The most useful method for dating the remains of plants and animals that lived within the last 50,000 years is radiocarbon dating (carbon-14 dating). This technique measures the decay of carbon-14 isotopes in organic materials, allowing scientists to determine the age of samples up to about 50,000 years old. It is widely used in Archaeology and Paleontology to date organic remains, such as bones and wood, providing valuable insights into past environments and ecosystems.
Tiny remains of animals and plants in streams come from the mountains. When it rains, these remains are washed down the mountains toward the streams.
decomposes break down the remains of dead plants and animals.
The biological accumulation of the skeletal remains of the plants and animals make up the fossils. A fossil refers to the trace of plants or animals that survived in the past.
A paleontologist studies fossilized remains of plants and animals.
The hardened remains of plants and animals are typically bones or fossils. Fossils are the hardened remains that are formed due to pressure from being squished between Earth's layers.
Dead Organisms Are Compressed By Dirt or Remains Of Dead Animals.
herbivores
lorpumete
fossil fuels
decomposes break down the remains of dead plants and animals.
Sedimentary rocks formed from the remains of plants and animals are called organic sedimentary rocks. Examples include coal, formed from the remains of plants, and limestone, formed from the shells of marine organisms.
Plants use the decaying remains of animals for nutrients. Animals use plants for nutrients and air. Plants also need air in order to survive. Air uses plants to be produced. -CO