Fossils

I know for a fact that it was found on the Continent of Africa but I'm not sure which counrty in Africa.

The oldest human remains were found in the Horn of Africa, Somilia.

shows that all three continents were once connected (joined) together. because the 'exact' same fossil types were found in all three different continents, which are now split from each other.

no

Actually, at one time, some Fossil watches were made in the US. In fact, I'm wearing one such watch now (says "Made in the USA of Swiss parts" on the back). Mine was purchased in the early 90s.

They are no longer made in the US, however.

Fossils can be found anywhere. They're found on every continent except Antarctica, but they can be found in the ocean floor under antarctica. Rarely you'll find them frozen in the ice, but there's a very low chance you will. You'll have a slightly larger chance if you go further inland (in ice?), because that part of antarctica almost never defrosts. But of course the correct answer is that they are not found in a specific place, they are found everywhere.

The planet Earth is about 4,600 million years old.

Fossil evidence becomes abundant in the geological record in the Cambrian Era, which was about 550 million years ago (when hard shelled animals appeared)

Therefore (550/4600)*100 = roughly 12% of Geological time contains abundant fossil evidence.

However, please note that (non abundant) fossil evidence goes back about 3600 million years, (3600/4600)*100 = roughly 73% of Geologic time.

Pangaea implies at some part in the Earth's evolution, probably before the rise of mammals and intelligent life ( Man) there was one major world continent that since has split up into the present seven. As life of intelligent type did not exist at the time, there is no way fossils can be dragged in to prove things one way or the other, though it does have a relative bearing on Atlantis and Atlantean studies.

"Glossopteris (Greek glossa, meaning "tongue", because the leaves were tongue-shaped) is the largest and best-known genus of the extinct order of seed ferns known as Glossopteridales (or in some cases as Arberiales or Dictyopteridiales). Long considered a fern after its discovery in 1824, it was later assigned to the gymnosperms. The genus is placed in the division Pteridospermatophyta. In reality, many of the plant groups included within this division are only distantly related to one another." That was straight out of the Wikipedia article. It explains what glossopteris is (or was), and a fossil of one of these long-gone plants would be what was asked about in the original question. A link is provided to our friends at Wikipedia for further information.

permineralized remains

There are alot of widespread fossil organisms from the Paleozoic;

-Brachiopods

-Bryozoa

-Trilobites

-Corals

-Crinoids

-Gastropods

-Nautaloids/Cephalopods

-Ostracods

-Scolecodonts

Once you get to devonian you may be able to find shark teeth.

After the Carboniferous, You can find plants, insects, and (rarely) reptiles.

Hope this helped!

The lower the level of a rock stratum, the older it is. Evolution is recorded in the sedimentary rock record, therefore, the simpler forms would show up in the oldest layers. The old life forms were usually very simple so the deeper down the sedimentary levels are, the older the fossils are their.

One of the primary Darwinian ideas for the extinction of dinosaurs is natural selection. This suggests that environmental changes, possibly due to a catastrophic event like an asteroid impact or volcanic eruptions, led to the extinction of dinosaurs as their traits were no longer advantageous for survival. Another idea is that competition with other species or inability to adapt quickly to changing conditions may have played a role in their extinction.

Artifacts are important to Historians (and Archaeologists) because they are actual evidence of past human activity.

However fossils are NOT important to historians as they are too old, they ARE important to Geologists.

Fossils are used by scientists to determine the where, what, why, when, and how of ancient organisms. Answering these questions will help in determining the environment and climate in which the organisms existed, adaptations made by the organisms to the environment and climate, type and amount of energy requirements of organisms, feeding habits, reproduction techniques, nesting habits, digestion methods, type of respiration, method of locomotion, hunting techniques, timing and cause of extinction events, and the progression of evolution. Fossils are also key indicators of possible fossil fuel deposits which are of great interest to humanity.

The study of fossils also leads to discoveries and understanding of Earth's processes which can benefit mankind. Study of the Cretaceous-Tertiary extinction event eventually led to the hypothesis that a large asteroid impacted Earth. Some astronomers are currently seeking out and cataloging possible impact asteroids in an attempt to predict such a future cataclysm and help in preventing it.

== == == == == == == == == == == == == == == ==

Marine depositional environments are more plentiful, and the hard shells and body parts of many marine organisms do not decay from bacteria, or are not easily destroyed by predation. Additionally, the organism's remains are much more likely to be covered from precipitating sediments settling out of the water.

cast

No. The hard bones are more likely to form a fossil. The soft parts will degenerate over time. This is why most of the fossils from the Pre-Cambrian and Cambrian periods are mostly shells, not the actual animals that inhabited them.

In the context of Western Civilization, the Earth's age was originally calculated in mainly philosophical and religious terms, with a wide variety of thinkers making estimates of the Earth's age based on sacred texts, spiritual revelations, or (quite distinctly) metaphysico-scientific studies of reality, among other things. It was not until the early modern era that stricter experimental science was utilized to derive the age of the Earth based on geological evidence.

It is generally determined by how long it has waisted away or if it has reached a certain disintegrating phase (an example would be a half-life). By learning how long a fossils minerals and dead cells have wasted away biologists can learn how old a fossil is relative to a period or our own time on earth.

The Precambrian is the informal name for the large expanse of time preceding the current Phanerozoic Eon. It began with the Earth's formation about 4.5 billion years ago and lasted until the advent of multicellular life about 542 million years ago. Overall the planetary environment was drastically different. Life appeared sometime late in the Precambrian, but it is not known when.

The Precambrian "supereon" is divided into three eons: the Hadean, Archaean, and Proterozoic.

Very little is known about the Precambrian, despite the fact that it comprises nearly 90% of the Earth's history. This is simply because Precambrian rocks are so old, and are either heavily metamorphosed, have been destroyed by erosion, or remain buried deep beneath Phanerozoic strata.

if the original organism dissolves or decays, leaving a hollow in the rock, that is a mold.

If the mold fills up with sediment which gradually hardens into the shape of the original organism, then that is a cast.

Casts are copies of fossilized plants or animals. Molds are hollow impressions of the fossil.

Lamarck's explanation of evolution is based on two principles: use and disuse and the inheritance of acquired characteristics. Lamarck's "use and disuse" principle explained his belief that the body parts that are commonly used become larger and stronger such as a giraffe's neck, while those that are not used deteriorate and become smaller. He also believed that an organism could pass these modifications to its offspring through the inheritance of acquired characteristics. Thus, Lamarck thought that evolution is driven by the innate drive of organisms to become more complex. Although he was later proven wrong, he was insightful in observing and recognizing that gradual evolutionary change does exist.

2 Half-Lifes= 1/4 Carbon 14 remaining. So 2 half lives have past. You add the 5730 years together to get 11460 years or 1.15*10^4 years.

The youngest fossils are typically found in recent sedimentary rock formations or on the surface of the Earth. These fossils are often from organisms that lived within the past few thousand years, such as the bones of mammoths or ancient human remains.

Inference (deduction) is the process of determining a conclusion based on given evidence. Since we often can't know precisely what a prehistoric animal or plant looked like (unless it was completely preserved, as is the case with ice or amber), we have to take what bones, casts, molds, etc. that exist, and infer something about the plant or animal based on the structure and surroundings. For example, based on what we know about structure and function of various anatomies of existing animals, we can infer things about dinosaurs based on the bone structures found in their fossils. We can also determine whether they were predators or prey, whether they hunted or traveled in herds, in what class of animal we can group them, and so forth.

MLB player Darwin Barney weighs 186 pounds.