devonian period?

Question

i need the description of the fossil record during that period.

Answer 1

Marine biota

Sea levels in the Devonian were generally high. Marine faunas continued to be dominated by bryozoa, diverse and abundant brachiopods and corals. Lily-like crinoids were abundant, and trilobites were still fairly common, but less diverse than in earlier periods. The ostracoderms were joined in the mid-Devonian by the first jawed fishes, the great armored placoderms, as well as the first sharks and ray-finned fish. The first shark, the Cladoselache, appeared in the oceans during the Devonian period. They became abundant and diverse. In the late Devonian the lobe-finned fish appeared, giving rise to the first tetrapods.

Reefs

A great barrier reef, now left high and dry in the Kimberley Basin of northwest Australia, once extended a thousand kilometers, fringing a Devonian continent. Reefs in general are built by various carbonate-secreting organisms that have the ability to erect wave-resistant frameworks close to sea level. The main contributors of the Devonian reefs were unlike modern reefs, which are constructed mainly by corals and calcareous algae. They were composed of calcareous algae and coral-like stromatoporoids, and tabulate and rugose corals, in that order of importance.

Terrestrial biota

By the Devonian Period, life was well underway in its colonization of the land. The bacterial and algal mats were joined early in the period by primitive plants that created the first recognizable soils and harbored some arthropods like mites, scorpions and myriapods. Early Devonian plants did not have roots or leaves like the plants most common today, and many had no vascular tissue at all. They probably spread largely by vegetative growth, and did not grow much more than a few centimeters tall.

By the Late Devonian, forests of small, primitive plants existed: lycophytes, sphenophytes, ferns, and progymnosperms had evolved. Most of these plants have true roots and leaves, and many were quite tall. The tree-like ancestral fern Archaeopteris, grew as a large tree with true wood. These are the oldest known trees of the world's first forests. By the end of the Devonian, the first seed-forming plants had appeared. This rapid appearance of so many plant groups and growth forms has been called the "Devonian Explosion". The primitive arthropods co-evolved with this diversified terrestrial vegetation structure. The evolving co-dependence of insects and seed-plants that characterizes a recognizably modern world had its genesis in the late Devonian. The development of soils and plant root systems probably led to changes in the speed and pattern of erosion and sediment deposition.

The 'greening' of the continents acted as a carbon dioxide sink, and atmospheric levels of this greenhouse gas may have dropped. This may have cooled the climate and led to a massive extinction event. see Late Devonian extinction.

Also in the Devonian, both vertebrates and arthropods were solidly established on the land.

Fungal life

While the marine fungi remained in the oceans and diversified into Nature's recyclers, land fungi were also recycling the land, decomposing both plants' and animals' dead bodies. Also, due to more terrestrial plants and animals appearance, fungi flourished.

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The Devonian seas were dominated by brachiopods, such as the spiriferids, and by tabulate and rugose corals, which built large bioherms, or reefs, in shallow waters. Encrusting red algae also contributed to reef building. In the Lower Devonian, ammonoids appeared, leaving us large limestone deposits from their shells. Bivalves, crinoid and blastoid echinoderms, graptolites, and trilobites were all present, though most groups of trilobites disappeared by the close of the Devonian.

The Devonian is also notable for the rapid diversification in fish. Benthic armored fish are common by the Early Devonian. These early fish are collectively called "ostracoderms", and include a number of different groups. By the Mid-Devonian, placoderms, the first jawed fish, appear. Many of these grew to large sizes and were fearsome predators. Of the greatest interest to us is the rise of the first sarcopterygiians, or the lobe-finned fish, which eventually produced the first tetrapods just before the end of the Devonian

Answer 2

The Devonian is also known as the age of Fishes. It was during this period that bony fish first appeared as contrasted with fish having cartilaginous skeletons i.e. sharks . Other forms of fossils common would still be trilobites, crinoids, cephalopod shells, bivalves and gastropods. Vegetable fossils would include ferns,algae, and probably cycads, although I don't remember for sure if they date from the Devonian or the Carboniferous.

Answer 3

A simple search on "devonian period fossils" will bring up lots of sites like the one below. Have fun!!

Answer 4

The Devonian is commonly referred to as the age of the fishes, though there were many different types of animals and plants alive during this period. There are many great paleontoloy sites on the web that are devoted to the Devonian.
http://www.ucmp.berkeley.edu/devonian/devonian.html
http://www.fossils-facts-and-finds.com/devonian_period.html
http://www.infoplease.com/ce6/sci/A0815352.html

It certainly is one of my favorite geologic periods.

Lots of great happenings all over the world.

Answer 5

bacteria is all i know.