Habitat Loss

See how human expansion and habitat loss has changed landscapes over millennia, and how this has impacted global diversity.

2 months ago

Latest Post Articles of Muslim Faith by Daniel Sanderson public


Human impacts have accelerated, but we have been transforming the planet for millenniaIN THIS SECTION

Humans have had such a profound impact on the planet’s ecosystems and climate that Earth might be defined by a new geological epoch: the Anthropocene (where “anthro” means “human”). Some think this new epoch should start at the Industrial Revolution, some at the advent of agriculture 10,000 to 15,000 years ago. This feeds into the popular notion that environmental destruction is a recent phenomenon.

The lives of our hunter-gatherer ancestors are instead romanticized. Many think they lived in balance with nature, unlike modern society where we fight against it. But when we look at the evidence of human impacts over millennia, it’s difficult to see how this was true.

Our ancient ancestors drove more than 178 of the world’s largest mammals (‘megafauna’) to extinction. This is known as the ‘Quaternary Megafauna Extinction’ (QME). The extent of these extinctions across continents is shown in the chart. Between 52,000 and 9,000 BC, more than 178 species of the world’s largest mammals (those heavier than 44 kilograms – ranging from mammals the size of sheep to elephants) were killed off. There is strong evidence to suggest that these were primarily driven by humans – we look at this in more detail later.

Africa was the least hard-hit, losing only 21% of its megafauna. Humans evolved in Africa, and hominins had already been interacting with mammals for a long time. The same is also likely to be true across Eurasia, where 35% of megafauna were lost. But Australia, North America and South America were particularly hard-hit; very soon after humans arrived, most large mammals were gone. Australia lost 88%; North America lost 83%; and South America, 72%.

Far from being in balance with ecosystems, very small populations of hunter-gatherers changed them forever. By 8,000 BC – almost at the end of the QME – there were only around 5 million people in the world. A few million killed off hundreds of species that we will never get back.

Did humans cause the Quaternary Megafauna Extinction?

The driver of the QME has been debated for centuries. Debate has been centered around how much was caused by humans and how much by changes in climate. Today the consensus is that most of these extinctions were caused by humans.

There are several reasons why we think our ancestors were responsible.

Extinction timings closely match the timing of human arrival. The timing of megafauna extinctions were not consistent across the world; instead, the timing of their demise coincided closely with the arrival of humans on each continent. The timing of human arrivals and extinction events is shown on the map.

Humans reached Australia somewhere between 65 to 44,000 years ago.1 Between 50 and 40,000 years ago, 82% of megafauna had been wiped out. It was tens of thousands of years before the extinctions in North and South America occurred. And several more before these occurred in Madagascar and the Caribbean islands. Elephant birds in Madagascar were still present eight millennia after the mammoth and mastodon were killed off in America. Extinction events followed man’s footsteps.

Significant climatic changes tend to be felt globally. If these extinction were solely due to climate we would expect them to occur at a similar time across the continents.

QME selectively impacted large mammals. There have been many extinction events in Earth’s history. There have been five big mass extinction events, and a number of smaller ones. These events don’t usually target specific groups of animals. Large ecological changes tend to impact everything from large to small mammals, reptiles, birds, and fish. During times of high climate variability over the past 66 million years (the ‘Cenozoic period’), neither small nor large mammals were more vulnerable to extinction.2

The QME was different and unique in the fossil record: it selectively killed off large mammals. This suggests a strong influence from humans since we selectively hunt larger ones. There are several reasons why large mammals in particular have been at greater risk since the arrival of humans.

Islands were more heavily impacted than Africa. As we saw previously, Africa was less-heavily impacted than other continents during this period. We would expect this since hominids had been interacting with mammals for a long time before this. These interactions between species would have impacted mammal populations more gradually and to a lesser extent. They may have already reached some form of equilibrium. When humans arrived on other continents – such as Australia or the Americas – these interactions were new and represented a step-change in the dynamics of the ecosystem. Humans were an efficient new predator.

There has now been many studies focused on the question of whether humans were the key driver of the QME. The consensus is yes. Climatic changes might have exacerbated the pressures on wildlife, but the QME can’t be explained by climate on its own. Our hunter-gatherer ancestors were key to the demise of these megafauna.

Human impact on ecosystems therefore date back tens of thousands of years, despite the Anthropocene paradigm that is this a recent phenomenon. We’ve not only been in direct competition with other mammals, we’ve also reshaped the landscape beyond recognition. Let’s take a look at this transformation.

Wilderness to farm: how humans have transformed the global landscape

Over the past 12,000 years humans have reshaped the world’s landscape from wilderness to farm. Our hunter-gatherer ancestors had a profound impact on other mammals, and minor impacts on land use through burning fires to clear land. But it wasn’t until the advent of agriculture that global land use really started to change.

Researchers at the History Database of the Global Environment (HYDE) reconstruct historical patterns of land use dating back millennia. The most recent reconstruction by Erle Ellis, Arthur Beusen and Kees Klein Goldewijk is shown in the chart.3

In 10,000 BC, 40% of Earth’s surface was completely wild and free from human influence – this consisted of pristine untouched forest, wild grasslands, shrubs and deserts. By this point at least 60% had been touched by humans in some way, here classified as ‘semi-natural land’. Semi-natural lands were inhabited but with only minor use for settlements or agriculture.

We began to see the first lands for pasture [with the beginnings of pastoralism, as we will see later] in 8,000 BC. Croplands appeared around 7,000 BC, followed by the rise of villages – densely populated agricultural settlements – around 6,000 BC.

Land used for farming – pasture and croplands – plus villages and much later, urban land, are collectively referred to as ‘used’ anthromes. It wasn’t until around 1,000 BC that ‘used’ anthromes reached 1% of Earth’s land. It was at this point that agriculture and human settlements were present across Mediterranean Europe, the Middle East, Africa and East Asia.

Humans very quickly became the dominant land user, reaching 5% of land use around the year 900; 10% by 1700; 25% by 1880; up to half of all land today.4

This came at an obvious cost to Earth’s ecosystems. We’ve lost one-third of all forests over the last 10,000 years. Wild grasslands and other natural habitats have been lost. And over the last few centuries more than half of semi-natural lands (with very sparse human influence) have become intensified.

Human demands for agriculture have transformed the global landscape. This has been a transition that dates back millennia, but has accelerated in recent centuries. To see how and where these changes occurred, let’s look at how agriculture spread across the world’s continents.

Country-by-country: how agriculture spread across the world

We’ve looked at the rise of global agriculture. But we’ve yet to see when and where these changes occurred.

To understand the history of populations and land use across the world, researchers built the ArchaeoGLOBE Project, a crowdsourcing approach which draws on archaeological expert knowledge country-by-country. Drawing on responses from 255 archaeologists with knowledge across 146 regions, Lucas Stephens et al. (2020) built a global picture of the extent and timing of foraging; pastoralism (animal agriculture); extensive and intensive agriculture; and urbanization.5 This dates back 10,000 years ago through to 1850.

Here they categorize land use across five categories:

Foraging: this includes the practices of foraging for foods such as fruit and wild plants; hunting and gathering wild animals; and fishing. It’s analogous to hunter-gatherers.

Pastoralism: this involves the management and raising of livestock including cattle, goats, sheep, chickens, pigs etc.

Extensive agriculture: this is where farmers grow crops but not continuously on the same plot of land. It includes farming approaches such as ‘slash-and-burn’ or ‘shifting cultivation’ where communities clear land to grow crops, then later abandon it to move elsewhere or leave it for several years to regenerate.

Intensive agriculture: this is continuous cultivation that is common of farming approaches in most high- and middle-income countries today. Cropland is managed year round, and annual harvests take place on the same plot of land.

Urbanization: the shift from rural areas with low population-density to population-dense urban centers.

The extent of these land uses were defined as ‘minimal’ (less than 1% of land area); ‘common’ (1 to 20% of land area) or ‘widespread’ (more than 20%).

In the maps we see the transition points for each of these land uses across the world. You can use the timeline at the bottom of each interactive chart to see how land uses changed over the course of millennia. For foraging, pastoralism, extensive and intensive agriculture, the dates of transition from none to minimal; common; then widespread use are shown. For urbanization, it’s the onset date of when cities became present.

10,000 years ago, foraging was still common across all regions. We shouldn’t underestimate the impact that these practices had on some ecosystems. Beyond the major decline in large mammals that we discussed earlier, hunter-gatherers had long-lasting impacts on many ecosystems even before the domestication of livestock and crops. Widespread use of fire increased greenhouse gas emissions, as well as altering water and vegetation cycles.

As we see, foraging communities began to shift towards pastoralism and extensive agriculture in Southwest Asia and the Mediterranean, as early as 10,000 years ago. By 8,000 to 6,000 years ago it had become commonplace. Pastoralism was particularly useful in arid regions where dry conditions made growing crops much more difficult. It therefore spread faster than extensive agriculture, becoming common across Northern Africa and Central Asia by 4,000 BP.  Southern Africa and Eurasia soon followed – embracing livestock before crop farming became common.

It wasn’t until 3,000 years ago that globally, extensive agriculture was more common than pastoralism. From there, the use of extensive and then intensive agriculture has continued to spread. Intensive farming (continuous cultivation of crops year after year) was constrained by climate to only a few regions – the Mediterranean, Southwest Asia, South Asia, and eastern China – until 2,000 years ago. But since then, it has rapidly become widespread across most of the world today.

Across most of the world, urbanization is a fairly recent phenomenon, playing only a minor role until the last few centuries. But some regions – across the Mediterranean, Central and Eastern Asia, and parts of Europe had their first cities thousands of years ago.

These maps show the spread of livestock and crop farming across the world. They represent the dispersal and growth of human populations, and continued effort to feed themselves. What’s hidden is the massive environmental changes that were occurring at every transition. As we saw earlier from the long-term changes in global land use, the expansion of agriculture came at the expense of forests and wild grasslands; and the rise of livestock created direct competition with other species.

To move forward we need to use less land for food, not more

Humans have been reshaping the planet for millennia. Food lies at the heart of this change: what we eat and how we get it. Earth has been transformed from a diverse wilderness to a giant man-made farm.

If we want to give land back to nature we need to reduce the amount of land we use for agriculture. While modern, intensive agriculture often gets a bad reputation it has been integral to sustaining the population we have today while saving land. Massive increases in crop yields means per capita land use for food today is much smaller than in the past.

To move forward we need this to continue: further increases in crop yields; less meat and dairy to reduce our demand for pasture; and more productive or selective livestock systems for the meat and dairy we do eat. Moving backwards towards low-density extensive agriculture or hunter-gatherer food production doesn’t work. Rather than making space for natural ecosystems to regenerate, they would continue to rob more and more species of their habitats.

Forest loss and deforestation


The world has lost one-third of its forests, but an end of deforestation is possible

Many people think of environmental concerns as a modern issue: humanity’s destruction of nature and ecosystems as a result of very recent population growth and increasing consumption. This is true for some problems, such as climate change. But it’s not the case for deforestation. Humans have been cutting down trees for millennia.

How much forest has the world lost? When in history did we lose it?

In the chart we see how the cover of the earth’s surface has changed over the past 10,000 years. This is shortly after the end of the last great ice age, through to the present day.6

Let’s start at the top. You see that of the 14.9 billion hectares of land on the planet, only 71% of it is habitable – the other 29% is either covered by ice and glaciers, or is barren land such as deserts, salt flats, or dunes. I have therefore excluded these categories so we can focus on how habitable land is used.

The bar chart just below shows the earth’s surface cover just after the end of the last ice age.7 10,000 years ago 57% of the world’s habitable land was covered by forest. That’s 6 billion hectares.  Today, only 4 billion hectares are left. The world has lost one-third of its forest – an area twice the size of the United States.

Only 10% of this was lost in the first half of this period, until 5,000 years ago. The global population at this time was small and growing very slowly – there were fewer than 50 million people in the world. The amount of land per person that was needed to produce enough food was not small – in fact, it was much larger than today. But a small global population overall meant there was little pressure on forests to make space for land to grow food, and as wood for energy.

If we fast-forward to 1700 when the global population had increased more than ten-fold, to 603 million. The amount of land used for agriculture – land to grow crops as well as grazing land for livestock – was expanding. You will notice in the chart that this was not only expanding into previously forested land, but also other land uses such as wild grasslands and shrubbery. Still, more than half of the world’s habitable land was forested.

The turn of the 20th century is when global forest loss reached the halfway point: half of total forest loss occurred from 8,000BC to 1900; the other half occurred in the last century alone. This emphasises two important points.

First, it reiterates that deforestation is not a new problem: relatively small populations of the past were capable of driving a large amount of forest loss. By 1900, there were 1.65 billion people in the world (five times fewer than we have today) but for most of the previous period, humans were deforesting the world with only tens or hundreds of millions. Even with the most basic of lifestyles compared to today’s standards, the per capita footprint of our ancestors would have been large. Low agricultural productivity and a reliance on wood for fuel meant that large amounts of land had to be cleared for basic provisions.

Second, it makes clear how much deforestation accelerated over the last century. In just over 100 years the world lost as much forest as it had in the previous 9,000 years. An area the size of the United States. From the chart we see that this was driven by the continued expansion of land for agriculture. By 1950, there was almost as much agricultural land as forest – 43% of habitable land. By 2018, this had increased to 46% while forests shrank to 38%. When we think of the growing pressures on land from modern populations we often picture sprawling megacities. But urban land accounts for just 1% of global habitable land. Humanity’s biggest footprint is due to what we eat, not where we live.

How can we put an end to our long history of deforestation?

This might paint a bleak picture for the future of the world’s forests: the United Nations projects that the global population will continue to grow, reaching 10.8 billion by 2100. But there are real reasons to believe that this century doesn’t have to replicate the destruction of the last one.

The world passed ‘peaked deforestation’ in the 1980s and it has been on the decline since then – we take a look at rates of forest loss since 1700 in our follow-up post. Improvements in crop yields mean the per capita demand for agricultural land continues to fall. We see this in the chart. Since 1961, the amount of land we use for agriculture increased by only 7%. Meanwhile, the global population increased by 147% – from 3.1 to 7.6 billion.8 This means that agricultural land per person more than halved, from 1.45 to 0.63 hectares.

In fact, the world may have already passed ‘peak agricultural land’ [we will look at this in more detail in an upcoming post]. And with the growth of technological innovations such as lab-grown meat and substitute products, there is the real possibility that we can continue to enjoy meat or meat-like foods while freeing up the massive amounts of land we use to raise livestock.

If we can take advantage of these innovations, we can bring deforestation to an end. A future with more people and more forest is possible.

Global deforestation peaked in the 1980s. Can we bring it to an end?

Since the end of the last great ice age – 10,000 years ago – the world has lost one-third of its forests.9 Two billion hectares of forest – an area twice the size of the United States – has been cleared to grow crops, raise livestock, and use for fuelwood.

In a previous post we looked at this change in global forests over the long-run. What this showed was that although humans have been deforesting the planet for millennia, the rate of forest loss accelerated rapidly in the last few centuries. Half of global forest loss occurred between 8,000BC and 1900; the other half was lost in the last century alone.

To understand this more recent loss of forest, let’s zoom in on the last 300 years. The world lost 1.5 billion hectares of forest over that period. That’s an area 1.5-times the size of the United States.

In the chart we see the decadal losses and gains in global forest cover. On the horizontal axis we have time, spanning from 1700 to 2020; on the vertical axis we have the decadal change in forest cover. The taller the bar, the larger the change in forest area. This is measured in hectares, which is equivalent to 10,000 m².

Forest loss measures the net change in forest cover: the loss in forests due to deforestation plus any expansion of forest through afforestation.10

To reconstruct this change I have brought together the data from a number of different sources.11 We’ve also differentiated between temperate forests (the sum of ‘boreal’ and ‘temperate’ areas), shown in green, and tropical forests (the sum of ‘tropical’ and ‘subtropical’ areas), shown in brown. It’s useful to make this distinction because – as we will see – where the world has lost forests has shifted.

The rate of forest loss changed a lot. From 1700 to 1850, 19 million hectares were being cleared every decade. That’s around half the size of Germany. From 1850 to 1920, losses were around 50% higher at 30 million hectares per decade –that’s like losing a forested area the size of Italy every 10 years. It was predominantly temperate forests that were being lost at this time. Population growth meant that today’s rich countries across Europe and North America needed more and more resources such as land for agriculture, wood for energy, and for construction.12

Moving into the 20th century there was a stepwise change in demand for agricultural land and energy from wood. Deforestation rates accelerated. From the 1920s through to the 1980s, decadal losses quadrupled to almost 120 million hectares. That’s equivalent to the area of South Africa. This increase was mostly driven by tropical deforestation as countries across Asia and Latin America followed the path of Europe and North America.

Global deforestation reached its peak in the 1980s. We lost 150 million hectares – an area half the size of India – during that decade. Clearing of the Brazilian Amazon for pasture and croplands was a major driver of this loss.

Since then, deforestation rates have steadily declined, to 78 million hectares in the 1990s; 52 million in the early 2000s; and 47 million in the last decade.

As we explore in more detail in our related article, countries tend to follow a predictable development in forest cover, a U-shaped curve.13 They lose forests as populations grow and demand for agricultural land and fuel increases, but eventually they reach the so-called ‘forest transition point’ where they begin to regrow more forests than they lose.

Within this global aggregated trend there are many forest transitions at local, national or regional levels occurring. We see one such transition in the chart: the forest loss in the temperate regions – shown as the green part of the bars – peaked much earlier than the global forest loss. In the first half of the 20th century, temperate forests reached their peak loss at 34 million hectares per decade, and by 1990 they had passed the ‘forest transition point’. For the past 30 years, temperate regions have seen a continued increase in forest cover through afforestation: you see this as the bars are now ‘positive’ (pointing upwards). Across temperate forests the world gained 6 million hectares in the last decade.

Tropical forests, on aggregate, have also passed peak deforestation in the 1980s – the longest of all bars – but have not passed the transition to reforestation. Some countries within this group are still far behind peak deforestation: without concerted effort to protect these forests it could be many decades before forests in those countries approach the transition point [as we show in a related post].14

The history of deforestation is a tragic one, in which we not only lost these wild and beautiful landscapes but also the wildlife within them. But, the fact that forest transitions are possible should give us confidence that a positive future is possible. Many countries have not only ended deforestation, but actually achieved substantial reforestation. It will be possible for our generation to achieve the same on the global scale and bring the 10,000 year history of forest loss to an end.

If we want to end deforestation we need to understand where and why it’s happening; where countries are within their transition; and what can be done to accelerate their progress through it. We need to pass the transition point as soon as possible, while minimizing the amount of forest we lose along the way.

Published 2 months ago