellular and extracellular locations in many plant taxa, including all taxa in Triticeae. These deposits of silica are called phytoliths, literally meaning “plant-rocks.” Many plants produce phytoliths with morphological characteristics that appear unique to a given taxon, a phenomenon giving them taxonomic significance. When plant tissue decomposes, any phytoliths formed are released into the surrounding environment thus becoming microfossils of the plants that produced them. Analysis of microfossil phytoliths can provide information to researchers in a wide variety of disciplines, including, archaeobotany, paleoecology, phytogeography and systematics. This paper reviews current methodologies and results of typologic and morphometric analysis of wheat and barley phytoliths.

Review of typologic and morphometric analysis of phytoliths produced by wheat and barley