Fossils of Neanderthals dating to the middle Palaeolithic period have been unearthed in northern Croatia, with the most famous and the best presented site in Krapina.

Fossils very similar to V. komodoensis have been found in Australia dating to greater than 3. 8 million years ago, and its body size remained stable on Flores, one of the handful of Indonesian islands where it is currently found, over the last 900, 000 years, " a time marked by major faunal turnovers, extinction of the island's megafauna, and the arrival of early hominids by 880 ka.

Fossils suggest they may have possessed many modern attributes even by the late Carboniferous, and it is possible that they captured small vertebrates, for some species had a wing span of 71 cm.

Fossils of pterosaurs only a few days to a week old ( called flaplings ) have been found, representing several pterosaur families, including pterodactylids, rhamphorhinchids, ctenochasmatids and azhdarchids.

Fossils from terrestrial dinosaurs also have been found in the Niobrara Chalk, suggesting that animals who died on shore must have been washed out to sea ( one specimen of a hadrosaur appears to have been scavenged by a shark ).

Fossils of the red panda Parailurus anglicus have been unearthed from China in the east to Britain in the west.

Fossils of species similar to modern devils have been found, but it is not known whether they were ancestors of the contemporary species, or whether the current devils co-existed with these species.

Fossils of dromaeosaurids more primitive than Velociraptor are known to have had feathers covering their bodies, and fully developed, feathered wings.

Fossils of early leopard ancestors have been found in East Africa and South Asia from the Pleistocene of 2 to 3. 5 Ma.

Fossils of all of these types have been found in rocks dated from.

Fossils of true geese are hard to assign to genus ; all that can be said is that their fossil record, particularly in North America, is dense and comprehensively documents many different species of true geese that have been around since about 10 million years ago in the Miocene.

Fossils from North Carolina were originally thought to have been of two Fratercula species, but were later reassigned to one Fratercula, the Tufted Puffin, and a Cerorhinca species.

Fossils have later been found in all continents except Australia and Antarctica.

Fossils from the Pleistocene era have been found in various parts of North America, including New York and Florida, leading scientists to believe that California Condors or their ancestors once lived on the west coast of North America as well as all the way to the eastern coast.

Fossils belonging to the genus Bassariscus, which includes the modern ringtail and cacomistle, have been identified from the Miocene epoch, around 20 million years ago.

Fossils have been found in the Upper Jurassic Morrison Formation of Wyoming ( U. S .).

Fossils of the species dating to the middle Pleistocene have been found in Italy.

Fossils have been found in the Berriasian ( Lower Cretaceous ) of Durlston Bay, Dorset.

Fossils have been found in Albian ( late )-Cenomanian ( early ), ( both Upper Cretaceous )- aged strata of the Cedar Mountain Formation in Utah ( USA ).

Fossils of the species Cedaromys parvus ( Eaton & Cifelli, 2001 ) have been found in strata of the same age in the Cedar Mountain Formation.

Fossils of this species have been found in the Torrejonian ( Paleocene )- age beds of Big Bend, Texas

Fossils have been found in the Lance Formation of Wyoming ( USA ).

Fossils ( from Latin fossus, literally " having been dug up ") are the preserved remains or traces of animals ( also known as zoolites ), plants, and other organisms from the remote past.

Fossils have also been found in Alaska dating from the Pleistocene.

Fossils of invertebrates are found in various types of sediment from the Phanerozoic.

Fossils found in Japan indicate that the local tigers were, like the surviving island subspecies, smaller than the mainland forms.

Fossils show it had bony skull outgrowths that resembled non-deciduous antlers found in Northern America approximately 35 million years ago.

Fossils of cyanobacterial mats ( stromatolites, which were instrumental in creating the free oxygen in the atmosphere ) are found throughout the Archean, becoming especially common late in the eon, while a few probable bacterial fossils are known from chert beds.

Fossils of the late and middle Triassic Warepan and Kaihikuan stages are found in the area.

Fossils are found in thin layers less than an inch thick.

Fossils from the devonian can be found within the limestone strata.

Fossils are commonly found in the Paleozoic strata that is exposed along the Mogollon Rim to the north and west of Payson along State Route 87 and State Route 260.

Fossils can be found in the limestone scree at the base of the cuttings.

Fossils can be found everywhere.

Fossils of the only named species ( D. torosus ) were found in Alberta, although other possible species from Alberta and Montana await description.

Fossils of both chough species were found in the mountains of the Canary Islands.

Fossils of both chough species were found in the mountains of the Canary Islands.

**** Genus Fibla Navás, 1915 ( Eocene-Recent ; Fossils: Baltic amber, Spain, USA )

Fossils of lungfish almost identical to this species have been uncovered in northern New South Wales, indicating that Neoceratodus has remained virtually unchanged for well over 100 million years, making it a living fossil and one of the oldest living vertebrate genera on the planet.

Fossils found near fossil palmwood include corals, sponges, and mollusks, indicating that the palms grew along prehistoric beaches.

Fossils of Eucommia have been found in 10 – 35 million year old brown coal deposits in central Europe and widely in North America ( Call & Dilcher 1997 ), indicating that the genus had a much wider range in the past.