Book contents
- Frontmatter
- Contents
- List of Contributors
- Preface
- Acknowledgements
- 1 Introduction
- PART I Fossil evidence and phylogeny
- PART II Biogeography and evolutionary biology
- PART III Anatomy of the fossil and living species of Theropithecus
- PART IV Behaviour and ecology of living and fossil species of Theropithecus
- 15 Social organization of the gelada
- 16 The ecology of Theropithecus gelada
- 17 Food digestion and energetic conditions in Theropithecus gelada
- 18 Socioecology of the extinct theropiths: a modelling approach
- 19 Ecological energetics and extinction of giant gelada baboons
- Appendix I A partial catalogue of fossil remains of Theropithecus
- Appendix II Conservation status of the gelada
- Index
18 - Socioecology of the extinct theropiths: a modelling approach
Published online by Cambridge University Press: 11 November 2009
- Frontmatter
- Contents
- List of Contributors
- Preface
- Acknowledgements
- 1 Introduction
- PART I Fossil evidence and phylogeny
- PART II Biogeography and evolutionary biology
- PART III Anatomy of the fossil and living species of Theropithecus
- PART IV Behaviour and ecology of living and fossil species of Theropithecus
- 15 Social organization of the gelada
- 16 The ecology of Theropithecus gelada
- 17 Food digestion and energetic conditions in Theropithecus gelada
- 18 Socioecology of the extinct theropiths: a modelling approach
- 19 Ecological energetics and extinction of giant gelada baboons
- Appendix I A partial catalogue of fossil remains of Theropithecus
- Appendix II Conservation status of the gelada
- Index
Summary
Summary
A systems model of the socioecology of extant gelada is used to predict maximum group sizes for populations of extinct theropiths living under various climatic conditions.
Under present climatic conditions, poor nutritional quality of the graze at low and high altitudes restricts the extant gelada to habitats lying between 1500–4000 m in altitude, but higher latitudes or lower global temperatures would make the colonization of lower altitudes possible.
The theropiths of the Plio-Pleistocene were not large enough to be able to exploit poorer quality vegetation at lower altitudes; consequently, they must have had an even more restricted distribution than the extant gelada.
The largest theropiths of the later Pleistocene could only have survived in the localities where they are known to have occurred if ambient temperatures were at least 6°C cooler than at present or graze quality was at least three times greater than is the case in modern grassland habitats; this suggests that they were restricted to the immediate vicinity of permanent water and thus that they would have been particularly vulnerable to extinction.
The analyses suggest that the largest species could not have lived in groups as large as those of contemporary gelada; nor could they have grown much larger in body size than they did.
Introduction
In this chapter, I use a model of the behavioural ecology of the extant gelada (Theropithecus gelada) to explore the likely constraints acting on the ecology the extinct congeners of this species.
- Type
- Chapter
- Information
- TheropithecusThe Rise and Fall of a Primate Genus, pp. 465 - 486Publisher: Cambridge University PressPrint publication year: 1993
- 12
- Cited by