OFFICIAL54 What limitation of Cotter's research does the professor mention?

[00:00.00]NARRATOR: Listen to part of a lecture in a geology class.
[00:04.01]MALE PROFESSOR: About 30 years ago a geologist named Edward Cotter—that's C-O-T-T-E-R— uh, published a paper that contained a very interesting hypothesis.
[00:15.72]He was studying ancient rivers in a North American mountain chain. [00:19.62]And he noticed that about 450 million years ago, rivers started to behave differently. [00:26.43]Before then, rivers were wide, shallow, and straight. [00:30.37]But after that time, they became deeper and had more curves; [00:34.90]they became increasingly meandering. And that's actually how rivers behave to this day.
[00:40.92]So, why might this change have happened?[00:44.68]FEMALE STUDENT: Maybe there was some kind of climate shift?[00:48.03]MALE PROFESSOR: Well…lots of climate shifts have happened since then.[00:51.67]MALE STUDENT: Was the change worldwide, or just in that geographical area?
[00:55.49]MALE PROFESSOR: Well, Cotter speculated that rivers changed worldwide, but he couldn't prove it… [01:01.47]because he only had evidence from the one North American mountain chain. [01:05.91]But his studies gave him an idea about why rivers started to change—[01:10.93]he hypothesized it had to do with the spread of plant life on Earth.[01:15.75]FEMALE STUDENT: So … there was no plant life before 450 million years ago?[01:20.90]MALE PROFESSOR: Very little according to fossil records. [01:24.78]Anyway, geologists were intrigued by this hypothesis, which claims that as plants evolved and spread, they had an effect on the terrain and rivers. [01:34.12]In the past 30 years, more studies have been done, [01:38.16]and now we have a lot of data about river systems from around 450 million years ago from all over the world.
[01:45.44]In a recent study, a couple of researchers gathered together the existing data and combined them with their own new field data to get a comprehensive picture of the situation.
[01:56.05]Their study was specifically designed to identify changes in the shapes of rivers during the time period when vegetation was evolving.
[02:04.42]And when the researchers compared the data about river shapes with data they had collected about plant life from the same period, the data seemed to prove Cotter's hypothesis.
[02:15.41]MALE STUDENT: OK, but how did plant life affect rivers?[02:18.76]MALE PROFESSOR: Well, in order to answer that question, we need to look at the geological evidence.
[02:24.32]You see, as rivers flow, they leave layers of sediment behind that eventually fossilize. [02:30.80]The content, thickness, and shape of these fossilized layers in rocks give us information about how rivers flowed. [02:38.10]The earliest records from 500 million years ago show that the sediment in river deposits was largely composed of coarse grains of sand and gravel. [02:48.19]That tells us that rivers weren't defined—they were very shallow and wide, almost like floods.
[02:55.94]But around the time of the rise of plant life, the content of those sediment layers began to change. [03:02.55]The coarse grains became much finer, [03:05.18]and we see evidence of mud. [03:07.37]This suggests that plants promoted the preservation of mud when they sent their roots into the ground. [03:13.48]The roots helped to reinforce the ground, which in turn allowed for the creation of riverbanks.
[03:20.12]And we also see evidence of a process called lateral accretion.
[03:26.07]Lateral accretion happens when water flows around a curve, a bend, in a riverbed. [03:32.49]Now, the speed of the flow on the outside of the bend is fastest and slowest on the inside of the bend. [03:39.75]This sets up what's called a secondary flow across the river bottom. [03:44.24]The fast-flowing water on the outside of the bend digs out material from the riverbank and pushes this material laterally across the bottom, and it gets deposited on the other side of the river, on the inner side of the bend.
[03:57.92]So when we see in the sediment layers evidence of lateral accretion— erosion on one side and deposits on the other—that's an indicator that a meandering river existed.
[04:10.44]And according to the study, strong evidence of lateral accretion appears in the geological record…[04:17.30]at the same time that there's also evidence of plants with underground root systems. [04:23.04]This suggests that plants promoted the development of modern rivers by creating stable banks, which resulted in the flow of water in single, meandering channels.[04:34.81]FEMALE STUDENT: So…It looks like the researchers were able to prove the hypothesis…
[04:40.31]MALE PROFESSOR: Well, there's no denying that the study presents a very strong case. [04:44.99]But some questions about this hypothesis remain. [04:48.97]For example, it's well-known that on other planets, like Mars, there's clear evidence of meandering rivers. [04:56.69]But is there evidence of vegetation on Mars? I think not.