Fossil evidence of the Asterales is rare and belongs to rather recent epochs, so the precise estimation of the order's age is quite difficult.

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 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 remains of members of this species have been found in the Torrejonian ( Paleocene )- age strata of the San Juan Basin of New Mexico and Wyoming.

In 2012, members of the network voted for a new climate change campaign, focusing on Unconventional Fossil Fuels.

Fossil remnants of members of Pasteurellaceae have never been reported and information on the diversification of taxa within the family can only be obtained by phylogenetic reconstruction.

Fossil teeth of D. giganteum, from the late Miocene Sinap Formation at the Turkish site of Kayadibi are larger than those from older localities, such as Eppelsheim, Wissberg and Montredon, indicating a tendency for increasing size of members of the species over time.

Excavations were resumed at the Walcott Quarry by the Geological Survey of Canada under the persuasion of trilobite expert Harry Blackmore Whittington, and a new quarry, the Raymond, was established about 20 metres higher up Fossil Ridge.

Fossil ferns and " seed ferns " include Pecopteris, Cyclopteris, Neuropteris, Alethopteris, and Sphenopteris ; Megaphyton and Caulopteris were tree ferns.

Fossil resin often contains other fossils called inclusions that were captured by the sticky resin.

They were of intense interest to Agassiz, and formed the subject of a special monograph by him published in 1844 – 45: Monographie des poissons fossiles du Vieux Gres Rouge, ou Systeme Devonien ( Old Red Sandstone ) des Iles Britanniques et de Russie (" Monograph on Fossil Fish of the Old Red Sandstone, or Devonian System of the British Isles and of Russia ").

Fossil fuels such as coal and gasoline store ancient energy derived from sunlight by organisms that later died, became buried and over time were then converted into these fuels.

Fossil trackways show that pterosaurs like Quetzalcoatlus northropi were quadrupeds.

Additional fossils of Pristinailurus bristoli were discovered at the Gray Fossil site in 2010 and in 2012.

A jawbone found in the mainland Jenolan Caves Fossil deposits in limestone caves at Naracoorte, South Australia, dating to the Miocene include specimens of S. laniarius, which were around 15 % larger and 50 % heavier than modern devils.

Fossils of an ancient equid were discovered in the Hagerman Fossil Beds National Monument in Hagerman, Idaho.

Fossil leopard bones and teeth dating from the Pliocene were found in Perrier in France, northeast of London, and in Valdarno in Italy.

Fossil gastropods were less common during the Palaeozoic era than bivalves.

OLED displays were used in watches made by Fossil ( JR-9465 ) and Diesel ( DZ-8076 ).

Fossil remains show that spruce, birch and poplars once grew beyond their northernmost modern range today, indicating that there were periods when the climate was warmer and wetter.

Fossil remains were found in the Upper Cretaceous strata of the Williams Fork Formation, in Colorado ( USA ).

Fossil remains were found in strata dating to the Kimmeridgian ( Upper Jurassic ) of Guimarota, Portugal.

Fossil remains of the species Henkelodon naias were discovered in the Kimmeridgian ( Upper Jurassic )- age strata of Guimarota, Portugal.

Fossil remains of the species Meketichoffatia krausei consisting of two upper jaws were found in Kimmeridgian ( Upper Jurassic )- age Camadas de Guimarota of Guimarota, Portugal.

Fossil remains of the species Sunnyodon notleyi were found in the Upper Jurassic or Lower Cretaceous-age strata of the Purbeck Formation in Durlston Bay, Dorset, England.

The genus Ecprepaulax was named by Hahn G. and Hahn R. in 1999 based on a single species Ecprepaulax anomala Fossil remains were found in Berriasian ( Lower Cretaceous ) strata in Portugal.

Fossil remains of the species Parendotherium herreroi were found in Barremian ( Lower Cretaceous )- age strata of Galve, Spain.

Fossil remains were found in the Campanian ( Upper Cretaceous )- age strata of Hermiin Tsav ( Khermeen Tsav ) in Mongolia.

Fossil remains were found in Clarkforkian ( Paleocene ) strata of Wyoming and Colorado.

Fossil remains of the species Cernaysia davidi ( Vianey-Liaud M. 1986 ) were found in Puercan ( Lower Paleocene ) strata of the San Juan Basin of New Mexico, ( USA ).