000 02734nab a2200265 4500
003 OSt
005 20220802175118.0
007 cr aa aaaaa
008 220802b |||||||| |||| 00| 0 eng d
100 _aMiller, Hannah R
_950652
245 _aBiogeomorphic feedbacks and the ecosystem engineering of recently deglaciated terrain/
260 _bSage,
_c2019.
300 _aVol 43, issue 1, 2019 : (24-45 p.).
520 _aMatthews’ 1992 geoecological model of vegetation succession within glacial forefields describes how following deglaciation the landscape evolves over time as the result of both biotic and abiotic factors, with the importance of each depending on the level of environmental stress within the system. We focus in this paper on how new understandings of abiotic factors and the potential for biogeomorphic feedbacks between abiotic and biotic factors makes further development of this model important. Disturbance and water dynamics are two abiotic factors that have been shown to create stress gradients that can drive early ecosystem succession. The subsequent establishment of microbial communities and vegetation can then result in biogeomorphic feedbacks via ecosystem engineering that influence the role of disturbance and water dynamics within the system. Microbes can act as ecosystem engineers by supplying nutrients (via remineralization of organic matter and nitrogen fixation), enhancing soil development, either decreasing (encouraging weathering) or increasing (binding sediment grains) geomorphic stability, and helping retain soil moisture. Vegetation can act as an ecosystem engineer by fixing nitrogen, enhancing soil development, modifying microbial community structure, creating seed banks, and increasing geomorphic stability. The feedbacks between vegetation and water dynamics in glacial forefields are still poorly studied. We propose a synthesized model of ecosystem succession within glacial forefields that combines Matthews’ initial geoecological model and Corenblit's model to illustrate how gradients in environmental stress combined with successional time drive the balance between abiotic and biotic factors and ultimately determine the successional stage and potential for biogeomorphic feedbacks.
650 _a Vegetation,
_950653
650 _a microbes,
_950654
650 _aAlpine,
_950655
650 _a biogeomorphic feedbacks,
_950656
650 _a glacial forefields,
_950657
650 _asuccession
_950658
700 _aLane, Stuart N
_950659
773 0 _012665
_916502
_dLondon: Sage Publication Ltd, 2019.
_tProgress in Physical Geography: Earth and Environment/
_x03091333
856 _uhttps://doi.org/10.1177/0309133318816536
942 _2ddc
_cART
999 _c12667
_d12667