A new study and timeline has been released showing 190 million years of tetrapod biodiversity, exceptional data for fossils and paleontology.
Recently, we have been able to provide some answers to the questions of how diverse through time has life been, based on the building of large fossil occurrence databases and new methods of analysing them. One such development has been the Paleobiology Database, a professional crowd-sourced archive of fossil history, where the context of fossils is provided in both space and time, and largely based on the published record of fossil discoveries.
…By applying SQS with our development of large fossil occurrence datasets, voila, we are able to gain renewed insight into the diversity of life through history in a way that accounts for the inherent biases of the fossil record!
And that’s just what a new study in PLOS Biology set out to do. Led by Roger Benson of the University of Oxford, an international team of researchers applied SQS to one of the largest tetrapod fossil occurrence databases ever assembled (if not the largest!), comprising more than 27,000 individual fossil occurrences! This represented almost 5000 fossil species, and the data were restricted to just those fossils that dwelled on land – so this excludes groups like ichthyosaurs and plesiosaurs, for example. They also excluded flying tetrapods, so birds, bats and mammals, as these are known to have very different preservational histories in the fossil record. For palaeontology though, this is definitely ‘big data’.
The team restricted their analyses to just the Mesozoic to early Paleogene, a time span of around 190 million years (a fairly long time, even by geological standards!). If you think about it, that’s 5000 species over about 190 million years, which compared to 30,000 around today is pretty weird even in itself.
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OPB-TV’s Oregon Experience honored Thomas Condon last week with his story. A preacher and pioneer geologist, Thomas Condon arrived in the Oregon Territory in 1853 and settled in The Dalles, and eventually became Oregon’s first state geologist and professor at Pacific University in Forest Grove, Oregon, and later to the brand new University of Oregon in 1876.
Thomas Condon always loved geology. He subscribed to scientific journals and collected rocks and fossils wherever he lived. Townspeople, teamsters, and soldiers stationed at Fort Dalles knew of his great knowledge of geology and began bringing him fossils to examine and identify.
By 1865 Condon was accompanying the soldiers on trips into Oregon’s interior and was the first to recognize the scientific significance of the area now known as the John Day Fossil Beds – where nearly 50 million years of time are preserved.
The mid 1800s was considered the Golden Age of Paleontology. Scientists were in competition to discover fossil specimens that would support Charles Darwin’s new theory of evolution. Early on Condon had began corresponding with prominent East coast paleontologists and sent them fossil specimens he’d collected for identification. The paleontologists in turn had the status and money to write articles and get the new discoveries published in leading scientific journals.
Some of Condon’s most famous ancient discoveries included parts of small three-toed ancestors of the modern horse. Yale University professor O.C. Marsh called the fossils the “missing link” in horse evolution and would write significant papers on the subject using Condon’s fossil discoveries as part of the evidence.
Today, you can find Condon’s fossil collection at the University of Oregon, and explore the Thomas Condon Paleontology Center at the John Day Fossil Beds National Monument in Central Oregon.
If you are heading north into Washington State, way far north towards the Canadian border, take time to drop by Western Washington University in Bellingham for their free and open to the public exhibit of the minerals, fossils of Washington state, reports the Bellingham Herald. The exhibit is on the ground floor and part of the first and second floors of the Environmental Studies Building.
It’s like a mini-museum, with displays that include mineral crystals, mammoth teeth and fossilized plant leaves, along with interpretive exhibits that highlight coal mining in Whatcom County and show some of the tools and equipment that scientists use to study the Earth. There’s even a seismograph and seismometer.
…Possibly the most fascinating display is a four-foot slab of sedimentary rock containing the three-toed footprint of a diatryma, a giant flightless bird from the Eocene Period, some 34 million to 56 million years ago. It was discovered in sedimentary rock that shook loose in a landslide several years ago near Racehorse Creek in the Mount Baker foothills. The slab was airlifted by helicopter to WWU.
As our members know well, Washington (as well as Oregon) is one of the most geologically dynamic areas in the world. This exhibit is designed to showcase what they are calling “Northwest Origins” going back more than 1 billion years old.
If you head up there, please let us know and consider writing a report about the exhibit for the website and newsletter.
Live Science reported that a 3.5-billion-year-old fossil microbial community has been found in Australia by scientists, revealing some of the most ancient fossil life forms ever discovered.
The new find reveals that a scant 1 billion years after Earth’s origin, complex microbial communities that clung to sediments along the windswept seashore had already begun harvesting energy from sunlight, rather than the rocks.
…A few stromatolites, or domelike like rock structures built by ancient microbial communities, have been found at the Strelley Pool formation in Australia that may date to about 3.45 billion years ago. Fossil sulfur-eating microbes from about 3.4 billion years ago have also been found there as well. Other fossils from South Africa reveal microbial communities that date to 2.9 billion years ago.
…More primitive rock-eating bacteria, called chemolithotrophs, likely evolved before the microbial mats, though no trace of Earth’s earliest pioneers has yet been found. Chemolithotrophs harvest energy by chemically modifying minerals such as iron or sulfur in the rock, and many such bacteria are still alive today.
But the newly discovered communities were anchored to the seashore close to sun and water, so they probably weren’t eating minerals found in rock. Instead, they must have harvested energy through photosynthesis, suggesting such bacteria evolved earlier than previously thought.