I
became a scientist one evening in 1978 when I was participating in the plant
ecology group studies seminar at the University of California at Santa Barbara.
I asked a stupid question.
I
was an undergraduate environmental biology major. I took some very good courses
that acquainted me (firsthand, with extensive field trips) with the ecology and
vegetation of southern California. I continue, over forty years later, to draw
from the wellspring of the inspiration I got at that time for my writing.
If
I just wanted to write, and to teach at perhaps a community college level, all
these experiences would have been enough. But I wanted to be a university
professor. For this, I needed to learn how to do my own research. If I had just
wanted to help a researcher, I could have become a lab technician. But I wanted
my own research to expand our understanding of nature.
When
we got back our graded exams in Bill Schlesinger’s plant ecology class in 1977,
I got an 88, which seemed kind of mediocre to me, but it turned out to be the
best grade in the class. Bill invited me to participate in the plant ecology
group studies seminar, which met once a week in the evenings. These were the
meetings in which the graduate students presented their own research, leading
to advanced degrees. I assumed I was up to the challenge of participating in
this.
The
instructors (all of the botanists at UC Santa Barbara) assured me that the
first quarter of this course all I had to do was participate intelligently in
discussions. In many cases, we read a paper published in a scientific journal
and discussed it. I, however, struggled to understand the papers. Anyone who
has, without training, looked at a scientific paper knows that scientific
research is a world unto itself. I read the papers as carefully as I could and
wrote down questions that seemed intelligent to me. But I was unable to launch
myself into a discussion that was at the level of some of the best researchers
in the world.
That
is, until one of the faculty said, “I want to hear from the new people.” I was
the only new person there. Bruce Mahall looked and sounded like a fierce
Scottish warrior.
Fortunately,
I had a question ready. The paper was about air pollution infiltrating into the
soils of a forest. My question was, “What is the oxygen layer?”
Everyone
in the room was stumped. They didn’t know what an oxygen layer was either.
Finally
one of the younger faculty piped up, “Oh, he’s talking about the O2
(oh-two) layer.” O2 is the chemical formula of atmospheric oxygen.
Each molecule consists of two oxygen atoms. I knew this from the year of
general chemistry, and another year of organic chemistry, that I had been
required to take from 1975 to 1977. But apparently, as it turns out, O2
also refers to the second organic layer in the soil. The two organic layers,
the second of which is sticky humus, sits on top of the mineral soil layers. I
think the young professor was gloating a little, as young professors at big
research universities often do. They have to prove themselves by outshining
others, even if the others are little undergrads. No harm done, though. I had
asked my question and was now a participant, rather than just an observer.
This
was the evening I became a scientist. My first act as a scientist was to ask a
stupid question. But, in a way, the entire history of science is about people
asking stupid questions and then pursuing the answers. For example, it is
obvious to us today that the Earth revolves around the Sun, but in Galileo’s
time, it was not obvious. Other scholars were openly hostile to Galileo. Go
outside and look. You cannot see the Earth going around the Sun; you have to
figure it out from evidence. This would not be the last stupid question I would
ask myself or others.
A
student could take the evening seminar course as many times as necessary,
because the course was never twice the same. The second time I took the course,
I had to sign up for leading one of the discussions. We sat at tables around a
central point. The signup sheet started on the other side from me. By the time
the sheet got to me, there were two slots left: the next week, and the week
after. Bill Schlesinger was my undergrad advisor and he signed up for the first
slot. I “chose” the second. I had no idea how to get started, so Bill offered
to show me how.
When
I went to his office, he said, “If I were you, I’d be pretty scared right now.”
I
think he was only half serious, since all the faculty and graduate students
knew to not judge me by their standards. Bill’s advice was pretty simple.
Choose a paper (within the topic the group had chosen), and then also read the
papers in the reference list at the end. Put them all together, and you have a
presentation.
The
next week I gave my presentation, something about nitrogen in grasslands. It
was apparently pretty good for an undergraduate. Some faculty told me so.
Cornelius H. Muller (“Neil”), however, did not say anything. He was a very old
and experienced plant ecology researcher, from back in the 1930s when to do
research all you had to do was ride your horse around. By riding his horse
around, he had discovered the complex mixture of oak species that lived on
hilltops over the Texas desert. (He spoke with a Texas accent.) This was an
important breakthrough in our ecological understanding, because the oak
woodlands of these “sky islands” were little remnants of what had once been
extensive oak forests, which died out as the weather became dry in recent
millennia, except for the hilltop survivors. He discovered several species that
had almost become extinct. As an elder statesman in ecology, he always wore a
tweed jacket, white shirt, and red bowtie. He came up to me after my
presentation. Though he said nothing, he had a tin of cookies, and offered me
one, with a smile. I think this meant he was pleased.
The
next summer, 1978, I was as ready for my own research as an undergraduate was
likely to be. Bill Schlesinger oversaw the research project. I remain amazed at
how a well-known and rapidly rising star of plant ecology took time for what
turned out to be a research project that was big on experience and short on
success. I had access to all of this grant-funded research equipment. Short on
success, but experience was what I needed.
I
chose to analyze the patterns of which plants grew where in an area of the
Santa Ynez Mountains upslope from Lompoc, California. In some places, there
were chaparral shrubs, that needed fire to persist; sage scrub bushes, that did
not; and some very interesting pine trees. These bishop pine trees were a
little population over a hundred miles away from its main habitat. This little
area was also unique because it did not have what we would normally call soil.
The ground consisted of a thick layer of diatomaceous earth. It had formed when
dead diatoms (floating single-celled algae) had built up in shallow oceans,
such as the Pacific coast that was only a few miles away, over the course of
millions of years. The diatoms became rock. Geologic forces (such as
earthquakes with which California is all too familiar) raised these rock
layers, bright white, up a few hundred feet. Here, and only here, was where the
bishop pines grew. Why? Nobody really knew. Here was my chance to not only get
experience but to advance the scientific understanding of nature.
The
diatomite is not really rock, and is very lightweight, as you can see from this 1978 photo of me.
We
quite reasonably assumed that the pines grew on the diatomaceous earth because
of the chemical composition of the earth, which was different from the soil of
the surrounding hills. My project was to estimate the importance of the
different kinds of plant cover (pines, chaparral, etc.) and to get soil
samples. We would, quite simply, see if the pines grew where they did because
of the chemistry of the soil samples.
Here
is where the experience came in. Crawling through a chaparral is difficult and
dangerous. Little branches almost completely fill the space. I was not a large
person but even I had trouble getting around in the chaparral. Rattlesnakes,
which were abundant, could get around in it better than I could. I also took
wood core samples from the pine trees. It was very hot. If I could do this
project, out in an almost brutal natural setting, then the life of a field
researcher was for me. I was on my way to eventually becoming a professor. You
don’t get there by sitting in a library.
But
it was not the only experience I had along the way to becoming a researcher. We
analyzed the major soil nutrients in Bill’s lab, which was one of the best
places to do so. When we compared the nutrient makeup with the vegetation
cover, we found that the pine forests had more magnesium in the soil than the
other types of plant cover. This might mean that pines grow best on
high-magnesium soil. Or not. But there was one puzzling aspect of the results.
The diatomaceous earth seemed to be ten percent sodium. When I presented my
results at the seminar, we were all puzzled. Bruce pointed out that if the
sodium was in the form of sea salt, not unthinkable with the ocean just a mile
away, then there would also be ten percent chloride, and the soil would therefore
be twenty percent salt. This would not only be enough to kill any plants, even
the pickleweeds down in the nearby salt marsh, but it would mean that the soil
would dissolve in the rain.
My
seminar presentation also turned out to be funny, but not because of the salt.
Some of my measurements were from the edges of the Johns Manville quarry, where
the company dug away whole hillsides of diatomaceous earth to sell. The man I
stayed with in Lompoc was the leader of the little church I attended, and as an
employee of JM, he got me permission to work near the mine. At the seminar, I
showed a picture of myself that I had taken with a camera on a tripod. I had on
a miner’s hard hat on which I had placed two flaps to cover my ears. I
explained that this was to keep the flies out of my ears. For some reason I
still do not understand, the whole room of professors and students erupted into
unaccountably prolonged laughter when I said this.
Later,
long after all interest in my research project had passed, Bill realized what
had happened. Sodium was one of the components of the solution which we had
used to extract nutrients for the analysis. The sodium was not actually in the
soil. This seemed like such an obvious blunder that only I could have made it,
but an eminent scientist had made it instead. The experience I got from this is
that anybody, even a great scientist, can make a silly mistake.