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      Stepwise and independent origins of roots among land plants

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          Abstract

          Roots are one of the three fundamental organ systems of vascular plants 1, where they play roles in anchorage, symbiosis, nutrient and water uptake 24. However, the fragmentary nature of the fossil record obscures their origins and makes it difficult to identify the sole defining characteristic of extant roots – the presence of self-renewing structures called root meristems covered by a root cap at their apex 19. Here we report the discovery of the oldest meristems of rooting axes preserved in the 407 million year old Rhynie chert, the earliest preserved terrestrial ecosystem 10. These meristems, of the lycopsid Asteroxylon mackiei 1114, lacked root caps and instead developed a continuous epidermis over the surface of the meristem. A. mackiei rooting axes and meristems are therefore unique among vascular plants. These data support the hypothesis that roots, as defined in extant vascular plants by the presence of a root cap 7, were a late innovation in the vascular lineage. Roots therefore acquired traits in a stepwise fashion. The relatively late origin of roots with caps in lycophytes is consistent with the hypothesis that roots evolved multiple times 2, rather than having a single origin 1, and the extensive similarities between lycophyte and euphyllophyte roots 1518 therefore represent examples of convergent evolution. The key phylogenetic position of A. mackiei, with its transitional rooting organ, between early diverging land plants that lacked roots and the derived plants that developed roots, demonstrates how roots were “assembled” during the course of plant evolution.

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          Automatic Panoramic Image Stitching using Invariant Features

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            Roots: evolutionary origins and biogeochemical significance.

            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 CO(2) levels generated by plant and microbial respiration in material with restricted diffusive contact with the atmosphere. Chemical weathering consumes CO(2) in converting silicates into bicarbonate and Si(OH)(4). The CO(2) consumed in weathering ultimately came from atmospheric CO(2) via photosynthesis and respiration; this use of CO(2) probably accounts for most of the postulated 10-fold decrease in atmospheric CO(2) from 400-350 million years ago, with significant effects on shoot evolution. Subsequent evolution of roots has yielded much-branched axes down to 40 microm 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").
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              The origin and early evolution of roots.

              Geological sites of exceptional fossil preservation are becoming a focus of research on root evolution because they retain edaphic and ecological context, and the remains of plant soft tissues are preserved in some. New information is emerging on the origins of rooting systems, their interactions with fungi, and their nature and diversity in the earliest forest ecosystems. Remarkably well-preserved fossils prove that mycorrhizal symbionts were diverse in simple rhizoid-based systems. Roots evolved in a piecemeal fashion and independently in several major clades through the Devonian Period (416 to 360 million years ago), rapidly extending functionality and complexity. Evidence from extinct arborescent clades indicates that polar auxin transport was recruited independently in several to regulate wood and root development. The broader impact of root evolution on the geochemical carbon cycle is a developing area and one in which the interests of the plant physiologist intersect with those of the geochemist.
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                Author and article information

                Journal
                0410462
                6011
                Nature
                Nature
                Nature
                0028-0836
                1476-4687
                21 September 2018
                22 August 2018
                September 2018
                01 March 2019
                : 561
                : 7722
                : 235-238
                Affiliations
                Department of Plant Sciences, University of Oxford, South Parks Road, Oxford, OX1 3RB, UK
                Author notes
                Corresponding Author: Correspondence to Liam Dolan liam.dolan@ 123456plants.ox.ac.uk .
                Article
                EMS78591
                10.1038/s41586-018-0445-z
                6175059
                30135586
                e1108357-734e-4472-9f7e-4749891d6958

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