Evolution (US Blad)

GIANTS FROM THE SWAMPS

CARBONIFEROUS PERIOD

Wet and warm swamps spread along the equator. They were habitats for gigantic flying insects and for the first vertebrate animals that lived entirely outside of water.

358 M YA and onwards

SWAMPS FORMED THE CARBONIFEROUS COAL

Seed fern

The dominant swamp plants were tree-sized club mosses and ferns. Once the plants died, they decayed, were buried, and slowly turned into coal. Since the 18th century, coal has been mined and burned to create electricity and heat homes.

Calamites trees (horsetails) Psaronius, tree fern

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Developing embryo Liquid-filled sac Egg casing

340 M YA

A PRIVATE POND

Land vertebrates evolved an exciting evolutionary step—the amniotic egg. This egg had a casing with a liquid-filled sac inside that allowed the developing young to float. The evolution of the amniotic egg freed vertebrates from the water and allowed them to take advantage of habitats on land. This process was similar to how plants evolved to live on land.

About 348 M YA STEP-BY-STEP

The transition of some vertebrate animals from water to land was a gradual process, but by the Early Carboniferous, the first fully land-living vertebrates had evolved. These vertebrates had strong limbs and backbones that could support their bodies out of water. Having eyes on top of their heads also helped to improve their vision on land.

The largest dragonfly (Meganeura) had a wingspan of 27.5 inches (70 cm).

325 M YA

TAKING TO THE SKIES

Although insects already existed by the Devonian, during the Carboniferous they formed many new species and spread far and wide. Insects were the first animals to evolve flight.

Delitzschala is the oldest known winged insect and had a wingspan of around 1 inch (2.5 cm).

PIONEERING PEOPLE

About 323.2–298.9 MYA

GIANT INSECTS AND OTHER ARTHROPODS

During this period, some arthropods (creatures with an exoskeleton) were enormous and there are several theories as to why this happened. Scientists know that there were higher levels of oxygen in the atmosphere at the time, most likely caused by the photosynthesis from the widespread swamp plants. So one theory is that this oversupply of oxygen allowed insects and other arthropods to evolve larger bodies. Another theory is that there were no flying predators to spot and eat the ones that grew larger.

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305 M YA and onwards

THE COAL SWAMPS COLLAPSE

Over a long time, dead swamp plants gathered and were fossilized as coal. They became a natural storage for carbon dioxide, preventing it from being released into the atmosphere. Less carbon dioxide in the atmosphere led to global cooling (again!). Glaciers spread and almost reached the equator. With more water locked up as ice, the sea level dropped. At the same time, the continents moved closer together, the climate became drier, and the lush swamps gradually shrank. Many plants died out, including the tree-like horsetails.

The scorpion Pulmonoscorpius was up to 27.5 inches (70 cm) long.

Eryops

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300 M YA MIGHTY PREDATORS

Amphibians were among the first vertebrates that lived most of their lives on land. Modern amphibians are small creatures like frogs and toads, but they were once enormous. Like frogs today, they laid their eggs in water and their young had gills. These tadpoles transformed into adults with lungs to live on land.

Millipedes such as this Arthropleura grew to almost 8 feet (2.4 m) long.

was a 6.5-foot- (2-m-) long monster amphibian and a fierce meat eater that swallowed its prey whole.

ALFRED SHERWOOD ROMER (1849–1973) studied land-dwelling vertebrates, such as ancient amphibians and reptiles, and how they were related to each other.

Club mosses (Lepidodendron)

THE CAUSES OF CLIMATE CHANGE

Earth's climate has constantly changed throughout history. Climate describes overall weather conditions and patterns, like temperature and rainfall, which happen over a long time. Weather refers to a particular event, for example a sunny day or a storm. The changes in our climate have been caused by several natural processes and, more recently, by humans.

Some of the heat from the Sun bounces off Earth's surface.

THE MILANKOVITCH CYCLES

For the past three million years, Earth has been alternating between ice ages and warm periods. These periods are caused by changes in the Earth’s distance to the Sun, which affects the amount of sunlight that reaches the Earth. Some of these changes happen roughly in 100,000-year cycles called Milankovitch cycles.

PIONEERING PEOPLE

The Milankovitch cycles were named after MILUTIN MILANKOVITCH (1879–1958). He calculated how Earth’s orbit and the tilt of Earth’s axis changed the incoming heat of the Sun. This explained the causes of the ice ages and his calculations are still used today.

and heat from the Sun

Earth

HOW TO GET WARM

Earth is the right temperature for life because certain gases in the atmosphere hold in the Sun's heat, just like the glass in a greenhouse does. During Earth's history, these greenhouse gases, such as carbon dioxide and methane, were released by volcanic eruptions and other natural processes. When the amount of greenhouse gas went down, the Earth cooled. When the amount went up, the Earth got hotter.

1. The Earth's axis is always tilted, but the angle of tilt changes every 41,000 years. When the angle is larger, Earth's polar regions lean closer to the Sun, receiving more sunlight and heat in summer. When the angle is smaller, Earth leans away from the Sun and receives less sunlight and heat.

2. Earth’s axis also rotates and can wobble like a spinning top. This wobble also affects the angle of the Earth towards the Sun.

3. Earth’s orbit—the path that it takes around the Sun—has an effect too. Sometimes the orbit is circular, but sometimes it becomes more oval shaped, which brings Earth closer to and sends it farther away from the Sun.

ALBEDO EFFECT

Another thing that can affect Earth’s temperature, but that isn’t part of the Milancovitch cycles, is called the Albedo Effect. This happens when large areas of the Earth are covered with ice. Pale surfaces like ice or snow reflect more heat than dark, bare soil, so this ice causes the planet to cool down.

Greenhouse gases trap some of the heat in Earth's atmosphere.

Sun

EXTINCTION OF MEGAFAUNA

Climate change can have a big impact on biodiversity. For example, giant animals once roamed North America but became extinct around 10,000–45,000 years ago. Some scientists believe that this extinction was probably caused by climate change and others think that hunting by humans also contributed.

THE CURRENT CLIMATE CRISIS

Greenhouse gases occur naturally, but during the last 200 years, the level of two of these gases has dramatically increased. This is largely due to human activities. For example, the burning of fossil fuels (coal, oil and gas), for electricity, heating, and to power vehicles, releases carbon dioxide. Also the increasing demand for meat and dairy products means that more animals are farmed. These animals release digestive gasses (burps and farts), that include methane. The increase of these greenhouse gasses has led to the current climate crisis.

Mastodon

Ground sloth

Saber-toothed cat

Hagerman horse

Camelops

DINOSAURS IN CHARGE

TRIASSIC AND JURASSIC PERIODS

After the Permian mass extinction, many new living things evolved. While some reptiles invaded the sea, dinosaurs large and small started to conquer the land. Earthquakes and volcanic eruptions caused Pangaea to split in two. Large oceans began to form between these landmasses, which led to more rainfall as water evaporated along the newly formed coastlines.

251–145.5 MYA THE BIGGEST REPTILES OF THE SEA

One group of reptiles that could swim and hunt for fish to eat were called nothosaurs (251–200 MYA). They could also crawl onto land to warm up in the sun and lay eggs. Ichthyosaurs (251–65.6 MYA), however, spent all their lives in the water. They were the largest marine reptiles of all time, and they grew to around 65 feet (20 m) long—almost twice as long as a bus.

225–190 MYA THE FIRST DINOSAUR

Eoraptor was a 3-foot- (1-m-) long dinosaur with light, hollow bones. It was an agile hunter who preyed on insects and small reptiles.

WHAT IS A DINOSAUR?

Dinosaurs were a group of reptiles, but they had certain features that set them apart. Unlike most reptiles' legs, which were sprawled out to the sides, dinosaurs' legs were directly beneath their bodies, giving them an upright stance. These straight legs could support a heavier body and allow for swift movement. Dinosaurs lived on land and laid hard-shelled eggs. Some also had small, colored feathers.

Around 201 MYA

END-TRIASSIC MASS EXTINCTION

At the end of the Triassic, volcanic eruptions released massive amounts of greenhouse gases, causing sudden global warming. This led to the extinction of many animals. It is not known why, but dinosaurs survived. They would go on to become the dominant land animals of the Jurassic and Cretaceous.

Nothosaurus

Giraffatitan was about 42.5 feet (13 m) tall.

201–65 MYA ENORMOUS VEGETARIANS

Sauropods were the tallest dinosaurs that we know of. Plant eaters, such as Giraffatitan and Diplodocus, had extremely long necks for reaching leaves high in the treetops. Their constant munching changed Jurassic landscapes by creating open forests.

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PIONEERING PEOPLE

ANUSUYA CHINSAMY-TURAN (1962–present) studies dinosaur bones under the microscope. She found out that dinosaur bones show growth rings (just like trees do). By counting the rings, she came up with a system to estimate the age of individual dinosaurs.

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Diplodocus grew up to 98 feet (30 m) long.

Around 155–145 MYA

TOUGH PLATES

Stegosaurus was an herbivore that had bony plates along its back. The plates could have made the dinosaur appear larger and helped it to scare off predators. Or they could have been used to regulate its body temperature by warming its blood in the sunlight or releasing heat to cool down.

Around

200

MYA MINIATURE MAMMALS

Early mammals were very small. Morganucodon, for example, only grew to around 4 inches (10 cm) long. It had back teeth that interlocked when its jaw closed. This feature is shared by all mammals and allows them to chew their prey. Reptiles, on the other hand, are unable to chew and just gulp down their food.

Morganucodon

Cypress tree Monkey Puzzle

Cycad tree Stegosaurus

Ginkgo tree

DISCOVER THE STORY OF LIFE ON EARTH AND HOW IT CAME TO BE, WITH REAL-LIFE SCIENTISTS SARAH DARWIN AND EVA MARIA SADOWSKI.

The Earth has come a very long way from the molten planet with oceans of magma that existed 4.5 billion years ago. Since then, the land has shifted, the climate has changed, and life has flourished. But how exactly did living things come to be?

Let authors Sarah Darwin and Eva Maria Sadowski enlighten you about the fascinating facts of evolution: what it is and how it works. Dive into the history of life on Earth and learn about the theory of natural selection that Sarah’s great-great-grandfather, Charles Darwin, and naturalist Alfred Russel Wallace came up with together. In this beautifully illustrated book, feature spreads explain the important things that you need to know, and a timeline plots the history of life on Earth.

Nature lovers will be delighted by this in-depth tour of life that leaves no stone unturned and will keep children (and adults) enthralled for hours. Find out how plants, humans, pet dogs, and everything else came to be and what this might mean for our future.

Sarah Darwin and Eva Maria Sadowski

Olga Baumert

8–12 years

$24.99 / CAN $33.75 Hardcover 64 pages 10.2 x 11 inches

Pub Date: Sept 5th 2023 ISBN: 978-1-912920-54-9

BISAC Codes:

JNF037050 / Science & Nature / Fossils JNF051150 / Science & Nature / Zoology JNF037030 / Science & Nature / Flowers & Plants

KEY SELLING POINTS:

• Co-authored by Sarah Darwin, Charles Darwin’s great-greatgranddaughter, and Eva Maria Sadowski.

• Stunning, luscious artwork throughout brings each page to life with everything from bacteria to dinosaurs and giant fungi to gingko trees.

• Offers an in-depth look at evolution, helping curious kids understand and engage with the world around them.

AUTHOR BIO:

DR. SARAH DARWIN originally trained as an artist and then as a scientist, specializing in botany. She spent several years living and working in the Galápagos Islands and studying the Galápagos tomatoes there. More recently she has been part of a project in Berlin studying nightingales. Sarah is the great-great-granddaughter of Charles Darwin and works at the Museum Für Naturkunde, Berlin.

DR. EVA-MARIA SADOWSKI is a paleobotanist who mainly studies plant remains that are enclosed in amber. Eva lives in Berlin and works at the Museum Für Naturkunde, Berlin.

ILLUSTRATOR BIO:

OLGA BAUMERT is an artist, illustrator, and graphic designer. Originally from Poland, she studied Fine Art and Jewellery before moving to the UK, where she received her degree in Graphic Design and Illustration at De Montfort University. Olga currently lives and works in Leicester, UK.

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