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Dymocks - The Medea Hypothesis by Peter Ward

Is Life on Earth Ultimately Self-Destructive?, The Medea Hypothesis, Peter Ward, Princeton University Press"

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Peter Ward: The Medea Hypothesis - VidInfo

Several lines of evidence have converged and more evidence is regularly amassed, which is telling a story of dramatic and rapid climate change spurring vegetation changes that initiated evolutionary adaptations in the cradle of humanity. Sediment cores off of East Africa in the Arabian Sea, land sediment records in East Africa, combined with studies of carbon-12/13 ratios of fossil teeth, are telling an interesting and familiar tale of human origins. Three mya, as Earth was moving toward an ice age and the climate dried, the familiar grasslands of the appeared for the first time. Cgrasses have higher proportions of carbon-13, and so will animals that eat them. The expanding Cgrasslands coincided with the disappearance of Lucy's species and the appearance of the robusts that (or perhaps eating animals that ate those plants), probably from those expanding grasslands.

Peter Ward: Life and Work, Medea Hypothesis, …

The (c. 5.3 to 2.6 mya) began warmer than , but was the prelude to today’s ice age, as temperatures steadily declined. An epoch of less than three million years reflects human interest in the recent past. Geologically and climatically, there was little noteworthy about the Pliocene (although the was created then), although two related events made for one of the most interesting evolutionary events yet studied. South America kept moving northward, and the currents that once in the Tethyan heyday were finally closed. The gap between North America and South America began to close about 3.5 mya, and by 2.7 mya the current land bridge had developed. Around three mya, the began, when fauna from each continent could raft or swim to the other side. South America had been isolated for 60 million years and only received the stray migrant, such as rodents and New World monkeys. North America, however, received repeated invasions from Asia and had exchanges with Europe and Greenland. North America also had much more diverse biomes than South America's, even though it had nothing like the Amazon rainforest. The ending of South America’s isolation provided the closest thing to a controlled experiment that paleobiologists would ever have. South America's fauna was devastated, far worse than European and African fauna were when Asia finally connected with them. More than 80% of all South American mammalian families and genera existing before the Oligocene were extinct by the Pleistocene. Proboscideans continued their spectacular success after leaving Africa, and species inhabited the warm, moist Amazonian biome, as well as the Andean mountainous terrain and pampas. The also invaded and thrived as a mixed feeder, grazing or browsing as conditions permitted. In came cats, dogs, camels (which became the ), horses, pigs, rabbits, raccoons, squirrels, deer, bears, tapirs, and others. They displaced virtually all species inhabiting the same niches on the South American side. All large South American predators were driven to extinction, as well as almost all browsers and grazers of the grasslands. The South American animals that migrated northward and survived in North America were almost always those that inhabited niches that no North American animal did, such as monkeys, (which survived because of their claws), and their small cousins (which survived because of their armor), , and (which survived because of their quills). The opossum was nearly eradicated by North American competition but survived and is the only marsupial that made it to North America and exists today. One large-hoofed herbivore survived: the . The (it weighed one metric ton!) survived for a million years after the interchange. , that , also survived and migrated to North America and lasted about a million years before dying out. In general, North American mammals were , which resulted from evolutionary pressures that South America had less of, in its isolation. They were able to outrun and outthink their South American competitors. South American animals made it past South America, but none of them drove any northern indigenous species of note to extinction.

The Medea Hypothesis by Peter Ward | LibraryThing

The Medea Hypothesis by Peter Ward | Waterstones

Janet Hunt visited St Anne’s School in Welton, East Yorkshire today, 7th March 2014, to deliver a one day Handling People with Special Needs Education refresher course. Peter and Anne from the school were joined by Graeme Oxtoby from Fredrick Holmes School and Jayne Ward, Julie Venus and Leanne Newton all from Ganton Special School. Brilliant comments received from all who attended including “Trainer made it interesting and fun, a good mix of theory and practical sessions” and “Janet Hunts training style is excellent

Janet Hunt visited St Anne’s School in Welton, East Yorkshire today, 7th March 2014, to deliver a one day Handling People with Special Needs Education refresher course. Peter and Anne from the school were joined by Graeme Oxtoby from Fredrick Holmes School and Jayne Ward, Julie Venus and Leanne Newton all from Ganton Special School.

The Medea Hypothesis, Peter Ward | ISBN …

The Medea Hypothesis by Peter Ward Hardcover Book, 180 pages Description

In "The Medea Hypothesis", renowned paleontologist Peter Ward proposes a revolutionary and provocative vision of life's relationship with the Earth's biosphere - one that has frightening implications for our future, yet also offer ...

Asteroid strikes get all the coverage, but “Medea Hypothesis” author Peter Ward argues that most of Earth’s mass extinctions were caused by lowly bacteria. The culprit, a poison called hydrogen sulfide, may have an interesting application in medicine.

Peter Ward (paleontologist) | Wiki | Everipedia
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BBC - Earth - How long will life survive on planet Earth?

In Paleocene oceans, sharks filled the empty niches left by aquatic reptiles, but it took coral reefs ten million years to begin to recover, . As Africa and India moved northward, the shrank, and in the late Paleocene and early Eocene, one of the last Tethyan anoxic events laid down Middle East oil, and the last Paleocene climate event is called the (“PETM”). The PETM has been the focus of a great deal of recent research because of its parallels to today’s industrial era, when carbon dioxide and other greenhouse gases are massively vented to the atmosphere, causing a warming atmosphere and acidifying oceans. The seafloor communities suffered a mass extinction and the PETM’s causes are uncertain, but the when the global ocean warmed sufficiently is a prominent hypothesis. Scientists also look to the usual suspects of volcanism, changes in oceanic circulation, and a bolide impact.

Die Off - OVERSHOOT LOOP: Evolution Under The …

When sea levels rise as dramatically as they did in the Cretaceous, coral reefs will be buried under rising waters and the ideal position, for both photosynthesis and oxygenation, is lost, and reefs can die, like burying a tree’s roots. About 125 mya, reefs made by , which thrived on , began to displace reefs made by stony corals. They may have prevailed because they could tolerate hot and saline waters better than stony corals could. About 116 mya, an , probably caused by volcanism, which temporarily halted rudist domination. But rudists flourished until the late Cretaceous, when they went extinct, perhaps due to changing climate, although there is also evidence that the rudists . Carbon dioxide levels steadily fell from the early Cretaceous until today, temperatures fell during the Cretaceous, and hot-climate organisms gradually became extinct during the Cretaceous. Around 93 mya, , perhaps caused by underwater volcanism, which again seems to have largely been confined to marine biomes. It was much more devastating than the previous one, and rudists were hit hard, although it was a more regional event. That event seems to have , and a family of . On land, , some of which seem to have , also went extinct. There had been a decline in sauropod and ornithischian diversity before that 93 mya extinction, but it subsequently rebounded. In the oceans, biomes beyond 60 degrees latitude were barely impacted, while those closer to the equator were devastated, which suggests that oceanic cooling was related. shows rising oxygen and declining carbon dioxide in the late Cretaceous, which reflected a general cooling trend that began in the mid-Cretaceous. Among the numerous hypotheses posited, late Cretaceous climate changes have been invoked for slowly driving dinosaurs to extinction, in the “they went out with a whimper, not a bang” scenario. However, it seems that dinosaurs did go out with a bang. A big one. Ammonoids seem to have been brought to the brink with nearly marine mass extinctions during their tenure on Earth, and it was no different with that late-Cretaceous extinction. Ammonoids recovered once again, and their lived in the late Cretaceous, but the end-Cretaceous extinction marked their final appearance as they went the way of and other iconic animals.

Changes in Forced Expiratory Volume in 1 Second over …

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