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Early Animal life. Fossils Many prehistoric plant and animal fossils have been found in sedimentary rock, particles of rock that have broken off from larger pieces of rock and have been carried away and made even smaller by the grinding of ice, water or wind. The fossilized remains of prehistoric plants and animals have also been founds trapped in ice, tar, peat and even in amber, which is hardened tree sap. Palaeontology, they study of fossils, began in England in the late 17th century. The analysis of fossils and rocks helps palaeontologists understand the history and developments of earth’s life forms and major geographic events. Living and non-living Living things - Living things are called organisms - All organisms can reproduce and metabolize - If something is alive, it can do most of the following: Mrs Ferg Move on its own Respire (breathe) Sense things in its surroundings or environment Feed or nourish itself Excrete Reproduce itself Grow Main differences between plants and animals: Characteristic Plants Animals Where does it get Energy from: Food from photosynthesis Food from eating other organisms How does it move: Usually cannot move itself Usually can move itself Does it have Sense organs: Limited ability to sense things Developed ability to sense things Gas released: Mostly oxygen Carbon dioxide What is its Cell structure: Cellulose cell walls, chloroplasts and vacuoles No cellulose cell walls, chloroplasts or vacuoles