6 articles
Biomineralization
Biomineralization is the process by which living organisms produce minerals to stiffen tissues, defend against enemies, or store material; in plants it is mostly silica deposited as phytoliths.
Calamites
Calamites is a genus of extinct tree-like horsetails, related to modern Equisetum, that co-dominated the swamp forests of the Carboniferous Period some 300 million years ago.
Evolutionary history of Equisetum
The evolutionary history of Equisetum, the horsetails, shows striking morphological stasis: molecular clocks place the genus's origin in the Early Jurassic or earlier, making it the oldest living vascular plant genus.
Fossil horsetails
Fossil horsetails are the preserved remains of the order Equisetales, jointed-stemmed plants known from the Devonian onward, whose extinct relatives included calamite trees up to 30 meters tall.
Silica in Equisetum: deposition and biomineralization
Silica in Equisetum (horsetails): amorphous SiO2 biomineralization from silicic acid, up to 25% of dry matter, deposited via callose templating and NIP aquaporin transporters, distinguishing horsetails from grasses.
Water transport and hydraulics of Equisetum
Water transport and hydraulics of Equisetum describes how horsetails, lacking vessels and secondary growth, move water through primary xylem and internal canals, with root pressure driving guttation and embolism refilling.