Lecture 20: Paleoecology Flashcards
Paleo:
-older or ancient, often relating to the [geologic] past
Ecology:
-relationships of organisms to one another and to their physical surroundings
Paleoecology
the study of past ecological communities
Paleoecology (extended definition)
the study of past composition and distribution of past ecosystems, and their changes through time on scale of decades to hundreds of millions of years.”
Two Major Types of Paleoecology:
1) Quaternary Paleoecology: Last ~2.8 million years
2) Deep-time Paleoecology: Based on fossils from pre- Quaternary sediments over a wide range of timescales
“Modern” Ecology is Taxonomically resolved whereas paleoecology is…
-temporally resolved
Examples of questions modern ecologists can answer:
- Where (in space) do changes in the environment occur?
- Which species are most affected after spatial disturbances?
- How do species distributions shift over space (e.g., landscapes)?
Examples of questions paleoecologists can answer:
- When (in time) did changes in the environment occur?
- Which species are most affected after temporal disturbances?
- Did the environment change when species were affected?
- How fast do changes take place (what are rates of change)?
most common method, longer record, resolution varies (years represented by each sample)
Piston Cores
less common, shorter core (~one meter), layering is preserved, fine examination is possible
Freeze Cores
The Paleoecological “Proxy”
Physical, chemical, or biological material preserved within the geologic record.
Physical Proxies
- Characteristics like sediment composition, texture, color, density, magnetism, etc.
- Changes in physical properties help infer past climate conditions.
- Environmental change, driven by climate, can alter physical properties of sediments in predictable ways.
Terrestrial Biological Proxies
- Remains of living organisms in terrestrial environments.
- Distribution or organism controlled by temperature, moisture, competition, etc.
- Presence in a sample allows scientists to make inferences about past climate and environmental changes.
- Includes pollen and spores, plant microfossils, charcoal, middens, phytoliths, and even lepidoptera scales
Direct proxy example
(e.g., gases trapped in glacial ice)
Indirect proxy example
(e.g., biological proxy)