Biogeomorphology
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upright=1.35, Slope stabilization by Chilean_rhubarb_on_the_coasts_of_Chacao_Channel._Vegetation_have_mostly_a_protective_effect_on_slopes..html" ;"title="Chacao_Channel.html" ;"title="Chilean rhubarb on the coasts of Chacao Channel">Chilean rhubarb on the coasts of Chacao Channel. Vegetation have mostly a protective effect on slopes.">Chacao_Channel.html" ;"title="Chilean rhubarb on the coasts of Chacao Channel">Chilean rhubarb on the coasts of Chacao Channel. Vegetation have mostly a protective effect on slopes. Biogeomorphology and ecogeomorphology are the study of interactions between organisms and the development of landforms, and are thus fields of study within geomorphology and ichnology. Organisms affect geomorphic processes in a variety of ways. For example, trees can reduce landslide potential where their
root In vascular plants, the roots are the organs of a plant that are modified to provide anchorage for the plant and take in water and nutrients into the plant body, which allows plants to grow taller and faster. They are most often below the su ...
s penetrate to underlying
rock Rock most often refers to: * Rock (geology), a naturally occurring solid aggregate of minerals or mineraloids * Rock music, a genre of popular music Rock or Rocks may also refer to: Places United Kingdom * Rock, Caerphilly, a location in Wales ...
,
plant Plants are predominantly photosynthetic eukaryotes of the kingdom Plantae. Historically, the plant kingdom encompassed all living things that were not animals, and included algae and fungi; however, all current definitions of Plantae exclu ...
s and their
litter Litter consists of waste products that have been discarded incorrectly, without consent, at an unsuitable location. Litter can also be used as a verb; to litter means to drop and leave objects, often man-made, such as aluminum cans, paper cups ...
inhibit soil erosion, biochemicals produced by plants accelerate the chemical
weathering Weathering is the deterioration of rocks, soils and minerals as well as wood and artificial materials through contact with water, atmospheric gases, and biological organisms. Weathering occurs ''in situ'' (on site, with little or no movement) ...
of bedrock and
regolith Regolith () is a blanket of unconsolidated, loose, heterogeneous superficial deposits covering solid rock. It includes dust, broken rocks, and other related materials and is present on Earth, the Moon, Mars, some asteroids, and other terrestr ...
, and marine
animal Animals are multicellular, eukaryotic organisms in the Kingdom (biology), biological kingdom Animalia. With few exceptions, animals Heterotroph, consume organic material, Cellular respiration#Aerobic respiration, breathe oxygen, are Motilit ...
s cause the bioerosion of
coral Corals are marine invertebrates within the class Anthozoa of the phylum Cnidaria. They typically form compact colonies of many identical individual polyps. Coral species include the important reef builders that inhabit tropical oceans and ...
. The study of the interactions between marine biota and coastal landform processes is called coastal biogeomorphology. Phytogeomorphology is an aspect of biogeomorphology that deals with the narrower subject of how terrain affects plant growth. In recent years a large number of articles have appeared in the literature dealing with how terrain attributes affect crop growth and yield in farm fields, and while they don't use the term phytogeomorphology the dependencies are the same.
Precision agriculture Precision agriculture (PA) is a farming management strategy based on observing, measuring and responding to temporal and spatial variability to improve agricultural production sustainability. It is used in both crop and livestock production. ...
models where crop variability is at least partially defined by terrain attributes can be considered as phytogeomorphological precision agriculture.


Overview

Biogeomorphology is a multidisciplinary focus of geomorphology that takes research approaches from both geomorphology and ecology. It is a sub discipline of geomorphology. Biogeomorphology can be synthesized into two distinct approaches: 1. The influences that geomorphology plays on the biodiversity and distribution of flora and fauna. 2. The influences that biotic factors have on the way landforms are developed. There has been much work on these approaches such as; the effect that parent material has on the distribution of plants, the increase of precipitation due to an influx of
transpiration Transpiration is the process of water movement through a plant and its evaporation from aerial parts, such as leaves, stems and flowers. Water is necessary for plants but only a small amount of water taken up by the roots is used for growth ...
, the stability of a hillslope due to the abundance of vegetation or, the increase of
sedimentation Sedimentation is the deposition of sediments. It takes place when particles in suspension settle out of the fluid in which they are entrained and come to rest against a barrier. This is due to their motion through the fluid in response to the ...
due to a beaver dam. Biogeomorphology shows the axiomatic relationship between certain land forming processes and biotic factors. That is, certain geomorphic processes shape the biota and biotic factors can shape land forming processes.


Origins and early work

The earliest work related to biogeomorphology was
Charles Darwin Charles Robert Darwin ( ; 12 February 1809 – 19 April 1882) was an English naturalist, geologist, and biologist, widely known for his contributions to evolutionary biology. His proposition that all species of life have descended ...
's 1881 book titled ''
The Formation of Vegetable Mould through the Action of Worms #REDIRECT The Formation of Vegetable Mould Through the Action of Worms #REDIRECT The Formation of Vegetable Mould Through the Action of Worms {{R from other capitalisation ...
{{R from other capitalisation ...
''.Darwin, C. 1881. "The Formation of Vegetable Mould, Through the Action of Worms, with Observations on their Habits." London: John Murray.Tsikalas, S.G., Whitesides, C.J. 2013. Worm geomorphology: lessons from Darwin. "Progress in Physical Geography" 37(2):270-281. Although the field of biogeomorphology had not yet been named, Darwin's work represents the earliest examination of a faunal organism influencing landscape process and form. Charles Darwin begins his work on worms with an examination of behavior and physiology, which then moves towards topics related to geomorphology, pedogenesis, and bioturbation. Observations and measurements of soil moved by earthworms, and emphasis on the role of earthworms in formation of humus, fertility of soils, and mixing of soils were all described in the book, which began to change the perspective on earthworms from pest to critical agent of pedogenesis.Meysman, F.J.R., Middelburg, J.J., Heip, C.H.R. 2006. Bioturbation: a fresh look at Darwin's last idea. "Trends in Ecology and Evolution" 21(12): 688-695. Despite the popularity of Darwin's final work, the scientific community was slow to recognize the significance of examining the role of organisms in influencing landscapes.Butler, D.R., Hupp, C.R. 2013. The role of biota in geomorphology: ecogeomorphology. Ed. Shroder, J.F. Treatise on Geomorphology, Volume 12. Elsevier: London. It wasn't until the late twentieth century that biogeomorphology began attracting the attention of more than a handful of researchers.


Research approaches

There are two approaches to research in biogeomorphology. One is through the statistical and empirically derived means. This is an approach commonly used in the fields of
ecology Ecology () is the study of the relationships between living organisms, including humans, and their physical environment. Ecology considers organisms at the individual, population, community, ecosystem, and biosphere level. Ecology overl ...
and
biology Biology is the scientific study of life. It is a natural science with a broad scope but has several unifying themes that tie it together as a single, coherent field. For instance, all organisms are made up of cells that process hereditary i ...
. The approach is simply to employ large replication studies and deriving patterns from statistical data. Whereas taking a more geomorphic research approach tends to derive patterns via theoretic knowledge and detailed measurements of multiple factors. In turn, this uses smaller sample sizes than that of large replication studies.


Biogeomorphological processes

There are several biogeomorphological processes. Bioerosion is the weathering and removal of abiotic material via organic processes. This can either be passive or active. Moreover, bioerosion is the chemical and or the mechanical weathering of landforms due to organic means. Bioprotection is essentially the effect that organisms have on reducing the action of geomorphic processes. Best shown by algae covering a rock surface acts as a buffer from the waves erosive work. Bioconstruction refers to bioconstructors or ecosystem engineers. Ecosystem engineers are organisms that build mounds, dams, reefs &c. More specifically they are organisms that change the environment physically, directly or indirectly controlling the abundance of resources available in the environment accessible to organisms.


Themes of complex systems in biogeomorphology

There are four main themes that underline the complex systems within biogeomorphology. The first of which is multiple casualty. Multiple casualty is the way in which biota is deposited. More specifically, multiple casualty is caused by various processes. That is, processes such as fires, floods and hillslope instability directly or indirectly determining the distribution of flora and in turn fauna. Ecosystem engineers are another theme underlying complex system of biogeomorphology. These organisms have the most profound effect on the overall ecosystem structure. Some of the most common ecosystem engineers are earthworms. Earthworms aid in the production of humus and increase both soil aeration and area for roots and root hairs to utilize. With more space for roots, this can increase soil stability. Another strong example of ecosystem engineers are beavers. Beavers can increase the sedimentation in a channel as well as increase runoff rates due to a reduction of vegetative cover needed to build their dams. Ecological topology is another theme of complex systems in biogeomorphology. This theme focuses on how the biota varies based on geographic location. This ecological topology is controlled by a concept called stability domain. Stability domain describes the interaction of a set species and certain abiotic factors that act as a medium to the function and structure of an environment. The final of the four underlying themes of the complex systems in biogeomorphology is ecological memory. Ecological memory is where certain biotic and abiotic factors have a recursive relationship and therefore can be encoded in organisms and the immediate environment. An example of this can simply be the flame retardant properties in the bark of Coastal Sequoias due to the recurrence of fires


Climate change

Biogeomorphology and ecogeomorphology can aid with assessing the impacts of global climate change. This can especially be seen in coastal and estuarine systems due to; sea level rise, increased global temperatures, increased sea temperature, a higher frequency in and intensity of storms, and varying distributions of precipitation. Biogeomorphology can outline some of the effects of climate change due to biocomplexity. Biocomplexity is in reference to the complex way in which organisms interact with their environment and its effect on
biodiversity Biodiversity or biological diversity is the variety and variability of life on Earth. Biodiversity is a measure of variation at the genetic (''genetic variability''), species (''species diversity''), and ecosystem (''ecosystem diversity'') l ...
. Using statistical data, one can derive how these environmental changes will affect the biodiversity of different trophic levels and different keystone species.


See also

* Biogeology * Biogeophysics * Coastal biogeomorphology * Phytogeomorphology


References


Bibliography

* * *{{cite conference, last=Osterkamp, first=W.R., author2=Friedman, J.M., title=Research Considerations for Biogeomorphology, book-title=Proceedings of the U.S. Geological Survey (USGS) Sediment Workshop 'Expanding Sediment Research Capabilities in Today's USGS', place=Reston, VA, and Harpers Ferry, WV, year=1997, url=http://water.usgs.gov/osw/techniques/workshop/osterkamp.html, access-date=2007-06-15


External links


Biogeomorphology Platform at Delft University of Technology