My
wife and I just got back from a visit to Buffalo National River in Arkansas. It
is a beautiful place to see nature at work. We stayed in an old hotel in
Harrison, and planned our days in such a way that we could work around the
intermittent and unpredictable rains. (I recommend the 1929 Hotel Seville in
Harrison as a place that is close to the river but inexpensively elegant in
case you have to sit around in the lobby during rain.) We did all of our hiking
between rains on May 28. One of the main attractions of Buffalo National River
is the green forests—which you cannot have without lots of rain.
Canoeists
and kayakers revere the Buffalo National River for its scenic limestone cliffs:
But
to an evolutionary ecologist, the river is also a living system. Along the river
itself we saw lots of seedlings and re-sprouted saplings of box elder,
sycamore, sweetgum, catalpa, birch, and persimmon. I do not know why, but we
saw not a single cottonwood. These trees grow in areas disturbed by strong
floods. If they get a chance, they grow into forests, at least the boxelders,
sycamores, and sweetgums; the catalpas do not live long enough to become canopy
trees, and the persimmons spread horizontally by underground stems rather than
upward to reach the canopy. In a floodplain forest long undisturbed by floods,
we saw very large birches and sweetgums, along with southern red oaks. This
photo is of a very tall birch, but it was still leaning halfway over the way it
did when it was a riverside sapling.
When
we hiked along Mill Creek, we saw some floodplain forests that were almost
monospecific stands of box elder:
The
riverside forests and the bluff forests were very different. Some species, such
as sweetgum, grew in both; but the bluff forests had no box elders. On a bluff,
we saw at least one tree species that seemed out of place: a chittamwood tree,
which I associate with drier forests. The bluff presumably provided an
ecological refuge for this tree, which would not be able to compete with the
tall oaks (white, northern red, southern red, and chinkapin) and hickories.
Some trees such as pawpaw specialized on open spots on the forest floor. Mesic
forests and drier forests have different conditions and different dominant tree
species; but because of dry microenvironments, trees more common in drier
forests can find a foothold in these mesic forests—this is one reason that
mesic forests have such high biodiversity. (We did not, however, see any post
oaks.) We recognized 42 flowering plant families; there must have been more.
(It’s nice to have a spouse who, though not a professional botanist, loves
plant families as much as I do.)
To
accommodate search engines that may search for information about these trees, I
will list some of the Latin names. Those of you who are not interested in Latin
names, please skip to the next paragraph.
Acer negundo (Aceraceae),
box elder
Asimina triloba (Annonaceae),
pawpaw
Betula nigra (Betulaceae),
birch
Catalpa
bignonioides
(Bignoniaceae), catalpa
Diospyros
virginiana
(Ebenaceae), persimmon
Liquidambar
styraciflua
(Altiginaceae), sweetgum
Platanus
occidentalis
(Platanaceae), sycamore
Quercus alba (Fagaceae),
white oak
Quercus falcata (Fagaceae),
southern red oak
Quercus
muhlenbergii
(Fagaceae), chinkapin oak
Quercus rubra (Fagaceae),
northern red oak
Sideroxylon lanuginosa (Sapotaceae),
chittamwood
We saw more than just plants, of course. It was also the perfect day for this beautiful species of fungus:
On
the rainy day we visited Mystic Caverns, which are very beautiful:
And
delicate: the oil from even one finger-touch can disrupt mineral deposition. Some
of the stalagmites resembled Schmoos from an Al Capp cartoon; in fact these
caverns used to be owned and operated by Dogpatch USA, a now bankrupt and
vine-engulfed amusement park right across the highway.
The
leader was a preacher and handgun instructor who preached us his guns and
creationism gospel. He pointed out, quite correctly, that calcite deposits can
form quickly; he should know, as he has watched them form. But he also showed
us a limestone rock with crinoids in it, and claimed that they could only have
come from The Great Flood. He did not consider the possibility that the
crinoids were in the limestone parent material upon and around which the
calcite deposits formed. I did not ask him any of a thousand possible
questions. What would have been the point? Besides, I was the guy who belted
out “Deep River,” an old gospel song, in the echo chamber (at the manager’s
invitation). This was where the orchestra used to stand in the 1930s when this
cavern had a moonshine still in the back and a dance floor. (Presumably some of
the people, drinking moonshine, thought they were dancing until somebody
stepped on their hands.) I chose to sing Deep River rather than to argue
against a creationist. I was, after all, on vacation. Most of the people on the
tour were what Mark Twain called Arkansaurians and would not have believed me;
the others were young people, including a Japanese couple, who got rained out
of their rock climbing plans and presumably already agreed with me. So this was
not what one would call a teachable moment.
The
Buffalo National River is a beautiful place to visit and to observe the natural
world closely.