"Medea Hypothesis" author Peter Ward argues that most of Earth's mass extinctions were caused by lowly bacteria. The culprit, a poison called hydrogen sulphide, may have an interesting application in medicine.
Title: Short-term Effects of Gamma Ray Bursts on Earth Authors: Osmel Martín (UCLV, Cuba), Douglas Galante (IAG-USP, Brazil), Rolando Cárdenas (UCLV, Cuba), J.E. Horvath (IAG-USP, Brazil)
The aim of the present work is to study the potential short-term atmospheric and biospheric influence of Gamma Ray Bursts on the Earth. We focus in the ultraviolet flash at the planet's surface, which occurs as a result of the retransmission of the \gamma radiation through the atmosphere. This would be the only important short-term effect on life. We mostly consider Archean and Proterozoic eons, and for completeness we also comment on the Phanerozoic. Therefore, in our study we consider atmospheres with oxygen levels ranging from 10^{-5} to 1% of the present atmospheric level, representing different moments in the oxygen rise history. Ecological consequences and some strategies to estimate their importance are outlined.
Palaeontologists can still hear the echo of the death knell that drove the dinosaurs and many other organisms to extinction following an asteroid collision at the end of the Cretaceous Period 65 million years ago.
"The evolutionary legacy of the end-Cretaceous extinction is very much with us. In fact, it can be seen in virtually every marine community, every lagoon, every continental shelf in the world," said University of Chicago paleontologist David Jablonski. It is, he said, "sort of an echo of the big bang for evolutionary biology."
This conclusion followed a detailed global analysis of marine bivalves, one of the few groups plentiful enough in the fossil record to allow such a study, which was funded by the National Aeronautics and Space Administration. Andrew Krug of the University of Chicago, Jablonski and James Valentine of the University of California, Berkeley, examined the geologic ages of every major lineage of living bivalves the world over, from oysters and scallops to quahogs and ****les.
Title: Whilst this Planet Has Gone Cycling On: What Role for Periodic Astronomical Phenomena in Large Scale Patterns in the History of Life? Authors: B.S. Lieberman, A.L. Melott (University of Kansas)
One of the longstanding debates in the history of palaeontology focuses on the issue of whether or not there have been long term cycles (operating over tens of millions of years) in biodiversity and extinction. Here we consider the history of this debate by connecting the skein from Grabau up to 2008. We focus on the evidence for periodicity that has emerged thus far, and conclude that there is indeed some evidence that periodicity may be real, though of course more work is needed. We also comment on possible causal mechanisms, focusing especially on the motion of our solar system in the Galaxy. Moreover, we consider the reasons why some scientists have opposed periodicity over the years. Finally, we consider the significance of this for our understanding of evolution and the history of life.
Hundreds of thousands of years ago, giant versions of Australia's unique wildlife stalked the continent. There were kangaroos up to 3m tall and enormous wallabies, wombats and echidnas. There were also koalas: larger and weightier than the creatures sometimes seen today in eucalyptus trees. Giant koalas died out about 50,000 years ago, along with most of Australia's "megafauna". For a long time, modern koalas were assumed to be dwarf descendants of those prehistoric animals. But now an Australian palaeontologist has established that the two koalas lived side by side - a finding that may throw new light on why the megafauna disappeared. Gilbert Price, of the University of Queensland, used improved dating techniques to analyse fossils of both types of koala, and found that the two species co-existed in Australian trees for hundreds of thousands of years.
The clock is ticking inexorably toward doomsday even if we don't kill ourselves by poisoning the environment or overheating the planet. You see, there's a little problem with the Sun. The Sun is slowly getting warmer as it burns the hydrogen in its core. In about 5 billion years, the Sun will begin evolving into a bloated red giant. Its outer gas shell will swell up, engulfing the Earth by the time it reaches its peak size and brightness 7 billion years from now. But long before that, in 1.1 billion years, the Sun will grow 11% brighter, raising average terrestrial temperatures to around 50 °C (120 °F). That will warm the oceans so much that they evaporate without boiling, like a pan of water left on a sunny kitchen counter.
An asteroid is the prime suspect only in the most recent of five mass extinctions, said USC earth scientist David Bottjer. The cataclysm 65 million years ago wiped out the dinosaurs.
"The other four have not been resolvable to a rock falling out of the sky" - David Bottjer.
For example, Bottjer and many others have published studies suggesting that the end-Permian extinction 250 million years ago happened in essence because "the earth got sick." The latest research from Bottjer's group suggests a similar slow dying during the extinction 200 million years ago at the boundary of the Triassic and Jurassic eras.
Evidence suggests that 'sick Earth' extinctions more likely In geology as in cancer research, the silver bullet theory always gets the headlines and nearly always turns out to be wrong. For geologists who study mass extinctions, the silver bullet is a giant asteroid plunging to earth. But an asteroid is the prime suspect only in the most recent of five mass extinctions, said USC earth scientist David Bottjer. The cataclysm 65 million years ago wiped out the dinosaurs.
Mass extinction refuge discovered It was the biggest mass extinction in Earth's history: a climate catastrophe about 252 million years ago that wiped out more than 95% of all plant and animal species on the planet. But scientists have theorised that somewhere in that oxygen-starved world, where a "runaway" greenhouse-gas disaster nearly stopped the evolution of life dead in its tracks, a few communities of primitive organisms -- including our own pre-mammal ancestors -- must have found a handful of habitable ecological niches in which to survive and wait out the primordial holocaust.
This week marks the 125th anniversary of the extinction of the quagga - a small zebra-like creature that once roamed the plains of South Africa. While most of her kind were hunted out of existence in the 1870s, one lone mare lived on at Amsterdam Zoo until 1883. There are just seven skeletons in the world and UCL Grant Museum is the only institution in England to hold one, making the quagga, even in death, extremely rare.