Me. Cook et We. Friedman, Tracheid structure in a primitive extant plant provides an evolutionary link to earliest fossil tracheids, INT J PL SC, 159(6), 1998, pp. 881-890
Most attempts to understand the early evolution of tracheids have centered
on fossil Silurian and Devonian vascular plants, and these efforts have led
to a wealth of new information on early water-conducting cells. All of the
se early tracheids appear to possess secondary cell wall thickenings compos
ed of two distinct layers: a layer adjacent to the primary cell wall that i
s prone to degradation (presumably during the process of fossilization) and
a degradation-resistant (possibly lignified) layer next to the cell lumen.
Developmental studies of secondary wall formation in tracheary elements of
extant vascular plants have been confined to highly derived seed plants, a
nd it is evident that the basic structure of these secondary cell wall thic
kenings does not correspond well to those of tracheids of the Late Silurian
and Early Devonian. Significantly, secondary cell wall thickenings of trac
heary elements of seed plants are not known to display the coupled degradat
ion-prone and degradation-resistant layers characteristic of tracheids in e
arly tracheophytes. We report a previously unknown pattern of cell wall for
mation in the tracheids of a living plant. We show that in Huperzia, one of
the most primitive extant vascular plants, secondary cell wall deposition
in tracheids includes a first-formed layer of wall material that is degrada
tion-prone ("template layer") and a later-formed degradation-resistant laye
r ("resistant layer"). These layers match precisely the pattern of wall thi
ckenings in the tracheids of early fossil vascular plants and provide an ev
olutionary link between tracheids of living vascular plants and those of th
eir earliest fossil ancestors. Moreover, our developmental data provide the
essential information for an explicit model of the early evolution of trac
heid secondary wall thickenings. Finally, congruence of tracheid structure
in extant Huperzia and Late Silurian and Early Devonian vascular plants sup
ports the hypothesis of a single origin of tracheids in land plants.