PP 1: Frameworks of Terrestrial Ecology: Site and Physiography

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Last updated 12:37 AM on 9/8/26
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19 Terms

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Major theme for the class

understanding whole ecosystems


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what is bio-ecology

ecosystems are centered on organisms, added to a non-specific abiotic environment

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what is geo-ecology

ecosystems are centered on geographic spaces, with a focus on the 3-dimensional units in which organisms dwell

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Basic site framework

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Basic site framework: abiotic factors

  • things that make up the physical environment

  • site = sum total of all physical factors of a specific place


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Basic site framework: biotic factors

  • the organisms themselves


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Basic site framework: ecosystem

  • site and biota bonded together, interacting and affecting each other

  • they are convenient to separate, but are inseparable in reality


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We define site along a moisture gradient

  • defined by moisture because that’s where the nutrients are

  • as water goes so does nutrients, so water is a key limiting factor


<ul><li><p>defined by moisture because that’s where the nutrients are</p></li><li><p>as water goes so does nutrients, so water is a key limiting factor</p></li></ul><p></p>
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Physiography: the key to everything

  • physiography is the physical geography of an area (typically geomorphology or topography)

  • we are most interested in ecological geomorphology- studying surface features and their form and substance

  • physiography= form (shape of the land) + substance (parent material)


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Characteristics of physiography include:

  • physiographic setting

  • specific landform

  • parent material of the landform

  • position of the landform in the landscape

  • position of the landform relative to others


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Physiography indirectly affects or controls:

  • macro- and microclimate

  • moisture flux

  • water table position

  • nutrient status


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Physiography also directly or indirectly controls:

  • the likelihood of disturbance

  • species occurrence and composition

  • growth and biomass accumulation

  • how ecosystems change (succession)

  • variation within and among species


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Physiographic systems of our glaciated terrain:

  • Outwash plains

  • Ice contact terrain

  • moraines

  • lake plains


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outwash plains info

  • water laid

  • both dry and wet

  • stratified drift


<ul><li><p><span style="color: rgb(247, 13, 13);">water laid</span></p></li><li><p>both dry and wet</p></li><li><p>stratified drift</p></li></ul><p></p>
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Ice contact terrain

  • water laid

  • includes kames, kettles, and eskers

  • semi-stratified drift


<ul><li><p>water laid</p></li><li><p>includes kames, kettles, and eskers</p></li><li><p>semi-stratified drift</p></li></ul><p></p>
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Moraines information

  • ice laid

  • includes end, ground, and interlobate moraines; unstratified drift


<ul><li><p>ice laid</p></li><li><p>includes end, ground, and interlobate moraines; unstratified drift</p></li></ul><p></p>
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lake plains information

  • lacustrine

  • sand or clay

  • stratified drift


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Physiography affects moisture availability in uplands:

  • water table position

  • capillary fringe

  • perched water table

  • soil texture and structure

  • soil organic matter

  • aspect

  • slope position

  • slope percent

  • spatial relationship to other features


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physiography patterns wetlands across a landscape:

  • poorly- and very-poorly drained soils

  • aeration (moving vs standing water)

  • nutrients affected by parent material and water movement

  • landscape position affects microclimate