A New History of Life

Begin the story of life on Earth with an overview of the unifying idea that will govern your exploration. Called Earth system science, this approach views Earth as an integrated network comprising the lithosphere, hydrosphere, atmosphere, and biosphere. Sample the complex interactions between these realms.

How was the great antiquity of Earth discovered? Survey the observations that led to the concept of deep time and, in the process, developed the tools that can read the story in rocks. End with a striking analogy that puts human time into perspective.

Delve into biostratigraphy, the study of fossil sequences in rock strata. The discovery that different layers of rock are characterized by distinctive fossils solved the problem of correlating sedimentary strata from different regions. This led to the geological time scale, initiating a revolution in Earth science.

Learn how paleontologists interpret fossils to reconstruct the traits and environments of extinct life forms. Examine some of the pitfalls of the field, including cultural biases that can lead to doubtful conclusions, such as that Tyrannosaurus rex was as terrible as depicted in the movies.

The history of science is marked by ideas that were before their time. One of the most important was Alfred Wegener's concept of continental drift, which was revived in the theory of plate tectonics. Explore the role that fossils played in this original grand unifying theory of geology.

Turn back the clock to Earth's earliest epoch, focusing on these questions: How did the solar system form and why do we live on a layered, differentiated planet? What do these events and the formation of the moon have to do with the evolution and development of life on Earth?

Investigate the origin of Earth's ocean. Then track down the oldest rocks on the planet, which shed light on the first continents. Also explore the nature of Earth's primordial atmosphere and why we are surrounded by a thick blanket of air despite periodic blasts of charged particles from the sun.

Probe possible scenarios for the origin of life, from the "warm little pond" filled with organic compounds that Charles Darwin envisioned, to deep ocean environments energized by volcanic vents. Sharpen the search by defining the properties that the earliest life must have had.

Did Martian meteorites seed the young Earth with simple life forms? Investigate this intriguing hypothesis. Then embark on a quest for Earth's oldest fossils, exploring their connection to organisms still found on the planet today, some of them hidden deep within the crust.

Trace the perils of life on the early Earth. Having survived a seething period of volcanism and a withering bombardment by asteroids, bacteria-like organisms flourished and began to transform the planet. Learn how their success was almost their undoing.

Follow the clues that suggest Earth went through a snowball phase around 635 million years ago, nearly ending life's story. How did it happen? How was it reversed? And above all, how did photosynthetic life survive if it was trapped beneath the ice for millions of years?

Make the transition to multicellular life, which grew in complexity as oxygen levels increased in the atmosphere, supporting creatures with more intricate metabolisms. This portion of the fossil record long eluded paleontologists, partly because few expected to find signs of life in ancient Precambrian rock.

The Cambrian period is notable for its immense variety of animals with many different body plans. In an explosion of diversification, shells, teeth, eyes, and other innovations emerged as creatures competed in an evolutionary arms race. Investigate the key factors driving this transformation.

In 1909, paleontologist Charles Walcott chanced on one of the most remarkable fossil finds in history: the Burgess Shale in the Canadian Rockies. Tour some of this quarry's astonishing specimens, which brought the world of the Cambrian explosion to vivid life.

Survey fossils that are often neglected in popular accounts of the history of life. Begin with corals and the reefs they build, which were teeming with invertebrates hundreds of millions of years ago. Then turn to micropaleontology, which is one of Professor Sutherland's research areas.

Earth's fossil record is punctuated with episodes when large fractions of all species abruptly disappeared. Examine the distinction between background extinction and mass extinction. Then look for factors that lead to these periodic catastrophes, and search beyond Earth for a possible explanation.

Five mass extinctions have occurred in the last 500 million years. Focus on the first of these, which extinguished the tropical paradise that flourished in the Ordovician period. Did plate tectonics initiate this radical transformation? Or could the cause have been extraterrestrial?

Consider the adaptations needed to make the transition from the buoyant, nourishing realm of water onto the perilous dry land, with its temperature extremes and relentless pull of gravity. Plants and animals each evolved unique adaptations to make this daring leap.

Search for the earliest vertebrates, which arose from chordates-animals with a rod-shaped notochord. Also probe the mystery of an extinct chordate called the conodont, which is valuable in oil exploration. Finally, discover why we have calcium phosphate skeletons.

The first vertebrates were easy targets for killer arthropods and other marine predators. What eventually gave them the upper hand? Trace the circuitous evolution of jaws and the rapid development of fish that followed. Also crucial was the internal skeleton, which has some surprising advantages.

How did vertebrates make the leap from water to land? Follow the quest for evolutionary transitional forms for land-dwelling vertebrates, focusing on the competing theories of gradualism and punctuated equilibrium. The answer to the puzzle may lie in a transitional environment between water and land.

Hunt for the fishapod—the missing link between fish and four-limbed vertebrates, or tetrapods. Begin by investigating some "living fossils," including the celebrated Coelacanth. Then join the expedition led by paleontologist Neil Shubin that discovered Tiktaalik, a fossil fishapod that made worldwide headlines.

Most of the world's coal deposits were laid down in the Carboniferous period, about 300 million years ago. Tour the global environment that created this unique formation and spawned many evolutionary innovations, including the amniotic egg. Also, discover why insects were much larger then than today.

Search for the origin of amniotes, which are egg-laying tetrapods, such as reptiles. Delve into the history of classification systems for life. The Linnaean system is based on resemblances between organisms. Learn why the more recent cladistic system, based on shared characteristics, implies that there is no such thing as a reptile.