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GEOL372 Evolution of New Zealand Biota

Evolution, extinction and other principles of paleontology; fossils, paleoecology and ancient environments; New Zealand Cenozoic fossils and stratigraphy.

Evolution of NZ Biota as revealed by fossils (invertebrates, vertebrates, plants) and some living groups:

  • What's distinctive about the biota from ancient Zealandia to modern NZ
  • Principles and methods of paleontology, evolution and extinction and historical developments
  • Paleoecology and paleoenvironments
  • Biogeographic signals in the NZ biota present and past

Paper title Evolution of New Zealand Biota
Paper code GEOL372
Subject Geology
EFTS 0.1500
Points 18 points
Teaching period First Semester
Domestic Tuition Fees (NZD) $1,018.05
International Tuition Fees (NZD) $4,320.00

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Prerequisite
GEOL 251 and GEOL 252
Restriction
GEOL 272
Schedule C
Science
Contact
geology@otago.ac.nz
Teaching staff
Professor Ewan Fordyce
Paper Structure
The NZ biota, present and past, including:
  • Physiography, climate, ocean circulation
  • Biogeographic signals
Principles and methods of paleontology, including:
  • Development of historical geology
  • Evolution before and after Darwin, extinction
  • Systematics, phylogeny, cladistics
  • Structure and function
Paleoecology and paleoenvironment, including:
  • Principles of ecology and paleoecology
  • Environments past and present
  • Fossils and sedimentology.
  • Taxonomic uniformitarianism - fossils and paleoenvironments
  • Marine paleoecology
  • Plants
  • Vertebrates
  • Trace fossils
Biogeographic signals in the NZ biota, including some combination of:
  • Moas
  • Beech trees
  • Land mammals
  • Cretaceous reptiles
  • Triassic ecosystems
Textbooks
Text books are not required for this paper.
Suggested readings will be identified.
Graduate Attributes Emphasised
Communication, Critical thinking, Environmental literacy, Information literacy, Research, Self-motivation, Teamwork.
View more information about Otago's graduate attributes.
Learning Outcomes
Students should gain understanding of the main macrofossil groups found in New Zealand and some key modern groups and their application to biostratigraphy, paleoecology (especially depositional settings, emphasising stratigraphy and outcrop-level sedimentology) and paleobiogeography (especially related to links with Gondwana and Gondwana breakup).

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Timetable

First Semester

Location
Dunedin
Teaching method
This paper is taught On Campus
Learning management system
Blackboard

Lecture

Stream Days Times Weeks
Attend
L1 Monday 08:00-08:50 9-14, 17-22
Monday 12:00-12:50 9-14, 17-21
Monday 14:00-14:50 22

Practical

Stream Days Times Weeks
Attend
P1 Monday 14:00-16:50 9-14, 17-21
Monday 15:00-16:50 22

Evolution, extinction and other principles of paleontology; fossils, paleoecology and ancient environments; New Zealand Cenozoic fossils and stratigraphy.

Evolution of NZ Biota as revealed by fossils (invertebrates, vertebrates, plants) and some living groups:

  • What's distinctive about the biota from ancient Zealandia to modern NZ
  • Principles and methods of paleontology, evolution and extinction and historical developments
  • Paleoecology and paleoenvironments
  • Biogeographic signals in the NZ biota present and past

Paper title Evolution of New Zealand Biota
Paper code GEOL372
Subject Geology
EFTS 0.1500
Points 18 points
Teaching period Not offered in 2018, expected to be offered in 2019
Domestic Tuition Fees Tuition Fees for 2018 have not yet been set
International Tuition Fees Tuition Fees for international students are elsewhere on this website.

^ Top of page

Prerequisite
GEOL 251 and GEOL 252
Restriction
GEOL 272
Schedule C
Science
Teaching Arrangements
Two lectures and one 3-hour laboratory per week.

Fieldwork:
One-day weekend field trip to South Otago (to study Triassic-Jurassic and Paleocene fossils and strata), normally in the first or second weekend of semester;
One-day weekend field trip to South Canterbury/Waitaki Valley (paleoecology exercise), normally about mid-semester.
Eligibility
Background requirements: 100-level stratigraphy and paleontology. An interest in the modern NZ biota (plants or animals) would be a significant help, though it is not essential.
GEOL 272 is for students in their second year of a geology or equivalent degree. GEOL 372 is for students in their third year of a geology or equivalent degree.
Contact
geology@otago.ac.nz
Teaching staff
Professor Ewan Fordyce
Paper Structure
The NZ biota, present and past, including:
  • Physiography, climate, ocean circulation
  • Biogeographic signals
Principles and methods of paleontology, including:
  • Development of historical geology
  • Evolution before and after Darwin, extinction
  • Systematics, phylogeny, cladistics
  • Structure and function
Paleoecology and paleoenvironment, including:
  • Principles of ecology and paleoecology
  • Environments past and present
  • Fossils and sedimentology
  • Taxonomic uniformitarianism - fossils and paleoenvironments
  • Marine paleoecology
  • Plants
  • Vertebrates
  • Trace fossils
Biogeographic signals in the NZ biota, including some combination of:
  • Moas
  • Beech trees
  • Land mammals
  • Cretaceous reptiles
  • Triassic ecosystems
Assessment is approximately an even split between internal (ongoing during the semester) and external (final exam). The final examination for GEOL 372 differs from that for GEOL 272, to reflect greater background knowledge and higher expectations of students taking the paper at 300-level.
Textbooks
Text books are not required for this paper. Suggested readings will be identified in the peer-reviewed literature.
You should also read relevant sections in the Encylopedia of Geology, accessible under E-journals/E-books via the Library web page.
Graduate Attributes Emphasised
Communication, Critical thinking, Environmental literacy, Information literacy, Research, Self-motivation, Teamwork.
View more information about Otago's graduate attributes.
Learning Outcomes
Students should gain understanding of the main macrofossil groups found in New Zealand and some key modern groups and their application to biostratigraphy, paleoecology (especially depositional settings, emphasising stratigraphy and outcrop-level sedimentology), paleoclimates, and paleobiogeography (especially related to links with Gondwana and Gondwana breakup).

^ Top of page

Timetable

Not offered in 2018, expected to be offered in 2019

Location
Dunedin
Teaching method
This paper is taught On Campus
Learning management system
Blackboard