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Global extinction: Gradual doom is just as bad as abrupt

A recent study published in the Geological Society of America Bulletin suggests that Earth's largest mass extinction, known as 'The Great Dying,' occurred over hundreds of thousands of years, not suddenly. The research, led by Thomas Algeo from the University of Cincinnati, found evidence of a prolonged die-off of marine life due to ma...

SourceUniversity of Cincinnati·JournalGeological Society of America Bulletin·DateFeb 3, 2012

Giant kraken lair discovered

Researchers have discovered a remarkable fossil site in Nevada where the remains of nine 45-foot-long ichthyosaurs suggest an even larger and more cunning sea monster existed: a Triassic kraken. The evidence implies that this ancient cephalopod was capable of intelligent manipulation of bones and preyed on these massive reptiles.

MIT: Oxygen's watery past

MIT researchers found evidence that tiny aerobic organisms may have evolved to survive on extremely low levels of oxygen in oceanic 'oxygen oases.' Laboratory experiments with yeast suggest early ancestors could have thrived with minimal O2, reconciling a debate over early Earth's atmosphere.

SourceMassachusetts Institute of Technology·JournalProceedings of the National Academy of Sciences·DateAug 16, 2011

Carbon release to atmosphere 10 times faster than in the past

Researchers found that carbon release into atmosphere today is nearly 10 times faster than during the Paleocene-Eocene Thermal Maximum, a 55.9 million-year-old event similar to current global warming. The study suggests this rapid change may not allow sufficient time for biological systems to adapt.

SourcePenn State·JournalNature Geoscience·DateJun 5, 2011

Plankton key to origin of Earth's first breathable atmosphere

Researchers studying the origin of Earth's first breathable atmosphere have found that ancient plankton played a critical role in providing oxygen. This discovery builds on earlier work that showed a reverse-greenhouse effect cooled the oceans, spawning giant plankton blooms and sending oxygen into the atmosphere.

SourceOhio State University·JournalProceedings of the National Academy of Sciences·DateFeb 21, 2011

Oxygen's challenge to early life

Researchers found evidence of oxygen-poor ocean conditions lasting 2-4 million years after the first appearance of animals, suggesting fluctuating oxygen levels may have driven rapid evolutionary turnover during the Cambrian Period. This study provides new insights into how early life evolved and flourished on Earth.

Scientists question fisheries health test

A widely used biodiversity indicator in fisheries is found to be an ineffective guide to trends in marine ecosystems, according to a new study published in Nature. The researchers recommend more direct monitoring and the development of trend-detection methods to better assess the impacts of fishing on marine biodiversity.

SourceCSIRO Australia·JournalNature·DateNov 23, 2010

Algeo tracks evidence of 'The Great Dying'

A team of researchers led by Thomas Algeo from the University of Cincinnati analyzed chemical evidence from rocks formed during the Permian-Triassic extinction event, which wiped out 90% of all living species. The study suggests that massive volcanic eruptions in Siberia and global climate change contributed to the catastrophic event.

The biggest crash on Earth

Scientists have used a new seismic method to investigate the collision process between India and Tibet, revealing a more pronounced boundary between rigid lithosphere and softer asthenosphere. The study provides insights into the processes involved in the collision and aims to reduce earthquake risk in the region.

SourceHelmholtz Association·JournalScience·DateSep 16, 2010