Biology 1010 Lecture Notes
Unit 3. Multicellular organisms
These notes were last updated Ocotober 24, 2001
Some key words, phrases, and ideas :
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multicellularity and organization: symmetry and cephalization; skeletal
systems; digestive systems; nervous systems
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coelom vs pseudocoelom; proterostomes vs deuterostomes
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sporophyte, gametophyte; ovules, seeds, pollen
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amniote eggs; stem amniote; terapsids and thecodonts
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Life in the Proterozoic
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status of life during the early Proterozoic
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origins of multicellularity
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what is multicellularity
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features of multicellular animals
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colonial aggregates to specialized tissues to specialized organs
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symmetry; cephalization and sensory systems
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skeletal/muscular systems
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digestive systems
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coeloms and pseudocoeloms
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protostomes and deuterostomes
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protostomes: mouth develops from the blastopore, spiral and determinate
cleavage, coleom develops from a split in the mesoderm
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deuterostomes: anus develops from the blastopore (mouth develops later),
radial and indeterminate cleavage, coelom develops from the digestive system
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early evolution of multicellular animals
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porifera (sponges)
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sessile filter-feeders (flagellate cells similar in shape to some types
of zooflagellates)
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primitive organization without well-defined tissues and organs
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structural framework of spicules/spongin
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cnidarians (jelly fish and corals)
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radial symmetry
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well-developed tissues but no organs
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beginnings of a digestive system and neuromuscular system
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cnidocytes with nematocysts
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polyp and medusa stages
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some colonial forms
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flatworms (turbellarians)
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bilateral symmetry--cephalization
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three basic tissues plus true organs
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digestive system
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eyespots and nervous system
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excretory system
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rotifers and nematodes
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bilateral, some with good cephalization
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three basic tissues plus true organs
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one-way digestive system
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ventral nerve cord and a ring-type brain
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pseudocoelom
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determinate development
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protostomes lineages
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mollusks (gastropods and cephalopods)
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body plan: visceral mass, mantle and mantle cavity, foot
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most with radula
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three important groups
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cephalopods -- foot divided into tentacles with suckers; well-developed
nervous system
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gastropods -- body twists during development; spiral shells
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bivalves -- right and left shells
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annelids (segmented worms, including leeches)
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onychophorans (segmented worms with primitive appendages)
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marine arthropods (trilobites, chelicerates, crustaceans)
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common features include a jointed exoskeleton, segmented body with usually
with some degree of specialization, complex nervous systems often with
compound eyes
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three important aquatic lineages
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trilobites (extinct group with a lobed body)
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chelicerates (horseshoe crabs and arachnids (spiders, scorpions, ticks,
and mites))
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usually body divided into cephalothorax and abdomen
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first pair of appendages are chelicerae, second pair are pedipalps; these
are followed by multiple pairs of walking legs
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breathe through book gills or book lungs
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crustaceans (crabs, copepods, cladocerans, barnacles, isopods (pill bugs),
and amphipods)
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body divided into cephalothorax and abdomen
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appendages are biramous (with two branches)
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first two pairs of appendages are antennae, the next three are modified
for chewing (mandibles and maxillae)
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deuterostome lineages
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echinoderms (starfish and sea urchins)
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secondary 5-fold radial symmetry
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unique tube feet
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carbonate plates just below the skin
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protochordates (arrow worms and acorn worms)
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arrow worms -- torpedo-like body with a tail extending past the anus; common
predators in the plankton
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acorn worms -- proboscis (trunk or nose) for gathering food and a worm-like
body; common benthic animals, some around the deep-sea vents; key features
for us include
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pharyngeal gill slits
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hollow dorsal nerve cord
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rudimentary cartilaginous skeleton
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chordates
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defining characteristics
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pharyngeal gill slits
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tail extending past the anus
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hollow dorsal nerve cord
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dorsal notochord
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major lineages
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urochordates (tunicates and the like)
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cephalochordates (lancelets)
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vertebrates
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Life in the Paleozoic (545 to 245 million years ago)
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early Paleozoic
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Cambrian seas--dominated by trilobites and brachiopods, with primitive
molluscs and echinoderms common; chordates are poorly represented in the
fossil record (ends 505 million years ago)
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Ordovician seas--trilobites and ammonites common as are starfish, corals,
gastropods, and bivalves (
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rise of the vertebrates
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armored agnathan fish--dominant vertebrates in the Ordovician and most
of the Silurian; with armor plates, but no jaws or vertebrae (use notochord)
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placoderm (jawed) fish--rose to dominance among the vertebrates in the
Silurian; armored, with jaws derived from gills, and a partially calcified
skeleton
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modern fishes--chondrichthyes (sharks and rays) and osteichthyes (bony
fish)
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arose from placoderms during the Devonian
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sharks are marine organisms with gill slits, fixed fins, torpedo shape,
cartilaginous endoskeleton,and no swim bladder
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bony fish started as fresh water organisms with gill opening, moveable
fins, variable shape, bony endoskeleton, and with a swim bladder (why?)
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movement to land (late Silurian early Devonian--about 400 million years
ago)
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requirements
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resistance to or protection from drying out
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resistance to or protection from ultraviolet light
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support structures
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some way to bring gametes together
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temperature regulation
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early colonizers
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algae and fungi
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spore plants
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eggs and zygotes protected in archegonium
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improvements in water relations in sporophyte
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stomata
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vascular tissue (also useful for support)
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difficulties with fertilization (bring sperm to the egg)
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uniramian arthropods (millipedes and centipedes, insects)
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exoskeleton for support, movement, protection from drying and UV
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many breathe through trachea (internal)
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many use internal fertilization
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many primitive forms eat microorganisms (bacteria, fungi, algae) already
present
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chelicerates
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exoskeleton for support, movement, protection from drying out and UV
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enclosed book gills to make book lungs
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many use internal fertilization
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probably ate uniramians
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amphibians
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endoskeleton from support and movement
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breathe through modified swim bladder (lungs), supplement in some cases
with skin breathing
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early forms retained scaly exterior (similar to early fish) providing some
protection from drying and UV
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fertilization still external, eggs unprotected, therefore eggs laid in
water, juveniles spend some time in water (tadpoles)
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origins of seed plants
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some spore plants developed separate male and female gametophytes (micro-
and macrogametophytes)
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some of these were provided with protective structures composed of sporophyte
tissue
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pollen grains (with a much reduced male gametophyte) and ovules (with a
female gametophyte) eventually evolved from these; seeds are mature ovules
with a developing sporophyte embryo inside (for a total of three generations)
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the evolution of seeds and improvements in the water relations of the sporophyte
allowed them to spread into drier areas
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origins of amniote eggs
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amniote eggs--new type of vertebrate egg with four basic membranes: amnion
(amniotic sac) containing amniotic fluid (a pool for the embryo to develop
in); yolk sac providing nourishment; allantois for waste; chorion associated
with shell formation
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organisms with amniote eggs and internal fertilization were no longer tied
to pools of water for reproduction; this lead to another period of adaptive
radiation in vertebrates
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important amniote lineages
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thecodonts and archosaurs
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pelycosaurs and therapsids
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ichthyosaurs and plesiosaurs
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lizards and snakes
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turtles
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by the end of the Paleozoic
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seas full of sharks and fish, modern-looking invertebrates, algae
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land covered in spore plants with growing numbers of seed plants; insects
and arachnids common, vertebrate life dominated by therapsids (Dimetrodon)
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Terrestrial life in the Mesozoic (245 to 65 million years ago)
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status of life at the beginning of the Mesozoic
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dinosaurs, birds, and mammals
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the question of warm-bloodedness
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advantages and disadvantages
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tests for warm-bloodness
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were dinosaurs warm-blooded
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evolution of mammals
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basic features: mammary glands, hair, external ears
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origins
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flowering plants
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new structures
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ovaries, carpels, and pistils; fruits
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stamens with anthers
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sepals and petals
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connections with pollination
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status of life at the end of the Mesozoic
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Terrestrial life in the Cenozoic
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status of life at the beginning of the Cenozoic
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rise and adaptive radiation of the mammals
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origins of humans
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earliest primates small, tree-dwelling, nocturnal, insect-eaters with with
grasping fingers and toes, binocular vision; split into two lineages, the
prosimians (lemurs and tarsiers) and the anthropoids
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anthropoids (monkey-like primates) are mostly diurnal, mostly plant-eaters,
with relatively large brains; most form complex social groups; split into
two lineages about 30 million years ago, the old world monkeys and the
new world monkeys
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hominoids split from the old world monkeys about 25 million years ago;
modern representatives include orangutans, gibbons, chimps, and gorillas
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hominids split from the hominoids about 8 million years ago in Africa;
basic change--bipedal
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genus Australopithecus--bipedal, brains about 500 cc; many species
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genus Homo--first appearance about 2.5 million years ago; distinguished
by slightly larger brains (700 cc) and primitive tools
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the number of early species is somewhat controversial, might include Homo
habilis, Homo rudolfensis, and Homo ergaster, might all
be representatives of one species, Homo habilis
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Homo erectus first appeared about 1.5 million years ago; distinguished
by larger brain (1000 cc), more advanced tools, definite social groupings;
spread from Africa throughout the Old World
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Homo sapiens first appeared between 0.5 and 0.2 million years ago;
marked by still larger brain size (1450 cc) and cosntantly improving tools;
spread from Africa throughout world starting about 0.1 million years ago,
reaching the New World about 0.01 million years ago; may soon spread to
other planets in the solar system
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