In my previous post about Laramidia, and in attempting to
explain how the plants and trees were able to provide enough fodder for the
large numbers of herbivorous dinosaurs that grazed there, I looked at how a
combination of climate, physical and meteorological barriers, and the food
value of the plants themselves, could have sustained such a voracious
herbivorous assault.
And yet, there was another driving force behind the ability
of the plants to, not only survive, but to flourish and quickly recover from sustained
grazing – and that was the dinosaurs themselves. Animal partnerships, relationships and
animal/plant relationships were almost certainly as evident in the past as they
are today and the term used to describe the change affected on one species that
interacts with another is coevolution.
The concept of coevolution was first raised by Charles
Darwin in Origin of Species and has been gradually refined through the years
but the theory still comes under intense scrutiny as scientists try and decide
whether the evidence presented for each individual example is truly
coevolution. In other words, any form of
interaction or symbiosis that produces evolutionary change can only be classed
as coevolution when substantiated by thorough research and the appropriate
phylogenetic analysis.
Having said that, however, there is ample evidence that implied
coevolutionary interaction is extremely likely and there are numerous examples around
today – bumblebees and flowers are an appropriate example. The effect of one
species on another cannot be denied and in its simplest form is very apparent.
Entire species have become extinct or virtually extinct because a foreign
species was introduced by accident or even on purpose. Examples are legion:
grey squirrels driving out the reds in England, possums in New Zealand devastating
flightless bird populations and, in Mauritius, even Man eradicated the dodo.
Indirect extinctions are yet another form of interaction
that is also far removed from coevolution.
The eradication of a species without any thought can have a massive effect,
from the smallest invertebrate through to the biggest apex predator – a domino
effect if you will. This form of extinction is most likely to affect different
species that are extremely dependent on each other or those taxa that are the
cornerstone of many niches thus affecting multiple species.
A couple of very simple examples of this include six species
of mite that became extinct when the Carolina parakeet disappeared and a vine
plant in Singapore that, when it disappeared, took with it one particular
species of butterfly that was dependent on it. To demonstrate a possible future
scenario, off the coast of California, there is a delicate ecosystem involving
kelp, sea urchins and sea otters. These three species are so totally dependent
on each other that the fragility of such ecosystems becomes evident.
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| Image by Katie Hale |
The sea otters keep the sea urchin population under control
which, if left unchecked, would completely devour the kelp forests. Without the
kelp, a multitude of different organisms would disappear and yet, without a
sufficient population of urchins, the sea otter population would quickly crash
and decline. This clearly demonstrates the fragility of such ecosystems and
dramatically highlights how the extinction of one species can affect so many
others.
Partnerships, or mutualism to give it its correct term, are
another form of interaction. The most oft cited example of this is the
relationship between ants and acacia trees. The ants depend on the acacia for
nesting and food whereby the plant
provides specialised thorns that provide shelter, special nectar buds that
provide food for the ants and leaf tips that are also of a high food value –
especially to the larvae. The ants, in return, remove fungal spores from the
tree that may invade the acacia host and provide aggressive defence against any
herbivore foolish enough to attempt to feed on the tree. This particular example
has often been cited as coevolution so amply demonstrates how hard it can be to
classify.
All of the examples highlighted above demonstrate how
different species affect one another through various examples of interaction.
Despite these all being contemporary examples, it does demonstrate that such
relationships have existed, almost certainly, from the earliest forms of life
right through to the present day. So how does this all relate to dinosaurs?
Bob Bakker, in his book the Dinosaur Heresies, featured a
chapter titled Mesozoic Arms Race in which he postulates how both herbivore and
carnivore spurred on the mutual evolution of the two groups – in other words,
true coevolution. As theropods got bigger to cope with larger prey, the
herbivores got bigger still. If it wasn’t size, it was armour, horns, teeth,
claws, agility, and social interaction – a plethora of derived traits
continually evolving to keep the different genera ahead of the game and ensure
survival. Those that did not evolve became extinct. This is the classic example
of survival of the fittest – natural selection. Evolve or die.
I suspect that trees and plants were also part of this life
or death struggle and that their ability to be able to sustain large populations
of giant herbivorous dinosaurs was a direct response to intense grazing
pressure from dinosaurs. As herbivorous dinosaurs got bigger and their ability
to crop the plants, masticate and digest plant material became more
sophisticated, the plants and trees had to adapt or become extinct. They had to
find new ways to be able to withstand the stress of being constantly cropped, be
able to reproduce quickly, and grow at inflated rates.
The fact that there are so many different shaped and sized
herbivorous dinosaurs is highly indicative that they were successful. Small
ornithopods would graze at low levels, mid-sized animals could take advantage
of both whilst animals such as brachiosaurs and titanosaurs could feed at
higher levels. Whilst appreciating this is a very simplified way of looking at
things, the point is well made. Herbivorous dinosaurs evolved into many
different and complex varieties to cope with the continually evolving plants.
In the Cretaceous, things moved on to another level with the
evolution of much more complex herbivorous dinosaurs. The well-publicised iguanodont and
hadrosaurian dental batteries, which enabled a much more efficient form of food
processing, along with ceratopsians, ankylosaurs, sauropods and other
ornithopods, pushed plants and trees to new heights of production.
But this time the plants and trees had even more help with
an increase in the amount of CO2 in the atmosphere, increased warmth and
moisture and this combination enabled the flora to grow at inflated rates. And
there was yet one more innovation by the plants to come which aided
reproduction, fertilisation and increased diversity and sustainability.
It has been often noted that the dinosaurs may have been
responsible for the appearance of flowers during the Cretaceous (eg again see
Bakker 1986). Although there is no foundation or scientific evidence to back
this assertion, it does appear likely that intense dinosaurian herbivory may
have contributed to the evolution of flowering plants (Barrett et al 2001 but
see also Lloyd et al 2008).
The truth is almost certainly something in between. The
dinosaurs probably prompted rapid development in plants to avoid eradication
and extinction. During the Cretaceous conditions were so good for growth that
the plants simply took advantage of the situation and evolved extremely rapidly
- with flowers simply another tool which allowed further diversity and
distribution. This enabled the dinosaurs to feed on an almost never ending
supply of fodder and is possibly the chief reason why Laramidia was able to
sustain such large populations of big dinosaurs.
References
Bakker, R. 1986. The
Dinosaur Heresies: New Theories Unlocking the Mystery of the Dinosaurs and
Their Extinction. William Morrow and Company, New York.
Barrett P.M, Willis K.J. Did dinosaurs invent flowers?
Dinosaur-angiosperm coevolution revisited. Biol. Rev. 2001;76:411–447.
doi:10.1017/S1464793101005735[PubMed]
Lloyd, G.T., Davis, K.E., Pisani, D., Tarver, J.E., Ruta,
M., Sakamoto, M., Hone, D.W.E., Jennings, R., and Benton, M.J. 2008. Dinosaurs
and the Cretaceous Terrestrial Revolution. Proceedings of the Royal Society,
Series B 275, 2483-2490 (doi:10.1098/rspb.2008.0715).


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