Cardiff University | Prifysgol Caerdydd ORCA
Online Research @ Cardiff 
WelshClear Cookie - decide language by browser settings

Roots: evolutionary origins and biogeochemical significance

Raven, J. A. and Edwards, Dianne 2001. Roots: evolutionary origins and biogeochemical significance. Journal of Experimental Botany 52 (S1) , pp. 381-401. 10.1093/jexbot/52.suppl_1.381

Full text not available from this repository.

Abstract

Roots, as organs distinguishable developmentally and anatomically from shoots (other than by occurrence of stomata and sporangia on above‐ground organs), evolved in the sporophytes of at least two distinct lineages of early vascular plants during their initial major radiation on land in Early Devonian times (c. 410–395 million years ago). This was some 15 million years after the appearance of tracheophytes and c. 50 million years after the earliest embryophytes of presumed bryophyte affinity. Both groups are known initially only from spores, but from comparative anatomy of extant bryophytes and later Lower Devonian fossils it is assumed that, during these times, below‐ground structures (if any) other than true roots fulfilled the functions of anchorage and of water and nutrient acquisition, despite lacking an endodermis (as do the roots of extant Lycopodium spp.). By 375 million years ago root‐like structures penetrated almost a metre into the substratum, greatly increasing the volume of mineral matter subject to weathering by the higher than atmospheric CO2 levels generated by plant and microbial respiration in material with restricted diffusive contact with the atmosphere. Chemical weathering consumes CO2 in converting silicates into bicarbonate and Si(OH)4. The CO2 consumed in weathering ultimately came from atmospheric CO2 via photosynthesis and respiration; this use of CO2 probably accounts for most of the postulated 10‐fold decrease in atmospheric CO2 from 400–350 million years ago, with significant effects on shoot evolution. Subsequent evolution of roots has yielded much‐branched axes down to 40 μm diameter, a lower limit set by long‐distance transport constraints. Finer structures involved in the uptake of nutrients of low diffusivity in soil evolved at least 400 million years ago as arbuscular mycorrhizas or as evaginations of ‘roots’ (‘root hairs’).

Item Type: Article
Date Type: Publication
Status: Published
Schools: Earth and Ocean Sciences
Subjects: Q Science > QE Geology
Q Science > QK Botany
Uncontrolled Keywords: Devonian; endodermis; phylogeny; Silurian; weathering
Publisher: Oxford University Press
ISSN: 0022-0957
Last Modified: 04 Jun 2017 02:09
URI: http://orca.cf.ac.uk/id/eprint/10064

Citation Data

Cited 215 times in Google Scholar. View in Google Scholar

Actions (repository staff only)

Edit Item Edit Item