te and detailed knowledge
of Palaeontology, must have recourse to other and more elaborate
treatises.
UNITED COLLEGE, ST ANDREWS.
October 2, 1876.
CONTENTS.
PART I.
PRINCIPLES OF PALAEONTOLOGY.
INTRODUCTION.
The general objects or geological science--The older theories of
catastrophistic and intermittent action--The more modern doctrines
of continuous and uniform action--Bearing of these doctrines
respectively on the origin or the existing terrestrial
order--Elements or truth in Catastrophism--General truth of the
doctrine of Continuity--Geological time.
CHAPTER I.
Definition of Palaeontology--Nature of Fossils--Different processes
of fossilisation.
CHAPTER II.
Aqueous and igneous rocks--General characters of the sedimentary
rocks--Mode or formation of the sedimentary rocks--Definition
of the term "formation"--Chief divisions of the aqueous
rocks--Mechanically-formed rocks, their characters and mode of
origin--Chemically and organically formed rocks--Calcareous
rocks--Chalk, its microscopic structure and mode of
formation--Limestone, varieties, structure, and origin--Phosphate
of lime--Concretions--Sulphate of lime--Silica and siliceous
deposits of various kinds--Greensands--Red clays--Carbon and
carbonaceous deposits.
CHAPTER III.
Chronological succession of the fossiliferous rocks--Tests or age
of strata--Value of Palaeontological evidence in stratigraphical
Geology--General sequence of the great formations.
CHAPTER IV.
The breaks in the palaeontological and geological record--Use of
the term "contemporaneous" as applied to groups of strata--General
sequence of strata and of life-forms interfered with by more or
less extensive gaps--Unconformability--Phenomena implied by
this--Causes of the imperfection of the palaeontological record.
CHAPTER V.
Conclusions to be drawn from fossils--Age of rocks--Mode of origin
of any fossiliferous bed--Fluviatile, lacustrine, and marine
deposits--Conclusions as to climate--Proofs of elevation and
subsidence of portions of the earth's crust derived from fossils.
CHAPTER VI.
The biological relations of fossils--Extinction of
life-forms--Geological range of different species--Persistent types
of life--Modern origin of existing animals and plants--Reference
of fossil forms to the existing primary divisions of the animal
kingdom--Departure of the older types of life from those now in
existence--Resemblance of the fossils of a gi
|