Early Earth and the Evolution of Life

Cell and Organismal Biology         

(This is intended to present a brief sketch of the evolution of our planet.    It is not, nor is it intended to be, an all inclusive history.)

 

TO THE URSULINE ACADEMY BIOLOGY HOMEPAGE, SOURCE OF THIS OUTLINE

     The Beginning

          Big Bang- Creation of the Universe

          Earth formed

               4.6 billion years ago

               cloud of gas and dust condensed into a sphere

               heat and radioactivity caused the planet to melt

 

     Early Earth

          Some cooling-- solid rocks formed~4 billion years ago-- Earth's Crust

          Volcanic activity-- violent and planet-wide

          Meteor shower bombards Earth

          Earth's Atmosphere 4- 3.8 billion years ago

               Volcanoes- CO2, N2 and other gases

               Meteorites- carry water in the form of ice, as well  as other substances

               Composition: CO, CO2, H2, N2, NH3, CH4 and water vapor (H2O)

               No free oxygen!

 

     Oceans

          Earth cooled enough for liquids to remain

          Thunderstorms drenched planet for thousands of years- forming oceans

          Earliest sedimentary rocks dated to this period

 

     Chemosynthesis Hypothesis

          Methane (CH4), ammonia (NH3), hydrogen (H2) and water vapor (H2O) from

               the earth's   atmosphere,

          Combined with UV rays and lightening, 

          Formed organic compounds, such as amino acids

          Thus, leading to the "Organic Soup".

 

     Evidence-1

          Stanley Miller

          Simulated Chemosynthesis Hypothesis in the laboratory

          Yielded amino acids, as well as, many other organic compounds

 

     Evidence 2

          Alexander Oparin and Sidney Fox

          Demonstrated that the organic soup would not remain a mix of simple

               molecules, but that

          More complex molecules (such as proteins) would be formed.

 

     Evidence-3

          Collections of the more complex molecules in the "organic soup" tend to

               gather into droplets.

          Some of these grow, and some reproduce.

          Called proto-life forms, because they have begun some tasks necessary for life.

 

     First Life

          Microfossils found near Lake Superior have been dated to 3.5 billion years old

          Prokaryotes- resembling bacteria

          Anaerobic- can live without oxygen

          Heterotrophs- obtained food and energy from the organic molecules in the soup

 

     Evolution of Photosynthesis-1

          Complex molecules in organic soup begin to run out.

          Some organisms have developed a method of making complex organic

               compounds using H2S and CO2.

          Competition for the food in the organic soup gives these autotrophs an advantage.

 

     Evolution of Photosynthesis-2

          Organisms who can make their own "food" have a better chance of survival.

          Evolution of autotrophs was very successful.

          Autotrophs became very commonplace all over Earth.

 

     Evolution of Modern Photosynthesis

          Organisms begin using H2O instead of H2S.

          The waste product, oxygen gas (O2), is formed instead of sulfur.

          Free oxygen is released into the atmosphere for the first time.

 

     Effects of Atmospheric  Oxygen Aerobes

          Oxygen is poisonous to most anaerobes

          Therefore, the majority of anaerobes that filled the oceans died.

          Evolution of aerobes-- Most anaerobes that survived began to use

               oxygen in their respiration.

          These organisms were more energy efficient than the remaining anaerobes,

               and so they proliferated.

 

     Effects of Atmospheric Oxygen Ozone

          Oxygen accumulated in the atmosphere.

          Oxygen in the upper atmosphere was split by UV rays into single atoms.

          These single atoms recombined to form O3, ozone.

 

     Effects of Atmospheric Oxygen Life on Land

          Ozone accumulated in the atmosphere.

          Ozone absorbed most of the harmful UV rays, making land a possible

               habitat for organisms.

          Organisms came out of the oceans and onto the land.

 

     Some Problems Encountered on Land

          How to keep from drying out?

          How to get oxygen?

          How to move?

          How to reproduce?

 

     Evolution of Monerans

          First to evolve

          All are prokaryotic

          Includes blue-green algae (cyanobacteria), and other bacteria

 

     Evolution of Protists

          Evolved from Monerans.

          Very diverse.

          Gave rise to all other eukaryotic organisms.

          Includes the green algae.

 

     Evolution of Fungi

          Most are multicellular heterotrophic eukaryotes

          Absorb dissolved organic substances from the surrounding environment

          A few are unicellular, such as yeast.

 

     Evolution of Plants -1

          All evolved from the green algae.

          Multicellular photosynthetic eukaryotes

          Adapted for life on land

 

     Evolution of Plants-2 Why Was It Easy For Plants To Adapt to Land?

          Light was abundant and not blocked by water

          CO2 was plentiful and circulated more freely

          Initially the land was unoccupied by competing forms of life

 

     Evolution of Plants-3 Plant Adaptations to Land

          A waxy coating to prevent water loss

          Stomata for gas exchange

          Reproductive organs protected from drying out by surrounding layers of cells

          Retention of fertilized egg and the development into an embryo

          Vascular systems evolved for transporting substances throughout the plant.

 

     Evolution of Animals

          All are multicellular heterotrophic eukaryotes

          All lack cell walls

          Mobility (of the entire organism or some of its parts) was required for obtaining food

 

     Sequence of Animal Evolution-1

          Sponges (Phylum Porifera)- did not evolve into any other group

          Jellyfish (Phylum Cnidaria)- radially symmetrical

          Flatworms (Phylum Platyhelminthes)

               may have evolved from Cnideria

               bilateral symmetry and ganglia

          Ribbonworms (Phylum Rhynchocoala)

               evolution of 1 way digestive tract

               evolution of primitive circulatory system

          Roundworms (Phylum Nematoda)- presence of pseudocoelom

          Mollusks (Phylum Mollusca)-

               most have shells (except octopus)

               coelom

          Segmented worms (Phylum Annelida)

               body divided into segments

               coelom

               example: earthworm

          Arthropods (Phylum Arthropoda)

               most numerous and diverse

               three major Classes:

                    Class: Arachnids-spiders, ticks, horseshoe crabs

                    Class: Insects- grasshoppers

                    Class: Crustaceans- lobsters

          Echinoderms (Phylum Echinodermata)

               body divided into 5 segments

               example: starfish, sanddollar

          Chordates (Phylum Chordata)

               presence of a notochord

               bilaterally symmetrical

               Subphylum: Vertebrata

                    segmented vertebral column-- a backbone

                    distinct head with a skull and brain

                    nerve chord protected by vertebral column.

                    Classes of Fish- evolution of the first jaws

                         Class Agnatha- lampreys and hagfish

                              jawless;

                             eel-like (no fins)

                         Class Chondrichthyes- sharks, rays,

                             skeleton of cartilage;

                             scales pointed

                         Class Osteichthyes- bony fish

                             bony skeletons;

                             fins;

                             scales;

                             air bladders.

                    Class: Amphibians

                        egg laying

                        have gills in larvae stage; lungs in adult stage

                        depend on moist environment for at least one part of their life cycle.

                        water evaporates rapidly from their skins

                        evolved from air-breathing lunged fish

                        ectothermic

                   Class: Reptiles (reptiles)

                        evolved from amphibians

                        developed the amniotic egg

                        scales

                        ectothermic

                   Class:  Aves  (Birds)

                        evolved from reptiles (specialized reptiles)

                        feathers

                        forelimbs are modified into wings

                        all lay amniotic eggs

                        endothermic

                  Class:  Mammals

                        hairy

                        mammary glands

                        endothermic

                        descended from reptiles

                     Order: Monotremes

                           transitional forms

                          duckbill platypus and spiny anteater

                     Order: Marsupials

                           pouched mammals

                           kangaroo and opossum

                     Order: Placentals- mammals with a placenta

                          Primates

                               New World Monkey- grasping tails

                               Old World Monkey- brachiation

                               Hominoids

                                     Gibbon

                                     Orangutan

                                     Gorilla

                                     Chimpanzee

                                     Hominid

                                           MAN- Homo sapien

 

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