Remembrance of plants past
Editorial
https://doi.org/10.1038/s41477-026-02322-8
Remembrance of plants past
Check for updates
The timescales on which plants
operate are both much shorter and
much longer than those on which we
function. All we can observe are the
traces they leave behind.
“Time present and time past
Are both perhaps present in time future,
And time future contained in time past.
If all time is eternally present
All time is unredeemable.”
—T. S. Eliot, Burnt Norton
T
ime is a very slippery concept.
We all have an essential feeling of
time and its passage, but as with
so much ‘common sense’, it does
not stand up to scientific scrutiny.
Einstein, with his theory of relativity, thoroughly debunked the idea of an absolute
universal time, showing that it was intimately
connected to the observer’s viewpoint and
that there was no way to define whether
two events happened at the same time or
even which came first. Meanwhile, others
espouse the philosophy of ‘presentism’
(poetically described at the beginning of
Eliot’s Four Quartets) — that the only reality
is the infinitesimally brief present, the past
being a construct of memory and the future
that of imagination.
It might seem that this has little to do with
plant biology, lying more in the realms of
philosophy or theoretical physics, but we
are constantly attempting to reconstruct the
dynamic processes of nature from static data,
a tangible memory of the past.
Arguably, the longest-scale memory of life
comes in the form of fossils. Palaeontology
is not without its challenges, especially when
nature plants
dealing with plants, as they possess few hard tissues, making conditions for good preservation
vanishingly rare. As a result, the fossil record for
the early evolution of plants is woefully incomplete. In all likelihood, this lies behind what
Charles Darwin described as an ‘abominable
mystery’ in a letter to Joseph Hooker: the sudden
abundance and diversity of flowering plant
fossils, particularly dicots, from the late Creta
ceous era and their absence before this time.
Since Darwin’s time, we have become more
comfortable with the idea that evolution does
not always proceed at a constant — slow —
pace. Even so, it can seem surprising that there
are so few, if any, uncontroversial fossils of
angiosperms from the early Cretaceous or
Jurassic eras. Of course, plants do have some
hard and therefore more easily preserved
tissues, specifically pollen. Pollen fossils
have been discovered from an earlier age
than fossils of more complete plants, but
interpretation of fossil pollen in isolation is
not straightforward. Paradoxically, we might
know more about the evolution of marine
algae in the Ordovician than we do about
their land-living descendants several hundred
million years later1. Fossil ‘memory’ can be
clear and detailed, but it is very forgetful.
The other botanical memory we have that
stretches back into geological time is the
DNA in the cells of living plants. While there
is a direct line of descent from the genomes
contained in the nuclei, mitochondria and
chloroplasts of modern plants to those of
their common ancestor and beyond, they
have not come to us as faithfully preserved
as fossils. Instead, they are handed down as
in the children’s game of whispers, in which a
simple phrase becomes corrupted by repeated
cycles of hearing and retelling through a chain
of individuals. Distortions of the genetic
message accumulate more slowly in organelles
than in the nucleus, owing to the absence of
recombination during cell division. However,
by combining a phylogeny of plastids from the
majority of current plant families with time
constraints derived from well-dated fossils, the
origin of angiosperms has been placed somewhere in the Triassic, more than 200 million
years ago2. This intriguingly corresponds
with the age of some angiosperm-like pollen
grains from around 245 million years ago3.
The memory of genomes is also used to
chart the more recent evolution of plant
groups, as in the study of the nuclear genomes
of water lilies published in this issue4.
Plants also retain memories of the times in
which they have lived. This is particularly true
for trees, whose concentric growth circles in
their trunks can be used to trace back climatic
conditions over thousands of years5, especially
when in association with fossilized wood6.
Even the most up-to-date video imaging
techniques used in cell biology are static slices
of events that are already in the past, albeit
separated by sufficiently small gaps in time as
to capture some of the dynamics of the system;
more time-lapse animation than present experience. On even shorter timescales, the ultrafast
processes of photosynthesis must be captured
by the electromagnetic ripples they produce.
Nonetheless, our only tool to prepare for
times future is to interrogate times past as
preserved in the memories of time present.
Published online: 22 May 2026
References
1. Liu, L. et al. Nat. Plants 11, 1116–1126 (2025).
2. Li, H. T. et al. Nat. Plants 5, 461–470 (2019).
3. Hochuli, P. A. & Feist-Burkhardt, S. Front. Plant Sci. 4,
344 (2013).
4. Zhang, J. et al. Nat. Plants https://doi.org/10.1038/
s41477-026-02281-0 (2026).
5. Opała-Owczarek, M. et al. Nat. Commun. 16, 11665 (2025).
6. Schubert, B. A. et al. Sci. Rep. 14, 17189 (2024).
Volume 12 | May 2026 | 899 | 899
(...truncated)