RM2K639FJ–Fossil metasequoia leaves, John Day Fossil Beds, Oregon, USA
RF2GN8MXB–Prehistoric plants fossils texture imprint on granite rock stone used as construction material to build a house on the Mediterranean island Crete
RMFRBR3R–Poço revestido com fósseis de madeira petrificada no Parque Paleobotânico
RM2JC7899–The botanic gardens at Coutances, Normandy, France
RM2JJWB1X–Chemnitz, Germany. 28th July, 2022. The Petrified Forest of Chemnitz is in the city's Natural History Museum. A newly discovered 291-million-year-old species is a roof skull amphibian with stocky hind legs and a large skull plate. The anatomical features of the insectivorous amphibian differ from all comparable forms known to date. The fossil was discovered during excavations between 2008 and 2011 in Chemnitz. The Petrified Forest of Chemnitz is an important paleobotanical fossil site. Credit: Jan Woitas/dpa/ZB/dpa/Alamy Live News
RF2JT88GJ–Pasture field and cattle raising and geological formation in Brazil. Paleobotanical site existing in the municipalities of São Pedro do Sul. Rural lan
RM2BDY8MH–Prehistoric Men Battle Cave Bear
RMRN6WTC–. The anatomy of woody plants. Botany -- Anatomy. 334 THE ANATOMY OF WOODY PLANTS relationship of the Abietineae rather than the Araucariineae with the Paleozoic gymnosperms known as Cordaitales. Not only do the Abietineae as a result of their anatomical organization and paleobotanical history present a strong claim to direct relationship with the older gymnosperms, but they supply equally compelling evidence that they are ancestral to other prominent coniferous subtribes. It will be well in this connection to begin with the in- ternal situation in the abietineous subtribe. It is readily subdi
RM2BE10BR–Prehistoric men using wooden clubs and stone axe to fend off an attacks by a large cave bear. The cave bear (Ursus spelaeus) was a species of bear that lived in Europe during the Pleistocene and became extinct at the beginning of the Last Glacial Maximum, about 27,500 years ago. Mammoths can be seen in the background. A mammoth is any species of the extinct genus Mammuthus, proboscideans commonly equipped with long, curved tusks and, in northern species, a covering of long hair. They lived from the Pliocene epoch (from around 5 million years ago) into the Holocene at about 4,500 years ago in A
RM2K639FP–Fossil oak leaf, John Day Fossil Beds National Monument, Oregon, USA
RF2GN8MRG–Prehistoric plants fossils texture imprint on granite rock stone used as construction material to build a house on the Mediterranean island Crete
RM2JC2KMP–Work in progress, Botanic Gardens, Coutances, Normandy, France
RM2JJWB1G–Chemnitz, Germany. 28th July, 2022. The Petrified Forest of Chemnitz is in the city's Natural History Museum. A newly discovered 291-million-year-old species is a roof skull amphibian with stocky hind legs and a large skull plate. The anatomical features of the insectivorous amphibian differ from all comparable forms known to date. The fossil was discovered during excavations between 2008 and 2011 in Chemnitz. The Petrified Forest of Chemnitz is an important paleobotanical fossil site. Credit: Jan Woitas/dpa/ZB/dpa/Alamy Live News
RF2JT88FG–Pasture field and cattle raising and geological formation in Brazil. Paleobotanical site existing in the municipalities of São Pedro do Sul. Rural lan
RM2BE0HK4–Prehistoric men using wooden clubs and stone axe to fend off an attacks by a large cave bear. The cave bear (Ursus spelaeus) was a species of bear that lived in Europe during the Pleistocene and became extinct at the beginning of the Last Glacial Maximum, about 27,500 years ago. Mammoths can be seen in the background. A mammoth is any species of the extinct genus Mammuthus, proboscideans commonly equipped with long, curved tusks and, in northern species, a covering of long hair. They lived from the Pliocene epoch (from around 5 million years ago) into the Holocene at about 4,500 years ago in A
RMT9642F–Carboniferous landscape. The fifth period of the Paleozoic Era. The Carboniferous Period spanned from about 355 million years to about 295 million years ago. The rocks that formed during this time interval are known as the Carboniferous System; they include a wide variety of sedimentary, igneous, and metamorphic rocks. Sedimentary rocks in the lower portion of the Carboniferous are typically carbonates, such as limestones and dolostones, and locally some evaporites.
RM2K639FW–Fossil elm leaf, John Day Fossil Beds National Monument, Oregon, USA
RF2GN8MRD–Prehistoric plants fossils texture imprint on granite rock stone used as construction material to build a house on the Mediterranean island Crete
RM2JJWB1Y–Chemnitz, Germany. 28th July, 2022. The original find of a 291-million-year-old amphibian from the Petrified Forest of Chemnitz is on display at the city's Natural History Museum. The newly discovered species is a roof skull amphibian with stocky hind legs and a large skull plate. The anatomical features of the insectivorous amphibian differ from all comparable forms known to date. The fossil was discovered during excavations between 2008 and 2011 in Chemnitz. The Petrified Forest of Chemnitz is an important paleobotanical fossil site. Credit: Jan Woitas/dpa/ZB/dpa/Alamy Live News
RMG15NFB–Devonian is the fourth period of the Paleozoic Era, encompassing an interval of geologic time between 418 and 362 million years before present based on radiometric data. The Devonian System encompasses all rocks deposited or formed during the Devonian Per
RM2K639FR–Fossil hornbeam leaf, John Day Fossil Beds National Monument, Oregon, USA
RM2JJWB1C–Chemnitz, Germany. 28th July, 2022. The original find of a 291-million-year-old amphibian from the Petrified Forest of Chemnitz is on display at the city's Natural History Museum. The newly discovered species is a roof skull amphibian with stocky hind legs and a large skull plate. The anatomical features of the insectivorous amphibian differ from all comparable forms known to date. The fossil was discovered during excavations between 2008 and 2011 in Chemnitz. The Petrified Forest of Chemnitz is an important paleobotanical fossil site. Credit: Jan Woitas/dpa/ZB/dpa/Alamy Live News
RMG15NF9–The Mesozoic Era is an interval of geological time from about 252 to 66 million years ago. It is often referred to as the Age of Reptiles because reptiles, namely non-avian dinosaurs, were the dominant terrestrial and marine vertebrates of the time. The M
RM2K639FM–Fossil pine seeds, John Day Fossil Beds National Monument, Oregon, USA
RM2JJWB1R–Chemnitz, Germany. 28th July, 2022. The original find of a 291-million-year-old amphibian from the Petrified Forest of Chemnitz is on display at the city's Natural History Museum. The newly discovered species is a roof skull amphibian with stocky hind legs and a large skull plate. The anatomical features of the insectivorous amphibian differ from all comparable forms known to date. The fossil was discovered during excavations between 2008 and 2011 in Chemnitz. The Petrified Forest of Chemnitz is an important paleobotanical fossil site. Credit: Jan Woitas/dpa/ZB/dpa/Alamy Live News
RMG15NFA–Meganeura is a genus of extinct insects from the Carboniferous period, which resembled and are related to the present day dragonflies. Meganeura were predatory, and fed on other insects, and even small amphibians. Carboniferous is the fifth period of the
RMHRJ9YF–Prehistoric, Jurassic Landscape
RMHRJ9YD–Prehistoric, Triassic Landscape
RMG15NF8–Chirotherium, also known as Cheirotherium (hand-beast), is the name of a Triassic archosaur known only from fossil imprints of its tracks (trace fossils). Its tracks were first found in 1834 in red sandstone in Thuringia, Germany, dating from about 243 mi
RMHRJHRC–Prehistoric, Devonian Landscape
RMHRJ9YA–Prehistoric, Devonian Landscape
RMHRJ9YK–Prehistoric, Eocene Landscape
RMG15NFG–Eocene landscape (56 to 34 million years ago). The second oldest of the five major worldwide divisions (epochs) of the Tertiary Period (Cenozoic Era), the interval of time (epoch) extending from the end of the Paleocene Epoch to the beginning of the Oligo
RMG15NFC–Devonian is the fourth period of the Paleozoic Era, encompassing an interval of geologic time between 418 and 362 million years before present based on radiometric data. The Devonian System encompasses all rocks deposited or formed during the Devonian Per
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