Page 92 - Introduction to Paleobiology and The Fossil Record
P. 92

Chapter 4






             Paleoecology and paleoclimates













               Key points

               •  Fossil organisms provide fundamental evidence of evolution; they also allow the recon-
                   struction of ancient animal and plant communities.
               •  Paleoecologists study the functions of single fossil organisms (paleoautecology) or the
                   composition and structure of fossil communities (paleosynecology).
               •  The paleoecology of fossil organisms can be described in terms of their life strategies
                   and trophic modes together with their habitats; virtually all fossil organisms interacted
                   with other fossil organisms and their surrounding environment.
               •  Populations and paleocommunities may be analyzed with a range of statistical
                   techniques.
               •  Evolutionary paleoecology charts the changing structure and composition of paleocom-
                   munities through time.
               •  There have been marked changes in the number and membership of Bambachian mega-
                   guilds (groups of organisms with similar adaptive strategies), the depth and height of
                   tiering, the intensity of predation, and the composition of shell concentrations through
                   time.
               •  Ecological events can be classifi ed and ranked in importance; they can be decoupled in
                   signifi cance from biodiversifi cation events.
               •  Paleoclimates can be described on the basis of climatically-sensitive biotas and sediments
                   together with stable isotopes.
               •  Climate has been an important factor in driving evolutionary change at a number of
                   different levels.
               •  Feedback loops between organisms and their environments indicate that the Gaia
                   hypothesis is a useful model for some of geological time.





                 I do not know what I may appear to the world, but to myself I seem to have been only
                 a boy playing on the sea-shore, and diverting myself in now and then fi nding a smoother
                 pebble or a prettier shell than ordinary, whilst the great ocean of truth lay all undiscovered
                 before me.
                                                  Sir Isaac Newton (shortly before his death in 1727)
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