Latest / Talking Science / The Anthropocene – Humanity as a Geological Force
Transcript
- 0:00Welcome to the deep dive. Whether you are prepping
- 0:03for a meeting, commuting, or just, you know,
- 0:05insanely curious about the world, you are in
- 0:08the right place. Yeah, we have a really fascinating
- 0:10one today. We really do. So today we are taking
- 0:12a stack of really profound source material and
- 0:15unpacking an idea that, well... it might just
- 0:19shift how you see your entire existence on this
- 0:21planet. Which I know sounds like a massive promise,
- 0:24but the concepts here are just wild. Right. So
- 0:28to get into the right headspace for this, I want
- 0:30you to just imagine the Earth as this massive
- 0:34ancient archivist, like just this silent librarian
- 0:38methodically writing down literally everything
- 0:41that ever happens on the planet. Obviously, you
- 0:43know, it's not using paper and ink. Yeah, no,
- 0:45no paper. It is logging the shifting continents,
- 0:48the ice ages and, you know, the occasional catastrophic
- 0:51asteroid impacts all in layers of mud, ice and
- 0:55stone. It's just a completely impartial record
- 0:57keeper. I mean, the planet simply absorbed whatever
- 0:59happens on the surface and permanently presses
- 1:01it into the rock layers for the rest of time.
- 1:03Right. And for billions of years, that process
- 1:06was driven entirely by blind natural forces.
- 1:09But the source material for our deep dive today,
- 1:12it forces us to confront this staggering concept.
- 1:17Yeah, the idea that we are no longer just living
- 1:18on the Earth. Exactly. The argument on the table
- 1:21is that human beings have become a geological
- 1:23force so overwhelmingly powerful that, well,
- 1:27we are changing the planet on a scale that will
- 1:30be perfectly legible in the rocks millions of
- 1:32years. We are essentially the ones writing in
- 1:35the Earth a diary now. And this brings us to
- 1:38the core concept of our exploration today, which
- 1:40is the Anthropocene. The Anthropocene. Yeah.
- 1:42It's a term you might have heard, like bleeding
- 1:44out of academic geology and into just everyday
- 1:46conversation. So Anthropo, meaning human, and
- 1:49scene. referring to a geological epoch. It's
- 1:53just such a heavy, provocative idea. So our mission
- 1:55today is to take an unhurried, you know, jargon
- 1:58-free look at what it actually means. Absolutely.
- 2:00We're going to break down how time actually works
- 2:03for a planet, what specific evidence we are currently,
- 2:06like, burying in the dirt for future geologists
- 2:10to find, and perhaps most surprisingly, the fascinating
- 2:13scientific drama over whether this new era is
- 2:16actually officially real. Let's start with the
- 2:19foundational piece here because... To understand
- 2:23how humans are supposedly hijacking the geological
- 2:25record, we really first have to understand how
- 2:27the Earth actually keeps time. Right, which is
- 2:30totally different from human history. Oh, completely.
- 2:32We have to step out of the realm of human history
- 2:35and into what geologists call deep time. I mean,
- 2:38the Earth is about four and a half billion years
- 2:40old. Which is just a number our brains simply
- 2:42aren't wired to comprehend. No, not at all. It's
- 2:44too big. I was reading about this in the sources,
- 2:46and the way geologists manage this immense span
- 2:50of time is through, like, this nested hierarchy
- 2:53of named time intervals. Yeah, it helps break
- 2:55it down into manageable chunks. Right. So you
- 2:58start with the largest chunks called eons, and
- 3:00those are broken down into eras, which are broken
- 3:02into periods, which finally break down into epochs.
- 3:05Think of it like the folders on your computer
- 3:09or just a basic calendar. That's a great way
- 3:11to put it. Yeah. So years contain months, months
- 3:14contain weeks, weeks contain days. It's all nested.
- 3:17And to visualize how they actually read this
- 3:19calendar. You know, you have to think about stratigraphy,
- 3:22which is the study of rock layers. Okay. So when
- 3:25a geologist looks at a canyon wall or, say, a
- 3:28deep core sample taken from the ocean floor,
- 3:31they are essentially looking at the spine of
- 3:33a massive book. Over millions of years, dirt,
- 3:36sand, organic matter, it all settles at the bottom
- 3:40of lakes and oceans. Just piling up slowly over
- 3:42time. Exactly. And the immense pressure from
- 3:45the earth compresses that sediment into solid
- 3:47rock. As the environment changes, the type of
- 3:50sediment changes. Yeah. And that creates these
- 3:52distinct visible bands or strata. So the boundaries
- 3:56between an era or an epoch, they aren't just
- 3:58arbitrary dates we picked. It's not like the
- 4:00boundary between December 31st and January 1st
- 4:03on our calendar. Right. Nature didn't just print
- 4:05a new calendar page. In geology, these boundaries
- 4:08are massive, unmistakable physical lines in the
- 4:11stone. Yeah, they mark genuine planet -wide physical
- 4:15changes. Like for a new geological time interval
- 4:18to be formally recognized, there has to be a
- 4:21distinct signature preserved in those rock layers.
- 4:23And it has to be everywhere, right? Exactly.
- 4:26It must be clear and global enough that a geologist
- 4:29digging in, I don't know, Australia and another
- 4:32one digging in Canada can both point to the exact
- 4:35same anomaly. Wow. OK, so what kind of anomalies
- 4:38are we talking about? Well, we are talking about
- 4:39things like the sudden rise or fall of huge groups
- 4:42of life, mass extinctions, dramatic shifts in
- 4:46the Earth's climate or massive changes to the
- 4:48composition of the atmosphere. Which brings us
- 4:51to the geological folder we currently occupy.
- 4:53Because officially, according to the current
- 4:55geological calendar, we live in an epoch called
- 4:58the Holocene. Right. And the Holocene began nearly
- 5:0012 ,000 years ago, just right at the end of the
- 5:03last ice age when massive glaciers finally retreated.
- 5:07And the sources made a really interesting point
- 5:09here. When geologists look at the rock and ice
- 5:11core layers from the Holocene, the defining characteristic
- 5:14they see is just incredible stability. Yes. It
- 5:19has been this remarkably warm, quiet, stable
- 5:23stretch of planetary time. And the significance
- 5:25of that stability for you listening right now,
- 5:28it honestly cannot be overstated. That quiet
- 5:30stretch of 12 ,000 years. is literally the cozy
- 5:34cradle in which all of human civilization has
- 5:37flourished. It really is. I mean, it's essentially
- 5:39been the Goldilocks zone for humanity. Right,
- 5:41because every farm, every city, every written
- 5:44word, every empire that rose and fell, all of
- 5:46it only happened because the Holocene provided
- 5:48a stable climate window. The predictable seasons
- 5:50allowed us to invent agriculture. And that allowed
- 5:53for static populations, which, you know, eventually
- 5:56allowed for the modern world. But, and here's
- 5:58the massive pivot. If the Holocene is defined
- 6:00by that beautiful, quiet stability, the whole
- 6:02proposal of the Anthropocene argues that human
- 6:05activity has violently ended that quiet period.
- 6:08Right. The argument is that we have pushed the
- 6:10Earth into a brand new, fundamentally different
- 6:12chapter. But I want to dig into the mechanism
- 6:14of this. Because if geological boundaries require
- 6:18a permanent physical marker in the rock, you
- 6:22know, like the iridium layer left by the asteroid
- 6:24that wiped out the dinosaurs. What on earth are
- 6:27humans laying down today that will survive the
- 6:30shifting tectonic plates? That's the big question.
- 6:33Like, are future geologists going to find fossilized
- 6:35smartphones millions of years in the future?
- 6:38Well, I mean, probably not an intact smartphone.
- 6:41Yeah. But it really all comes down to permanence.
- 6:44What is going to become the rocks of tomorrow?
- 6:47Okay, so let's methodically walk through the
- 6:49evidence detailed in our source material, starting
- 6:51with something we use every day, plastics. Right,
- 6:53plastics. We manufacture plastic on such a colossal
- 6:57scale, and as we all know, it takes so incredibly
- 6:59long to degrade. So it's now spread across literally
- 7:02every corner of the planet. Yeah, the sources
- 7:04mention it's not just sitting in landfills anymore.
- 7:07Microplastics have made their way all the way
- 7:09down into deep ocean sediments. And that's crucial.
- 7:12Because when those ocean sediments slowly pile
- 7:15up and eventually get subjected to the immense
- 7:18heat and pressure of the Earth's crust over millions
- 7:20of years, they bake into sedimentary rocks. Because
- 7:24the plastic becomes part of the rock. Exactly.
- 7:26The synthetic polymers of our plastic trash will
- 7:29get permanently locked into that rock matrix.
- 7:31They won't look like a perfectly preserved water
- 7:34bottle, but they will form a distinct... carbon
- 7:38-heavy chemical band that has just never existed
- 7:41in nature before. Wow. And some geologists call
- 7:44these technofossils, right? Yes, technofossils.
- 7:47It's a weird synthetic band of rock just wrapping
- 7:50around the entire globe. That is wild to picture.
- 7:53And then the sources detail the impact of concrete.
- 7:56Which, if you think about it, is essentially
- 7:57just an artificial rock that we invented. Yeah,
- 7:59that's exactly what it is. And we have poured
- 8:01such a staggering volume of concrete that it
- 8:04basically coats the planet's surface in a way
- 8:07nothing in nature ever naturally has. So it's
- 8:09this dense footprint that will absolutely leave
- 8:12a massive scar in the geological record. Absolutely.
- 8:15And it's not just the solid stuff on the ground.
- 8:18We're also leaving permanent markers in the atmosphere
- 8:21and the oceans. Okay. How does that work? Like,
- 8:23how does air become rock? Well, think about the
- 8:26slow carbon cycle. Normally, the Earth regulates
- 8:29its temperature over millions of years. Carbon
- 8:31gets locked in rocks. It's slowly released by
- 8:34volcanoes into the atmosphere, absorbed by rain,
- 8:37washed into the oceans, and eventually settles
- 8:39back into the rocks. A very slow, balanced loop.
- 8:42Exactly. But humans have dug up hundreds of millions
- 8:45of years worth of stored carbon -like coal and
- 8:48oil, and we've burned it in a matter of just
- 8:50a few decades. Which drastically alters the atmospheric
- 8:53chemistry really fast. Right. And by changing
- 8:56the air so quickly, we are changing the ocean's
- 8:59chemistry. As the oceans absorb all that excess
- 9:02carbon, they become more acidic. And the sources
- 9:04say that acidification changes how certain microscopic
- 9:07sea creatures form their shells? Yes, it fundamentally
- 9:10alters their biology. So when those trillions
- 9:14of creatures die and fall to the ocean floor,
- 9:17the actual makeup of that sediment is changed.
- 9:20Future geologists will see a sudden, really sharp
- 9:23shift in the chemical composition of the limestone
- 9:26and chalk that's forming right now. That is just,
- 9:28wow. So we are changing the air, which changes
- 9:31the water, which changes the mud, which eventually
- 9:33becomes the stone. It's like this domino effect
- 9:36of permanence. It really is. Everything is connected.
- 9:38But, okay. One of the most memorable details
- 9:41from the source material, for me anyway, is the
- 9:43fingerprint of agriculture. I was just totally
- 9:46fascinated by how industrial farming is going
- 9:49to look to a paleontologist. Two million years
- 9:51from now. Oh, the fossil record of the present
- 9:53day is going to look incredibly strange to them.
- 9:55I mean, future paleontologists will find this
- 9:58overwhelming, globally distributed presence of
- 10:00billions of domestic animals. Specifically cows,
- 10:03pigs, and chickens, right? Yes, specifically
- 10:05them. The sheer biomass of domestic animals completely
- 10:08dwarfs all wild mammals and birds today. The
- 10:11stat that blew my mind was the chickens. We are
- 10:14essentially laying down a global layer of chicken
- 10:17bones. Yeah, it sounds almost funny, but it's
- 10:19true. Because of the incredible scale of industrial
- 10:22poultry farming, the modern broiler chicken is
- 10:25actually the most numerous bird on the planet.
- 10:27Its bones are going to be absolutely everywhere
- 10:29in the fossil record. Just a global stratum of
- 10:32chicken bones. That is crazy to think about.
- 10:36And right alongside those bones, you have the
- 10:38chemical footprint of farming. Our use of artificial
- 10:42fertilizers has been so extensive that we have
- 10:45actually doubled the natural flow of elements
- 10:47like nitrogen and phosphorus through the environment.
- 10:50Doubled it. Globally. Yeah. Those chemicals run
- 10:53off our fields, they enter the river systems,
- 10:55and they settle into the sediment. So that massive
- 10:57chemical spike will also be permanently locked
- 11:00into the rock. Okay, I also want to make sure
- 11:02we bring up the 1950s atomic tests. Because of
- 11:05all the evidence in the source material, this
- 11:06seems like the most dramatic piece. Oh, it is
- 11:09arguably the sharpest marker of all of them.
- 11:11In the mid -20th century, humanity began detonating
- 11:14nuclear weapons above ground. Right, the atmospheric
- 11:17tests. Yeah. And those tests sprinkled radioactive
- 11:19isotopes worldwide within a span of just a few
- 11:22short years. And just to clarify for everyone,
- 11:24an isotope is basically a variant of an element
- 11:27that has extra neutrons, which makes it unstable
- 11:29and radioactive, right? Yes, exactly. And the
- 11:32key thing for geology is that they decay at a
- 11:35very specific predictable rate. So they act like
- 11:38a built -in clock in the rock. Oh, that's incredibly
- 11:41useful for future scientists. It is. When future
- 11:44geologists examine our layer, they won't just
- 11:46see a gradual shift in chemistry like with the
- 11:49carbon cycle. They will see a razor -sharp global
- 11:52marker of radioactive isotopes like plutonium
- 11:55-239 that just suddenly appear everywhere all
- 11:58at once. So if we take all of this together,
- 12:00the techno fossils from plastic, the sheer volume
- 12:03of concrete, the chemical shift from carbon fertilizers,
- 12:06the global layer of chicken bones and the radioactive
- 12:09fallout. I mean, these create exactly the kind
- 12:12of clear, global, lasting signals that geologists
- 12:15use to mark the boundaries of deep time. They
- 12:18really do. The evidence points to a massive planetary
- 12:21transition. The end of an epoch is almost always
- 12:24marked by something sudden and dramatic in the
- 12:27rock. Like we mentioned earlier, the asteroid
- 12:29impact that ended the age of the dinosaurs. Right.
- 12:32Except in this case, the geological force reshaping
- 12:35the biosphere isn't coming from space. The cause
- 12:38is us, which, and this is where the story gets
- 12:40really interesting, leads us to a fascinating
- 12:43scientific plot twist. Yeah, the plot twist.
- 12:47Because with all this staggering planet -wide
- 12:49evidence, you would naturally assume that declaring
- 12:52the Anthropocene an official epoch is just a
- 12:54settled fact. You'd think the textbooks are already
- 12:56being updated. You would think so, yes. But science
- 12:58requires rigorous honesty, and as of right now,
- 13:01based on the sources we're looking at, the Anthropocene
- 13:03is actually not an officially recognized division
- 13:06of geological time. No, it is not. The International
- 13:09Scientific Bodies The specific committees of
- 13:12stratigraphers who formerly governed the geological
- 13:14timescale, they actually recently declined to
- 13:17ratify the Anthropocene as a new epoch. Wait,
- 13:20really? So they voted it down. I think this is
- 13:23where the scientific community is actually fractured
- 13:25right now, which is just fascinating, because
- 13:27it's crucial to understand that the formal rejection
- 13:29by these committees is absolutely not a group
- 13:32of scientists saying humans aren't having an
- 13:34impact. Oh, no, not at all. Let's be very clear
- 13:37about that. The broad scientific reality of human
- 13:40transformation is completely undisputed by these
- 13:43groups. No one is denying what's happening to
- 13:46the environment. OK, so if the evidence is literally
- 13:49written in concrete and radiation, why isn't
- 13:52it official yet? What is the debate actually
- 13:54about? The debate entirely centers on the nuance
- 13:57of how geology actually works as a bureaucratic
- 14:01and scientific discipline. Administrative rules,
- 14:03basically. Exactly. To create an official epoch,
- 14:06you cannot just point to a general trend of environmental
- 14:08change and say, look, things are different. The
- 14:11rules of stratigraphy require strict, very rigid
- 14:14thresholds. globally agreed upon starting marker
- 14:19in the rock. Oh, I read about this. In geology,
- 14:22this is affectionately called a golden spike,
- 14:24right? Yes, a golden spike. Or, if you want the
- 14:28official term, a global boundary stratotype section
- 14:31and point. I think we'll stick with Golden Spike,
- 14:34but that is a literal specific location on Earth,
- 14:37isn't it? Like maybe a specific cliff face in
- 14:39Italy or a lake bed in Canada. Right. It's a
- 14:42real place where geologists can point to one
- 14:45exact millimeter of rock and say, right here
- 14:47at this specific line, the epoch officially began.
- 14:51So that level of precision has to be the heart
- 14:54of the problem here. It is. Finding a single
- 14:57synchronous marker for human impact is incredibly
- 15:00difficult. Why? Because human history is terribly
- 15:03messy and asynchronous. Right. We didn't all
- 15:05do the same things at the exact same time. Exactly.
- 15:08For example, some scientists argue the Anthropocene
- 15:10should start with the agricultural revolution
- 15:12thousands of years ago. Because, you know, that's
- 15:15when we started clearing forests en masse and
- 15:17raising methane -producing livestock. But the
- 15:19agricultural revolution didn't happen everywhere
- 15:21at once. It took thousands of years to spread
- 15:24across the globe. So it doesn't leave a clean,
- 15:26single line in the global rock record. Precisely.
- 15:30Other scientists argue it should start with the
- 15:32Industrial Revolution in the 1800s when we started
- 15:34burning coal. But again, industrialization was
- 15:37gradual. It was regional. So what did the group
- 15:40pushing for the Anthropocene propose? They argued
- 15:43that the best golden spike is actually the radioactive
- 15:45fallout from those 1950s atomic tests we talked
- 15:48about. Because it is sudden, it is global, and
- 15:51it leaves a permanent chemical line everywhere
- 15:53simultaneously. Okay, but if you use the 1950s
- 15:57as the official starting line for the Anthropocene,
- 15:59you're essentially telling the historical record
- 16:02that all the massive human impacts before 1950
- 16:05don't count as part of the human epoch. And that
- 16:08is the exact tension that caused it to be voted
- 16:11down. It ignores thousands of years of deforestation,
- 16:13the extinction of countless species, the entire
- 16:16Industrial Revolution. Right. The stratigraphers
- 16:18voting against it were making a careful, highly
- 16:21technical judgment. They felt that pinning the
- 16:24entire human transformation of Earth to a single
- 16:26date in the 1950s was just too restrictive. It
- 16:29didn't accurately reflect the long... really
- 16:32complex history of our interaction with the planet.
- 16:34So they were basically arguing over administrative
- 16:37boundary lines, not denying the reality of what
- 16:40we are doing to the Earth. Yes, exactly. The
- 16:43analogy from the source material that perfectly
- 16:45summarizes this administrative tension is thinking
- 16:48about a house renovation. Oh, the house analogy
- 16:50is great. Yeah. So imagine a new family moves
- 16:54into an old house and immediately starts knocking
- 16:57down walls, tearing up the floorboards, painting
- 17:00everything neon green. Everyone in the neighborhood
- 17:03can clearly see the sledgehammers. The physical
- 17:06transformation of the house is totally obvious
- 17:08and undeniable. Down at the city council. Right.
- 17:12Down at the city council, the bureaucrats are
- 17:14locked in this heated, endless debate over the
- 17:17exact millisecond. The new residency officially
- 17:19began for tax purposes. Did it start when they
- 17:22signed the mortgage? when they move the first
- 17:24couch in, or when they knock down the first wall.
- 17:27And the paperwork of geology just requires a
- 17:29level of synchronous precision that makes the
- 17:32Anthropocene really difficult to formalize right
- 17:34now. But it's worth noting that even the scientists
- 17:38who opposed the formal designation still use
- 17:41the word Anthropocene. in their daily work. So
- 17:44it's still a highly relevant concept. Oh, very
- 17:46much so. They see it as a profoundly legitimate
- 17:49way to describe this age of human influence.
- 17:52They just don't think it fits neatly into the
- 17:54rigid filing cabinet of a formal geological epoch
- 17:57based on the current traditional rules. So the
- 18:00honest summary for you listening right now is
- 18:03this. The human impact on the Earth is real,
- 18:06it is actively being written in the stones, and
- 18:08it is widely accepted by the scientific community.
- 18:11The rigorous debate over how to categorize it
- 18:13is simply a reflection of scientists taking their
- 18:16discipline really seriously. Yeah, that's exactly
- 18:18the right way to frame it. Which brings us to
- 18:19the final piece of our deep dive today. Because
- 18:22whether or not the Anthropocene ever gets a formal
- 18:24golden spike on a chart somewhere, the deeper
- 18:27reality of this concept fundamentally changes
- 18:29our understanding of ourselves. It really does.
- 18:32We have to weigh human actions against the entirety
- 18:35of Earth's history. I mean, for almost all of
- 18:38that 4 .5 billion year timeline, the great forces
- 18:42shaping the planet were entirely blind and unthinking.
- 18:46Right. A dinosaur couldn't stop a wandering ice
- 18:48age. No. Early sea life couldn't halt the drifting
- 18:51of tectonic plates. Life just had to adapt to
- 18:54whatever the Earth blindly decided to do. But
- 18:56the source material highlights this awe -inspiring
- 18:59and honestly slightly terrifying fact. If you
- 19:02compress Earth's entire history into a single
- 19:0524 -hour clock, human beings show up in just
- 19:08the last few seconds before midnight. So a tiny
- 19:11blip. A tiny blip. Yet in that fraction of a
- 19:13fraction of time, our mining, our construction,
- 19:15and our agriculture now move more rock and soil.
- 19:18around the surface of the Earth than all the
- 19:21natural rivers combined. Think about that. A
- 19:23single species has joined the ranks of ice ages
- 19:26and tectonic plates. We have literally become
- 19:28a force of nature. And understanding the scale
- 19:31isn't just about, you know, memorizing facts
- 19:33to sound informed at a dinner party. The argument
- 19:35for science itself is that this knowledge allows
- 19:37us to see our own massive effects clearly. And
- 19:40to weigh them honestly. With that staggering
- 19:43planetary level power comes an incredible responsibility.
- 19:46Absolutely. The Anthropocene is essentially a
- 19:49mirror held up to our species. It's a geological
- 19:52record being written right now, today, about
- 19:55what we chose to do with our brief moment of
- 19:57enormous power. We are the very first species
- 20:00in the history of the entire planet to actually
- 20:02be aware that we are leaving a layer in the rock.
- 20:05We have the unique capability to study our own
- 20:07impact in real time. Which is an incredible privilege,
- 20:10but a huge burden. It is. Which leaves us with
- 20:14a final thought to mull over as you go about
- 20:16your day. Think back to that massive silent librarian
- 20:19we talked about at the very beginning of the
- 20:21deep dive, methodically recording everything
- 20:23in the Earth's stone diary. Still writing, even
- 20:26right now. Millions of years from now, if some
- 20:28future geologists, whatever they might look like,
- 20:31if they examine the rock layer we are leaving
- 20:33behind in this exact moment, what story will
- 20:36it tell? Will they see a chaotic, polluted layer
- 20:38of plastic and radiation that eventually stabilized
- 20:41and thinned out because we learned to balance
- 20:43our tremendous power? Or will the Anthropocene
- 20:46just be a thin, abrupt, devastating boundary
- 20:49line marking our sudden, dramatic end. It's quite
- 20:52a question to leave people with. It is. The geological
- 20:54record is still being written, and thankfully
- 20:56for now, the pen is still in our hands.