Title page for ETD etd-04042007-122740


Type of Document Dissertation
Author Dong, Lin
Author's Email Address lindong@vt.edu
URN etd-04042007-122740
Title Contributions to the Proterozoic and Cambrian Evolution of Eukaryotes
Degree PhD
Department Geosciences
Advisory Committee
Advisor Name Title
Xiao, Shuhai Committee Chair
Dove, Patricia M. Committee Member
Kowalewski, Michal Committee Member
Read, James Fredrick Committee Member
Scheckler, Stephen E. Committee Member
Keywords
  • Ediacaran
  • South China
  • Protoarenicola
  • Pararenicola
  • Sinosabellidites
  • heterotrophic
Date of Defense 2007-03-27
Availability unrestricted
Abstract
This thesis makes several contributions to improve our understanding of

Proterozoic-Cambrian evolution of eukaryote life. Chapter 1 provides, for the first time, a quantitative characterization of the evolutionary trends of Proterozoic macroalgae. The analysis reveals that morphological disparity of Paleoproterozoic macroalgae was low but increased in the Mesoproterozoic and Ediacaran, with a plateau in between. There was also a significant increase in thallus surface/volume ratio and maximum canopy height of the Ediacaran macroalgal communities. The prolonged plateau between the Mesoproterozoic and Ediacaran may be related to either nutrient stress or the absence of animal grazing pressure. The Ediacaran increase in surface/volume ratio and morphological complexity may have been driven by decreasing pCO2 levels and increasing animal grazing pressure.

Chapter 2 presents a systematic re-examination of the carbonaceous compression fossils Protoarenicola baiguashanensis Wang, 1982, Pararenicola huaiyuanensis Wang, 1982, and Sinosabellidites huainanensis Zheng, 1980, from the early Neoproterozoic Liulaobei and Jiuliqiao formations in northern Anhui, North China. These fossils were previously interpreted as worm-like metazoans. Our study reveals new morphological features that weaken the metazoan interpretation. Instead, the new data indicate that these fossils can be alternatively interpreted as erect epibenthic organisms, possibly coenocytic algae.

Chapter 3 examines two important eukaryote fossils: Horodyskia Yochelson and Fedonkin, 2000, and Palaeopascichnus Palij, 1976, from the upper Ediacaran chert of the Liuchapo Formation in central Guizhou, South China. These exceptionally preserved fossils offer us a unique opportunity to investigate their body constructions and affinities. The morphologies of Horodyskia and Palaeopascichnus support a phylogenetic relationship with agglutinated foraminifers, shedding new light on the divergence of bikont eukaryotes, the rise of rhizarians, and the ecological importance of heterotrophic eukaryotes in Proterozoic ecosystems.

Chapter 4 focuses on Cambrian microfossils that represent the primary producers—cyanobacteria and eukaryotic phytoplankton (acritarchs). Careful investigation of the basal Cambrian Yanjiahe Formation in the Yangtze Gorges area and the Yurtus Formation in the Aksu area revealed abundant acanthomorphic acritarchs, clustered coccoidal microfossils, filamentous cyanobacteria, and tubular microfossils. This study confirms previous stratigraphic correlation between the Yanjiahe and Yurtus formations and suggests that animals and phytoplankton radiated in tandem during the Cambrian explosion.

Files
  Filename       Size       Approximate Download Time (Hours:Minutes:Seconds) 
 
 28.8 Modem   56K Modem   ISDN (64 Kb)   ISDN (128 Kb)   Higher-speed Access 
  DongDissertation2007final.pdf 166.23 Mb 12:49:35 06:35:47 05:46:18 02:53:09 00:14:46

Browse All Available ETDs by ( Author | Department )

dla home
etds imagebase journals news ereserve special collections
virgnia tech home contact dla university libraries

If you have questions or technical problems, please Contact DLA.