Scientific Expedition // 2018

Surveying the Late Devonian Mass Extinction in Mongolia

Connecting the dots on climate change through the Late Devonian Mass extinctions

Introduction

 

In 2018, I accompanied a team of geologists and researchers to the Gobi-Altai desert. Their research into the late Devonian mass extinctions more than 350 million years ago has many implications on our understanding of how climate change is affecting ecosystems across the planet now.

In partnership with The Explorer’s Club and The National Geographic Society, I was afforded the opportunity to photograph these heroes of science, and help fulfill one of my goals: to elevate the standing of scientists and explorers through photography.

The Team

A small group from Appalachian State University
set out to study, document, and catalogue geological findings from the Late Devonian Period. With colleagues from the Institute of Paleontology and Geology, Mongolian Academy of Science, the team spent several weeks in the remote region of the Gobi-Altai Desert.

The Campsite

After several days of arduous travel by plane and off-roading SUVs, we found ourselves nestled in a verdant valley situated between the Gobi Desert and the Altai Mountain range. From our campsite, the desert and undulating hills seemed to fade infinitely into the horizon–a truly humbling feeling. The scale and remoteness of the place felt alien, and it was here that we would set up camp for three weeks.

The Field Site

The area you see here was at the shore near an ancient volcano. Over the millennia it was mostly under water, but also sometimes exposed to the elements, and has shifted onto its side through tectonic plate movements. Perfect conditions for Geologists to study! This ‘section’ has a varied history, perfect for learning about how life on earth changed as time progressed.

365 million years ago (roughly)…

This area was teeming with life, but as organisms die their bodies, along with soot & ash from volcanic eruptions, sink to the bottom of the ocean and fossilize into distinct layers over time. The area you can see below represents several millions of years of deposits.

Mapping by Kilometer

 

This ‘section’ forms only a small part of the larger picture of what happened in this area around 365 millions years ago. As we are looking at the effect that a nearby volcano had on creating the mass extinction, it was important to understand the geological make up of the surrounding region. Imagine standing in Times Square and trying to get a sense of what it would have looked like 100 years ago. Here we do that for 100s of millions of years in the past!

To do this, the team trecked on foot up and down the surrounding mountains and the valleys (and in the process also scouted the fantastic shoot locations I ended up using for the individual portraits).

Mapping by Meter

 

Over time, Geological processes have the power to transform a landscape. For example, seasonal mountain runoff deposits new material over a fairly short period of time. To understand the rough age and layout of a section, it is necessary to walk and take a meter by meter reading of the surrounding area.

If the kilometer mapping is done by climbing a hill and looking out from it’s apex, meter mapping is done by walking around and kicking rocks.

Mapping by Centimeter

 

At this scale, almost all of a geologists work is done in the classic squat pose. A real challenge for a portrait photographer, you really start to get a ‘down to the ground’ perspective of the work. The centimeter work is done close to the ground, doing a thorough forensic analysis of each layer of deposit (strata). This is the real meat and potatoes of the work.

Each layer is sampled and will be transported to a lab for chemical analysis. This is the work that shows gives us a concrete sense of how deposits changed over time.

This is where you find out, for example, that a species of algae may have taken over an ecosystem, or that a species of choral has gone extinct.

The Fossils

Fossils are the key to unlocking the whole mystery. The final piece that puts the puzzle together. Father and son team Johnny and Will Waters took charge of this meticulous work. Without them, there’s really no way to know about species loss.

It was fascinating to see them work and identify species, and seeing how these ancient organisms have evolved over time, and seeing fossils of species that don’t exist anymore at all.

It’s All About the Algae

 

The Algae tells the whole story.

But first, remember when I told you to pay attention to the layer of lighter material?

Eagle-eyed observers will see that there’s a couple other thinner layers of the same, left of the big strip. Every one of these light-colored stripes was a volcanic eruption, spanning many years, each pushing the ecosystem to the brink, but never causing a mass extinction. Until the big, thick layer of Ash that’s so clearly visible even from a drone shot…

We know the Devonian Mass Extinction happened over millennia, but there was one main event. Until now it had never been clearly defined.

The algae give us a huge clue. While the fossil record shows that diversity was decreasing throughout the period, the biggest change came after a huge layer of algal deposits.

We’ve all heard of an ‘Algal Bloom’, when Algae takes over and grows at an exponential pace in the ocean. It happens when ecosystems collapse and Algae takes advantage of what’s left.

Because the Algae has few predators and feeds on all the nutrients and oxygen in the ocean, it causes all other species to literally choke, causing an extinction.

All those millions of years ago, there was very little land-based life, and most species lived in the oceans. This is why the Devonian Mass Extinction, which caused death in the oceans, had such an effect on all life on earth.

 
 

Why it Matters

 

The conditions created by the Algal bloom is called Anoxia which literally means ‘no oxygen’.

Anoxia is happening again in our oceans. These days fertilizer run-off from farming, as well as ecosystem collapse, algal blooms and other factors cause Ocean anoxia in regions across the planet. These can have huge effects as our planet’s climate changes.

In the fossil record in Mongolia, there’s proof of many small extinction events, which eventually resulted in a catastrophic collapse of the ecosystem.

It is important to learn lessons from the past, and this research into the Devonian Mass Extinction give us important clues about how man-made climate change is playing out.

The Local People

High above our home base, tucked into the valleys near the Chinese border, lives a couple of military families. They agreed to let me photograph them a couple of times, including portraits with the camels onto which one of them was loading their belongings, ready to move to a new spot.

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