Jump to content

User:Abyssal/Portal:Permian

From Wikipedia, the free encyclopedia


The Permian Portal


Introduction

Show new selections below (purge)

Selected article on the Permian world and its legacies

Death Valley viewed from space.
Death Valley viewed from space.

The exposed geology of the Death Valley area presents a diverse and complex set of at least 23 formations of sedimentary units, two major gaps in the geologic record called unconformities, and at least one distinct set of related formations geologists call a group. The oldest rocks in the area are extensively metamorphosed by intense heat and pressure and are at least 1700 million years old. These rocks were intruded by a mass of granite 1400 Ma (million years ago) and later uplifted and exposed to nearly 500 million years of erosion.

Marine deposition occurred 1200 to 800 Ma, creating thick sequences of conglomerate, mudstone, and carbonate rock topped by stromatolites, and possibly glacial deposits from the hypothesized Snowball Earth event. Rifting thinned huge roughly linear parts of the supercontinent Rodinia enough to allow sea water to invade and divide its landmass into component continents separated by narrow straits. A passive margin developed on the edges of these new seas in the Death Valley region. Carbonate banks formed on this part of the two margins only to be subsided as the continental crust thinned until it broke, giving birth to a new ocean basin. An accretion wedge of clastic sediment then started to accumulate at the base of the submerged precipice, entombing the region's first known fossils of complex life. These sandy mudflats gave way about 550 Ma to a carbonate platform which lasted for the next 300 million years of Paleozoic time. (see more...)

Did you know?

Skeletal mount of Scutosaurus.
Skeletal mount of Scutosaurus.

Need help?

Do you have a question about Abyssal/Portal:Permian that you can't find the answer to?

Consider asking it at the Wikipedia reference desk.

Selected image

Life restoration of Casea.

Life restoration of Casea broilii, a pelycosaur from the Late Permian of Europe and North America.
Photo credit: Nobu Tamura

Selected article on the Permian in human science, culture and economics

Edward Drinker Cope (left) and Othniel Charles Marsh (right).
Edward Drinker Cope (left) and Othniel Charles Marsh (right).
Bone Sharps, Cowboys, and Thunder Lizards: A Tale of Edward Drinker Cope, Othniel Charles Marsh, and the Gilded Age of Paleontology (2005) is a graphic novel written by Jim Ottaviani and illustrated by the company Big Time Attic. The book tells a slightly fictionalized account of the Bone Wars, a period of intense excavation, speculation, and rivalry which led to a greater understanding of dinosaurs in the western United States. This novel is the first semi-fictional work written by Ottaviani; previously, he had taken no creative license with the characters he depicted, portraying them strictly according to historical sources.

Bone Sharps follows the two scientists Edward Drinker Cope and Othniel Marsh as they engage in an intense rivalry for prestige. Ottaviani has Cope and Marsh interact and meet many important figures of the Gilded Age, from P. T. Barnum to U.S. Grant, as the two scientists pursue their hotheaded and sometimes illegal acquisitions of fossils. Unlike in his previous books, "the scientists are the bad guys this time". Upon release, the novel received praise from critics for its exceptional historical content, although some reviewers wished more fiction had been woven into the story. (see more...)

Quality Content

Featured Permian articles - Amphibian
Good Permian articles - Dimetrodon - Temnospondyli

Things you can do


Here are some tasks awaiting attention:

Current Permian FACs - none currently

Associated Wikimedia

The following Wikimedia Foundation sister projects provide more on this subject:


¤ Category:Geologic time portals