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Fossil and evidence
Fossil evidence of pre-Cambrian life has since been found, extending the history of life back for billions of years.
Fossil evidence suggests that they originated during, or before, the early Jurassic Period.
Fossil evidence suggests that people from the north brought the Dingo to Australia about 5000 years ago.
Fossil evidence and DNA sequence analysis suggest that this mutualism appeared 400-460 million years ago, when the first plants were colonizing land.
Fossil evidence indicates that members of the Welwitschiaceae were present in South America during the Lower Cretaceous ( Mesozoic era ).
Fossil evidence of pelicans dates back at least 30 million years, to the remains of a beak very similar to that of modern species recovered from Oligocene strata in France.
Fossil evidence indicates that the ancestral North American magpie had arrived in its current range around the mid-Pliocene ( 3-4 mya ) and that the Yellow-billed Magpie lineage split off rather soon thereafter due to the Sierra Nevada uplift and the beginning ice ages.
It has a large global population, including an estimated 17 – 28 million individuals in Europe Fossil evidence suggests the Rock Dove originated in southern Asia and skeletal remains unearthed in Israel confirm their existence there for at least three hundred thousand years.
Fossil evidence for the evolution of biotic pollination discussion.
Fossil evidence also suggests that a certain Cambrian form of euthycarcinoid ( an extinct arthropod ) may also have mated by amplexus.
Fossil evidence suggests that the nyala has been a separate species since the end of the Miocene ( 5. 8 million years ago ).
Fossil evidence suggests that it has only recently become adapted to the Mediterranean climate as its closest relatives are part of the Madrean pine-oak woodlands found at higher elevations in the southwest US and Mexico.
Fossil evidence reveals that Laysan Ducks once lived across the entire archipelago, but today survive only on three small, isolated islands.
Fossil evidence of a third species — Ridgen's Penguin ( A. ridgeni )— has been found in fossil records from the late Pliocene, about three million years ago, in New Zealand.
Fossil evidence from some ophiacodonts shows that parts of the skin was covered in rows of osteoderms, presumably overlain by horny scutes.
Fossil evidence indicates that the fisher's range extended farther south than it does today.
Fossil evidence indicates the Enhydra lineage became isolated in the North Pacific approximately 2 Mya, giving rise to the now-extinct Enhydra macrodonta and the modern sea otter, Enhydra lutris.
Fossil evidence suggests Didelphodon was a small predator, perhaps filling the niche that foxes do today.
Fossil evidence indicates that the genus originated in West Africa during the Paleocene, and spread to Asia, to South America, and to Europe and thence to North America.
Fossil of Sinornithosaurus | Sinornithosaurus millenii, the first evidence of feathers in dromaeosaurids
Fossil evidence shows it had a wider distribution in the past, south to central Mexico.
Fossil evidence shows that the toes were probably lobed, as in today's grebes, rather than webbed as in those of loons.
Fossil evidence showed that tens of thousands of years ago, ground sloths, horses, elephants and camels roamed among redwood trees in what is now Los Angeles, according to an MTA summary of the 300-page report.
Fossil evidence suggests the Entodacrya may have originated in Asia ( Marivaux et al., 2004 ) and this is cited as potential evidence for an Asian origin for Caviomorpha as well.

Fossil and is
Fossil resin ( colloquially called amber ) is a natural polymer found in many types of strata throughout the world, even the Arctic.
Fossil wood is wood that is preserved in the fossil record.
Fossil trading is the practice of buying and selling fossils.
Fossil collecting ( some times, in a non-scientific sense, fossil hunting ) is the collection of fossils for scientific study, hobby, or profit.
Fossil collecting, as practiced by amateurs, is the predecessor of modern paleontology and many still collect fossils and study fossils as amateurs.
Fossil Olea pollen has been found in Macedonia, Greece, and other places around Mediterranean, indicating that this genus is an original element of the Mediterranean flora.
* August 20 – Florissant Fossil Beds National Monument is established in Florissant, CO, USA
" I suggest that this is a good time to think soberly about our responsibilities to our descendants-those who will ring out the Fossil Fuel Age.
Fossil fuel combustion is a primary contributor, but so are biofuels and even the burning of hydrogen.
Fossil Lake is an area nearby where many fossils of prehistoric animals have been identified.
The geology of Grant County is rich, including one of the largest fossil concentrations in North America: The John Day Fossil Beds, which the U. S. Congress designated as a National Monument in 1974.
The Ashfall Fossil Beds National Natural Landmark is located within the county.
The power plant is the second largest plant in the TVA Fossil Fuels Plant Inventory with a rated output of 2, 630 megawatts.
The Riversleigh Fossil Fields Section of the park is a World Heritage Site and contains many fossil remains.
Hagerman is the home of the Hagerman Fossil Beds National Monument of the U. S. National Park Service.
The Old Trail Museum in Choteau is home to the Maiasaura type fossil, which is the Montana State Fossil.
Aurora is the home of the Aurora Fossil Museum, which houses specimens collected from the local PCS Phosphate Mine.
Fossil is a city in and the county seat of Wheeler County, Oregon, United States.
Fossil is the county seat of Wheeler County.
Fossil is located in north-central Oregon at the intersection of Oregon Route 19 with Oregon Route 218.
The Clarno Unit of the John Day Fossil Beds National Monument is west of the city along Route 218.

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