An illustration of trilobites moving about on the bottom of a warm Paleozoic sea.
Trilobites are a well-known fossil group of extinct marine arthropods that form the class Trilobita. Trilobites form one of the earliest known groups of arthropods. The first appearance of trilobites in the fossil record defines the base of the Atdabanian stage of the Early Cambrian period (521 million years ago), and they flourished throughout the lower Paleozoic era before beginning a drawn-out decline to extinction when, during the Devonian, all trilobite orders except Proetida died out. Trilobites finally disappeared in the mass extinction at the end of the Permian about 250 million years ago. The trilobites were among the most successful of all early animals, roaming the oceans for over 270 million years Trilobites range in length from 1 millimetre (0.04 in) to 72 centimetres (28 in), with a typical size range of 3–10 cm (1.2–3.9 in). The world's largest trilobite, Isotelus rex, was found in 1998 by Canadian scientists in Ordovician rocks on the shores of Hudson Bay. (definition Source: Wikipedia) Full resolution stock illustration available: A 3-D computer illustration of colonies of the tiny extinct marine animals known as Diplograptus (Graptolites) of the Ordovician period (which occurred from 505 to 438 million years ago). Diplograptus is characterized by a caplike float from which featherlike assemblages of graptolite organisms were suspended. Though purely an artistic interpretation, the structure of the animal is inferred through scientific notation of what the species may have looked like within the environment in which they existed.
A herd of Woolly Mammoths march through an ice age forest 60,000 years ago. (c) Aunt Spray LLC 2015 'Winter Forest' HDRI sIBL background archive image courtesy of HDRLabs, www.hdrlabs.com under CC License. This image may be downloaded freely and used for non-commercial purposes only, and without alteration. Credit to Aunt Spray LLC must be given in any use. ![]()
A 3-D computer illustration of colonies of the tiny extinct marine animals known as Diplograptus (Graptolites) of the Ordovician period (which occurred from 505 to 438 million years ago). Diplograptus is characterized by a caplike float from which featherlike assemblages of graptolite organisms were suspended. Though purely an artistic interpretation, the structure of the animal is inferred through scientific notation of what the species may have looked like within the environment in which they existed.
Purchase full resolution commercial use stock image Here An illustration of the extinct giant ground sloth Megalonyx searching a tree for food in an Ice Age Ohio forest. Megalonyx jeffersonii was a large, heavily built animal about 9.8 feet (3 m) long existing from the Miocene through the Pleistocene.
|
Aunt SprayDesigner/Illustrator Archives
August 2021
Categories
All
|