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Fossil remains of beavers are found in the peat and other superficial deposits of Britain and the continent of Europe ; while in the Pleistocene formations of Britain and Siberia, remains of a giant extinct beaver have been found, Trogontherium cuvieri, representing a genus by itself.
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Fossil and remains
Fossil remains of true finches are rare, and those that are known can mostly be assigned to extant genera at least.
Fossil remains of Florida manatee ancestors date back about 45 million years.
Fossil fuels formed from the fossilized remains of dead plants by exposure to heat and pressure in the Earth's crust over millions of years.
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.
The Riversleigh Fossil Fields Section of the park is a World Heritage Site and contains many fossil remains.
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 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 have been found in strata dating to the Upper Paleocene in Nao-mugen and Bayn Ulan of China.
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 consisting of two upper jaws have been found in the Kimmeridgian ( Upper Jurassic )- age strata 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.
Fossil remains of the single species Hahnodon taqueti consist of a single lower molar found in Lower Cretaceous strata in Morocco.
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 Plagiaulax becklesii are known from Durlston Bay in Dorset, England.
Fossil remains are known from the Upper Jurassic and Lower Cretaceous of Europe and Asia.
Fossil remains are known from the Kimmeridgian ( Upper Jurassic )- age strata of Guimarota, Portugal.
Fossil remains of the species Loxaulax valdensis consist of a tooth found in Valangian ( Lower Cretaceous ) strata of the Cliff End bonebed in Hastings, England.
Fossil remains come from the Lower Cretaceous of Mongolia.
Fossil remains of the species Parendotherium herreroi were found in Barremian ( Lower Cretaceous )- age strata of Galve, Spain.
Fossil remains of the species " Cimexomys " gregoryi ( Eaton J. G.
Fossil and are
Fossil sites with exceptional preservation — sometimes including preserved soft tissues — are known as Lagerstätten.
Fossil fuels such as coal and petroleum are also included in this category because they are formed from decayed organic matter.
First discovered in 1972 by French physicist Francis Perrin, they are collectively known as the Oklo Fossil Reactors.
The frequency with which panda fossils are being found at Gray Fossil Site suggests the species played a large role in the overall ecosystem of the area.
Fossil records of crayfish older than 30 million years are rare, but fossilised burrows have been found from strata as old as the late Palaeozoic or early Mesozoic.
Fossil deposits are also abundant there.
Fossil plants with anatomically preserved xylem are known from the Silurian ( more than 400 million years ago ), and trace fossils resembling individual xylem cells may be found in earlier Ordovician rocks.
Fossil fuels are fuels formed by natural processes such as anaerobic decomposition of buried dead organisms.
Fossil fuels are non-renewable resources because they take millions of years to form, and reserves are being depleted much faster than new ones are being made.
Fossil fuels are of great importance because they can be burned ( oxidized to carbon dioxide and water ), producing significant amounts of energy per unit weight.
Fossil records are rare but 16 million year old fossils show that Albatrosses and Shearwaters haven't changed much since then.
Fossil fuel combustion is a primary contributor, but so are biofuels and even the burning of hydrogen.
Fossil species have ( correctly or incorrectly ) been assigned to this genus, but only extant species are listed below.
The remnants of ferns, semi-tropical and temperate deciduous forests, shellfish, saber-toothed tigers, extinct horse and camel species, and giant sloth, among other extinct species found in the John Day Fossil Beds, are a reminder that the flora and fauna of the region has changed significantly over the millennia.
The caves, such as the Victoria Fossil Cave and Blanche Cave, are often not far below ground, and holes open up creating traps for the unwary.
About 30 minutes ' walk north of Darlington are the Fossil Cliffs, located in Fossil Bay and packed with fossils.
The Sheep Rock Unit of the John Day Fossil Beds National Monument, including the Thomas Condon Paleontology Center and the James Cant Ranch Historic District and museum, are miles north of Picture Gorge along Route 19.
Golf tournaments are held each year at a six-hole golf course at Kinzua, near Fossil.
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