The field trip
to Arran was disappointingly devoid of interesting fossils. But, on the last day,
the paleos (plus a group of honorary geologists) went (on an invigorating trip
over a mountain) to work on an Arthropleura trackway. Arthropleura was the largest land
vertebrate we know, a colossal millipede (or maybe centipede… the actual
relationships are not clear) that could grow to over two metres in length! It
lived in near-coast areas of the Carboniferous period, some 300 million years
ago, and was a heavily protected herbivore that would have fed mostly on plant
litter or detritus.
The group was
too large for us all to work on the short preserved trackway, so I was
delegated to examine the other fossil on the site: Stigmaria, a plant root belonging to one of the colossal
Carboniferous club mosses (which are
not mosses at all: they are closer to true trees, but distinguished by having
leaves attached directly to the stem, i.e. no branches in between).
Stigmaria is a morphotaxon, a group of body parts that
is too poorly known to know its evolutionary origin, but is still given a
taxonomic name so that it can be easily referred to. Morphotaxa are common
practice in paleobotany, the study of extinct plants, since you rarely find
fossils of entire plants, but usually only leaves, pollen, trunks or branches
and nothing more. It is then the challenge of paleobotanists to puzzle certain
morphotaxa together into a whole organism, if possible (which rarely is the
case). Stigmaria is considered to be
the roots of Lepidodendron, a 40
metres tall club moss, or lycopod. (So, Stigmaria
is part of Lepidodendron, but
only Lepidodendron is an actual,
classified organism; Stigmaria is
just the roots.)
Reconstruction of Lepidodendron with its Stigmaria
roots.
Some of the best
specimens are quite large and look like this:
Excellent specimen of Stigmaria from http://the-haskellok.com/fossils/id113.html
But the ones on
Arran are not as spectacular.
These are much
smaller and only have the outline preserved. They look nothing like the example
specimens above, and I would never have guessed they were the same unless the
professor had told us. (I am still a bit sceptical…)
There was a
whole bed full of these tiny root pieces.
The root pieces
are short (5-10 cm, mostly) and
abundant. They are tapering (i.e.
narrow toward one end) and mostly gently
curved, as one can expect of plant roots, which need to be hard enough to
penetrate the soil, but soft enough to wriggle around and form a net to cover a
large volume from which to absorb nutrients and water. Some are branching, some are not. The branching
is simple. (I did not see any that branched more than once.)
This makes a bit
of sense considering that the club mosses are quite primitive vascular plants,
so I do not expect their roots to be amazingly complex. However, those pits in
the surface of the better specimens from above make me curious. Could they have
been simple adaptations to increase the surface area for absorption of the
roots, or might they have been points where small rootlets or root hairs came
out? I found this reconstruction on the internet:
Interpretation of the purpose of the
depressions on the surface of Stigmaria
seen in better-preserved specimens.
I interpret it
as suggesting that smaller projections came out of a main root to enhance the
area of soil the roots were in contact with and could take up water and
nutrients from. Actually, I am inclined to speculate that the small,
featureless parts I was looking at could be those protrusions only. The only
thing that makes me want to think twice before jumping to conclusions is that a
great number of the fossils I was examining were branching, which may or may
not make sense with that idea. If those mini-roots were branching, it was
probably to the advantage of the plant, but since I have not heard of anything
like it before, I am reserved not to make a judgement just yet. I prefer to be
cautious and merely put forward the idea rather than take a stand here and now.
Regardless, Stigmaria ought to have been an
efficient root form to be able to anchor and support a giant such as Lepidodendron. Taller trees need
stronger roots to keep them from falling over from strong winds. The roots must
also absorb enough water and nutrients for the large plant to survive. Without
roots, we would not have many plants managing to grow more than a few
decimetres over the ground, and Stigmaria
was one among many pioneering roots in the early forests of the world.
I have three well preserved very detailed stigmaria root fossils. What shall I do with them? Can I sell them? If so, what are they worth?
ReplyDeleteHi Roger!
ReplyDeleteThat sounds fantastic!
Unfortunately, I have no clue to how much they would be worth... Maybe you could search the internet for other people selling plant fossils to give you an idea.
However, before doing anything, I would check around with local museums if they would have any ideas of what to do – who knows, maybe they will be interested in purchasing them for their collections!
Do you remember where abouts you found them? I'm sure that if you want them to contribute to science or something, they'd be really interested in the place you found them (sounds like there could be lots more!! and also, only yesterday, I had a meeting with feedback for one of our fieldtrips, and the trip leader emphasised the importance of knowing where the fossils come from so that paleontologists can work out the context – age, environment, cause of death, cause of preservation, etc.).
... or, the third option would be to just keep them and be that awesome guy with three amazing Stigmaria fossils!! ;)
Hope this helped give you a sense of what you could do :)
Best wishes
Sebastian
Kenny Barr MN
ReplyDelete701378