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If aliens came to Earth 100 millions years in the future, what traces would they find of long-extinct humanity's brief reign on the planet? This engaging and thought-provoking account looks at what our species will leave behind, buried deep in the rock strata, and provides us with a warning of our devastating environmental impact.
What would alien visitors in the far future, piecing together the history of earth, find of our brief reign? What clues will we leave? What fossils? Just as we have gained knowledge of the past, of ancient climates and the activities of creatures long dead, so too might they decode the rocks. The Earth After Us takes a novel approach to show how geologists unravel the information in the rocks. As the alien scientists start investigating the strata, what story will they tell of us? What kind of fossils will humans leave behind? What will happen to cities, cars, and plastic cups? How thick a layer will the 'human stratum' be? And will it be obvious which species dominated the planet?
"Every pebble has many stories to tell. Its particular atoms, its crystals, its minerals, its grains, its textures, its strata, its tiny fossils bear evidence to a history that stretches back billions of years."--Book flap.
Rocks, more than anything else, underpin our lives. They make up the solid structure of the Earth and of other rocky planets, and are present at the cores of gas giant planets. We live on the rocky surface of the planet, grow our food on weathered debris derived from rocks, and we obtain nearly all of the raw materials with which we found our civilization from rocks. From the Earth's crust to building bricks, rocks contain our sense of planetary history, and are a guide to our future. In this Very Short Introduction Jan Zalsiewicz looks at the nature and variety of rocks, and the processes by which they are formed. Starting from the origin of rocks and their key role in the formation of the ...
Reviews the evidence underpinning the Anthropocene as a geological epoch written by the Anthropocene Working Group investigating it. The book discusses ongoing changes to the Earth system within the context of deep geological time, allowing a comparison between the global transition taking place today with major transitions in Earth history.
Humankind has pervasively influenced the Earth’s atmosphere, biosphere, geosphere, hydrosphere and cryosphere, arguably to the point of fashioning a new geological epoch, the Anthropocene. To constrain the Anthropocene as a potential formal unit within the Geological Time Scale, a spectrum of indicators of anthropogenically-induced environmental change is considered, and shown as stratigraphical signals that may be used to characterize an Anthropocene unit, and to recognize its base. This volume describes a range of evidence that may help to define this potential new time unit and details key signatures that could be used in its definition. These signatures include lithostratigraphical (novel deposits, minerals and mineral magnetism), biostratigraphical (macro- and micro-palaeontological successions and human-induced trace fossils) and chemostratigraphical (organic, inorganic and radiogenic signatures in deposits, speleothems and ice and volcanic eruptions). We include, finally, the suggestion that humans have created a further sphere, the technosphere, that drives global change.
Presents a history of climate to reveal that the climatic changes happening hardly compare to the changes the Earth has seen over the last 4.5 billion years.
More than a decade ago, Nobel Prize-winning atmospheric chemist Paul Crutzen first suggested that we were now living in the Anthropocene, a new geological epoch in which human dominance of biological, chemical and geological processes on Earth was already an undeniable reality. Crutzen's ideas inspired Christian Schwagerl to do further documentation and to write this stimulating book. Well-equipped to take on such a task, Schwagerl has been a political, science and environmental journalist for more than 20 years. He first studied biology at the University of Berlin, completing his Master of Science degree at the University of Reading (UK). He is a past winner of the Georg von Holtzbrinck Prize for Science Journalism, the IUCN-Reuters Media Awards for excellence in Environmental Reporting (Category Europe, together with Philip Bethge and Rafaela von Bredow) and the Econsense Journalism Award for sustainability.
In this book, geologists Jan Zalasiewicz and Mark Williams consider the deep history of oceans, how and when they may have formed on the young Earth - topics of intense current research - how they became salty, and how they evolved through Earth history.