The AMNH course The Dynamic Earth: A Course for Educators provides students with an overview of the origin and evolution of the Earth. Informed by the recently released Next Generation Science Standards, this course examines geological time scales, radiometric dating, and how scientists “read the rocks.” We will explore dramatic changes in the Earth over the last 4 billion years, including how the evolution of life on Earth has affected its atmosphere. In addition to looking at geology on a global scale, participants will take to their own backyards to explore and share their local geologic history. Course participants will bring their understanding of the dynamic Earth - along with content resources, discussion questions, and assignments - into their own teaching.
Evolution of Early Earth's Atmosphere
Loading...
Из курса от партнера American Museum of Natural History
The Dynamic Earth: A Course for Educators
98 оценки
Explore Related Videos
At Coursera, you will find the best lectures in the world. Here are some of our personalized recommendations for you
Из урока
Evolution of the Atmosphere
You will learn how the evolution of photosynthetic life changed the concentration of oxygen in the oceans and atmosphere, and how this is reflected in the rock record. You will also become familiar with how the Next Generation Science Standards connect to this week’s content. Finally, you will complete a written assignment: an analysis of a local geologic feature.
Познакомьтесь с преподавателями
Edmond Mathez, Ph.D.Curator and Professor
Department of Earth and Planetary Sciences
Ro Kinzler, Ph.D.Senior Director
Science Education
This week we're going to talk about the changing composition of the early
atmosphere, and one of the most profound events in that changing composition.
In fact one of the most profound events in Earth evolution, was the
oxygenation of the atmosphere beginning about 2.4 billions years ago, when the
atmosphere essentially contained no oxygen to about 2.1 billion years.
and in that interval,
the oxygen content of the atmosphere increased to approximately
several tenths of a percent, or perhaps a percent.
That's known as the Great Oxygenation Event.
And, what we're going to do is spin out a theory that the oxygen that that caused
this increase came from photosynthesis. from photosynthesizing organisms
such as cyanobacteria, that appeared in the geologic, or that
appeared on, on the planet perhaps a billion years before.
The primary evidence being in fossils known as stromatolites.
So the question is, well, what do we really know?
And that's what I want to explore today.
And to begin that exploration, I'm going to pose two questions.
The first question is,
was the GOE, in other words, the
Great Oxygenation Event, primarily due to biological innovation?
And by that we're talking about photosynthesis.
Or was there some fundamental change in the solid earth that
contributed to or was the primary driver of GOE, of the GOE?
In other words, is there some other cause, or something else
that combined with the production of photo the production of oxygen,
by photosynthesis that caused this increase in oxygen?
And then second question is that
if photosynthesis was important, did photosynthesis actually
emerge just before the Great Oxygenation Event at the end of the Archean?
Or did photosynthesis begin earlier in Earth history?
And did oxygen just was oxygen
just slowly added to the Earth's system to some point where it, there,
there was a threshold that reached, and all of a sudden it increased dramatically?
So let's investigate those two questions.
To begin our investigation, let's consider the evidence for the earliest life.
And to do that, we'll go to West
Greenland, in a sequence of rocks known as the
Isua Complex.
And these rocks crop out near the capital of Greenland, which is the town of Nuuk.
they crop out near the ice cap.
And the, the Isua rocks are essentially among the
oldest surface deposits that we know of on Earth.
They consist mainly of highly
metamorphosed lavas, and highly metamorphosed other
kinds of rocks, that in some cases, we really can't recognize what
they are.
But in some places, what one finds are little enclaves, that
one can actually recognize what the rocks were before they were metamorphosed.
And this photograph right here is is of one such outcrop.
And I think you can see the bedding in that
photograph, suggesting that that layer, layering suggest that it was sedimentary.
these rocks date to 3800 million years ago.
And they hold the evidence for the first life.
So what is that evidence?
As I said, these are metamorphic rocks,
and these metamorpha sediments contain the mineral garnet.
we know from dating techniques, that that garnet formed at about 3.8 billion years.
But as you can see in this
particular slide, the garnet contains small inclusions.
And these inclusions
form trains, that run through the garnet.
And many of those inclusions are made of carbonaceous material.
So, this is a map of the distribution of carbon over this garnet grain.
And you can actually map inclusions with these high concentrations of carbon.
It turns out that the ratio of carbon 13 to carbon 12 in those inclusions,
is consistent with a biogenic origin for these carbons.
That is the primary evidence that life existed on Earth at 3.8 billion years ago.
This is not very strong evidence, we have to admit.
it's not very strong evidence, because we don't really know what happened to this
carbon during the metamorphism. Metamorphic processes can actually
change the carbon 13 to carbon 12 ratio. so we don't
actually know what happened, prior to the entrapment of the carbon in the garnet.
But what we do know, is that these carbons these inclusion carbons, have
not changed their composition since they were trapped at 3.8 billion years ago.
Now as I mentioned the evidence for photosynthetic organisms
also exist in the form of stromatolites.
The first evidence of which appears on the planet about 3.4 billion years ago.
But a very important piece of evidence about the nature of early life, occurs at
about 2.7 billion years. When we find bio-markers, or
in other words, molecular fossils, that provide evidence that bacteria and
eukaryotes existed on Earth at that time. Molecular fossils,
that is to say bio-markers, are these relatively refractory organic compounds.
they're derived mainly from lipids.
lipids are compounds that make up cellular membranes, for example.
And these compounds become incorporated in the sediments, and of
course they do break down with time and, and lithification.
But absent extreme metamorphism, certain structural components of these compounds
survive, and we find them in these rocks. So they've survived for billions of years.
Some of these structural components are
diagnostic of bacteria such as cyanobacteria.
Some other structural components, are also diagnostic of eukaryotes.
And if that's true, eukaryotes certainly
must have indicated the presence of photosynthesis.
So there's good evidence, that photosynthesis existed at
least by 2.7 billion years, and probably earlier.
So what is the significance of these observations that life may have
existed on Earth at 3.8 billion years? And that by at least
2.7 billion years fairly complex forms of life existed.
Well, it's embodied in in this statement here, the
Archean saw the emergence of quote, diverse metabolic pathways,
photosynthesis, carbon fixation, nutrient assimilation, and lipid biosynthesis.
It was the cardinal epoch of biochemical innovation.
And that's a quote from Waldbauer et al.,
in 2009.
That's the significance of these observations.
The Archean was this cardinal epoch of biochemical innovation.
But now let's think about photosynthesis. Here's a model reaction.
Carbon dioxide plus water goes to the
organic compounds that make up the organism
plus oxygen, and of course we need energy for that, in the form of sunlight.
Well, I think you can see by this model reaction, what I mean
by a model reaction, is a simple reaction that illustrates a general process.
I think you can see that
the oxygen actually isn't going to build up in the system unless
the oxygen and the oxygen and the organic material Is separated.
Because if the organic material is just sitting
around on the surface, it's going to oxidize with
any excess oxygen to form carbon dioxide, and
oxygen isn't going to build up in the system.
So we need to figure out a way to get rid of the
organic material. And one way to do that is to bury it.
And now this brings us to another
question, how are we going to bury organic compounds?
And it brings us to the matter of the role of tectonics of this whole affair.
Here's a map.
This is a map of all the present
day continents, not in their present position of course.
And the black areas are the areas of exposed
Archean crust.
The gray areas of exposed Proterozoic crust, and the
white areas the you know, the younger Phanerozoic crust.
That is crust that's less than about 640 billion years old.
so there's extensive Archean crust.
But what we observe is that most Archean crust is
really made of igneous rocks and metamorphic equivalents of igneous rocks.
While the Proterozoic crust, is characterized
as well by extensive sedimentary basin.
So at the end of the Archean, just
before the Great Oxygenation Event, it appears that that
was the time of the beginning of the development
of large sedimentary basins, and erosion of the continents.
So in other words this is a time also of extensive shallow seas.
Which could have been you know, provided expanded
habitat for stromatolites. the continents must have eroded at
this time, to produce all this sediment that we see in the rock record.
erosion implies that it was rock weathering,
and rock weathering implies that that, or, or
is a process rather that we expect
to influence both ocean composition, and atmosphere composition.
And the presence of the sedimentary basins is one way to
rapidly very organic material.
More generally, plate tectonics must have existed at this time.
And that also means that there was biochemical recycling,
between the surface of the planet and the mantle.
So maybe
this burial involved injection of carbon by
subduction and water by subduction into the mantle.
So all of these processes could help oxidize the Earth.
So let's return to the original questions.
you know, what was the cause of the Great Oxygenation Event?
And,
you know, what was the role of photosynthesis?
And, I think fundamentally, we just don't
know the answers to those questions.
They remain unanswered.
Ознакомьтесь с нашим каталогом
Присоединяйтесь бесплатно и получайте персонализированные рекомендации, обновления и предложения.
Coursera делает лучшее в мире образование доступным каждому, предлагая онлайн-курсы от ведущих университетов и организаций.
© Coursera Inc., 2019 Все права защищены.
