Book contents
- Frontmatter
- Contents
- List of contributors
- Preface
- PART I Introductory perspectives
- PART II Theory, experiments, and models in landscape ecology
- PART III Landscape patterns
- PART IV Landscape dynamics on multiple scales
- 14 Landscape sensitivity and timescales of landscape change
- 15 The time dimension in landscape ecology: cultural soils and spatial pattern in early landscapes
- 16 The legacy of landscape history: the role of paleoecological analysis
- 17 Landscape ecology and global change
- PART V Applications of landscape ecology
- PART VI Cultural perspectives and landscape planning
- PART VII Retrospect and prospect
- Index
- Plate section
- References
14 - Landscape sensitivity and timescales of landscape change
from PART IV - Landscape dynamics on multiple scales
Published online by Cambridge University Press: 20 November 2009
Book contents
- Frontmatter
- Contents
- List of contributors
- Preface
- PART I Introductory perspectives
- PART II Theory, experiments, and models in landscape ecology
- PART III Landscape patterns
- PART IV Landscape dynamics on multiple scales
- 14 Landscape sensitivity and timescales of landscape change
- 15 The time dimension in landscape ecology: cultural soils and spatial pattern in early landscapes
- 16 The legacy of landscape history: the role of paleoecological analysis
- 17 Landscape ecology and global change
- PART V Applications of landscape ecology
- PART VI Cultural perspectives and landscape planning
- PART VII Retrospect and prospect
- Index
- Plate section
- References
Summary
Ideas concerning what is now usually termed “landscape sensitivity” have been a part of geomorphological thinking for half a century, illustrated by the concepts of biostasie and rhexistasie formulated by Erhart (1955) to describe the switch from biogeochemical equilibrium and chemical sedimentation to conditions of erosion and clastic sedimentation. However, the term was first used explicitly by Brunsden and Thornes (1979) to assist understanding of episodes of accelerated erosion and sedimentation as they affect the natural landscape. Although widely employed, the concept has received less attention than might have been expected, and was not widely reviewed until D. Thomas and Allison (1993) brought together a series of papers to show the impacts of environment and land-use changes on landscapes. More recently, another symposium has reviewed the concept and its applications (M. Thomas and Simpson, 2001).
The notion of sensitivity is related to the concept of erosion thresholds and to other aspects of systems analysis, widely discussed since the publication of papers by Knox (1972), Schumm and Parker (1973), and Schumm (1977, 1979) in the 1970s. But “landscape” is a complex entity that has proved difficult to subject to systems analysis. Most geomorphologists have felt more at home with research into fluvial and hillslope systems, and issues concerning landscape per se have received less attention. Often this has implied a lack of emphasis on the role of the vegetation cover and much greater concern with stream channels than with interfluves and hillslopes.
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- Issues and Perspectives in Landscape Ecology , pp. 131 - 151Publisher: Cambridge University PressPrint publication year: 2005
References
Alexander, R. W., Harvey, A. M., Calvo, A. C., James, P. A., and Carda, A. (1994). Natural stabilisation mechanisms on badland slopes. In Environmental Change in Drylands: Biogeographical and Geomorphological Perspectives, ed. , and . Chichester: Wiley, pp. 85–111.Google Scholar
, and (1998). Correlated millennial-scale changes in surface hydrography and terrigenous sediment yield inferred from last-glacial marine deposits off northeastern Brazil. Quaternary Research, 50, 157–166.CrossRefGoogle Scholar
(1993). Rainfall and slope failure in Hong Kong. Engineering Geology, 36, 141–147.CrossRefGoogle Scholar
(1987). Palaeoflood hydrology and extraordinary flood events. Journal of Hydrology, 96, 77–99.CrossRefGoogle Scholar
(2002a). Paraglacial geomorphology. Quaternary Science Reviews, 21, 1935–2017.CrossRefGoogle Scholar
(2002b). A general model of paraglacial landscape response. The Holocene, 12, 371–376.CrossRefGoogle Scholar
, , and (1997). Interhemispheric synchrony of the last deglaciation inferred from alkenone palaeothermomotry. Nature, 385, 707–710.CrossRefGoogle Scholar
, , and (2000). Hydrological impact of Heinrich events in the subtropical northeast Atlantic. Science, 289, 1321–1324.CrossRefGoogle ScholarPubMed
and (1997). Phases of enhanced rapid mass movement and climatic variation during the Holocene: a synthesis. Paläoklimaforschung Palaeoclimate Research, 19, 409–440.Google Scholar
, and (1994). Fluvial response to late Quaternary climatic and environmental change, Edwards Plateau, Texas. Palaeogeography, Palaeoclimatology and Palaeoecology, 108, 1–21.CrossRefGoogle Scholar
, , , et al. (1997). A pervasive millennial-scale cycle in North Atlantic Holocene and Glacial climates. Science, 278, 1257–1266.CrossRefGoogle Scholar
(1980). Widespread episodes of stream erosion during the Holocene and their climatic cause. Nature, 283, 655–656.CrossRefGoogle Scholar
Brown, A. G. (1996). Human dimensions of palaeohydrological change. In global Continental Changes: the Context of Palaeohydrology, ed. , , and . Geological Society Special Publication 115 London: Geological Society, pp. 57–72.Google Scholar
Brown, A. G. (1998). Fluvial evidence of the medieval warm period and the late medieval climatic deterioration in Europe. In Palaeohydrology and Environmental Change, ed. , , and . Chichester: Wiley, pp. 43–52.Google Scholar
and (1979). Landscape sensitivity and change. Institute of British Geographers, Transactions, 4, 463–484.CrossRefGoogle Scholar
and (1999). The evolution and significance of soil–vegetation patterns following land abandonment and fire in Spain. Catena, 37, 107–127.CrossRefGoogle Scholar
(2002). Sea level changes forced ice breakouts in the last glacial cycle: new results from coral terraces. Quaternary Science Reviews, 21, 1229–1240.CrossRefGoogle Scholar
and (1972). Paraglacial sedimentation: a consideration of fluvial processes conditioned by glaciation. Geological Society of America Bulletin, 83, 3059–3071.CrossRefGoogle Scholar
and (1989). Disequilibrium of Holocene sediment yield in glaciated British Columbia. Nature, 337, 452–454.CrossRefGoogle Scholar
(1997). Catastrophic landscape evolution in a humid region (SE Brazil): inheritances from tectonic, climatic and land use induced changes. Geografia Física e Dinâmica Quaternária, Suppl. III, 21–48.Google Scholar
, , , et al. (1993). Evidence for general instability of climate from a 250 kyr ice-core record. Nature, 364, 218–220.CrossRefGoogle Scholar
and (2001). Lake sediments, erosion and landscape change during the Holocene in Britain and Ireland. Catena, 42, 143–173.CrossRefGoogle Scholar
(1955). Biostasie et rhexistasie: esquise d'une théorie sur le rôle de la pédogenèse en tant que phénomène géologique. Comptes Rendues Academie des Sciences Française, 241, 1218–1220.Google Scholar
and (2001). Rapid changes of glacial climate simulated in a coupled climate model. Nature, 409, 153–158.CrossRefGoogle Scholar
, , and (1996). Late Quaternary climate changes and mass movement frequency and magnitude in the Cantabrian region, Spain. Geomorphology, 15, 291–309.CrossRefGoogle Scholar
(2001). Coupling between hillslopes and channels in upland fluvial systems: implications for landscape sensitivity, illustrated from the Howgill Fells, northwest England. Catena, 42, 225–250.CrossRefGoogle Scholar
(2002). Effective timescales of coupling within fluvial systems. Geomorphology, 44, 175–201.CrossRefGoogle Scholar
(1988). Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130 000 years. Quaternary Research, 29, 142–152.CrossRefGoogle Scholar
, and (2002). Interhemispheric space-time attributes of the Dansgaard–Oeschger oscillations between 100 and 0 ka. Quaternary Science Reviews, 21, 1213–1228.CrossRefGoogle Scholar
(1973). Landslides of Rio de Janeiro and the Serra das Araras Escarpment, Brazil. US Geological Survey Professional Paper, 697.Google Scholar
Kadomura, H. (1995). Palaeoecological and palaeohydrological changes in the humid tropics during the last 20 000 years, with reference to equatorial Africa. In Global Continental Palaeohydrology, ed. , , and . Chichester: Wiley, pp. 177–202.Google Scholar
Kershaw, A. P. (1992). The development of rainforest–savanna boundaries in tropical Australia. In Nature and Dynamics of Forest–Savanna Boundaries, ed. , , and . London: Chapman and Hall, pp. 55–271.Google Scholar
(1972). Valley alluviation in southwestern Wisconsin. Annals of the Association of American Geographers, 62, 401–410.CrossRefGoogle Scholar
(1993). Large increases in flood magnitude in response to modest changes in climate. Nature, 361, 430–432.CrossRefGoogle Scholar
Knox, J. C. (1995). Fluvial systems since 20 000 years BP. In Global Continental Palaeohydrology, ed. , , and . Chichester: Wiley, pp. 7–108.Google Scholar
and (1993). A rainfall intensity–duration threshold for landslides in a humid tropical environment, Puerto Rico. Geografiska Annaler, 75A, 13–23.CrossRefGoogle Scholar
, and (2001). The fluvial system response to abrupt climate change during the last cold stage: the Upper Pleistocene River Thames fluvial succession at Ashton Keynes, UK. Global and Planetary Change, 28, 341–359.CrossRefGoogle Scholar
(1975). Slope failures in Hong Kong. Quarterly Journal of Engineering Geology, 8, 31–65.CrossRefGoogle Scholar
and (1993). Holocene river alluviation in Britain. Zeitschrift für Geomorphologie, 88, 109–122.Google Scholar
Maley, J. (1992). The African rainforest vegetation and palaeoenvironments during the Quaternary. In Tropical Forests and Climate, ed. . Dordrecht: Kluwer.CrossRefGoogle Scholar
and (2000). The last glacial cycle from the humid tropics of northeastern Australia: comparison of a terrestrial and a marine record. Palaeogeography, Palaeoclimatology and Palaeoecology, 155, 155–176.CrossRefGoogle Scholar
, and (2001). Alluvial fans, landslides and Late Quaternary climatic change in the wet tropics of northeast Queensland. Australian Journal of Earth Sciences, 48, 875–882.CrossRefGoogle Scholar
(2003). Sources of non-linearity and complexity in geomorphic systems. Progress in Physical Geography, 27, 1–23.CrossRefGoogle Scholar
Ruxton, B. P. (1968). Order and disorder in landform. In Land Evaluation, ed. . Melbourne: Macmillan, pp. 29–39.Google Scholar
, , , and (2000). European climatic response to millennia-scale changes in the atmosphere–ocean system during the last glacial period. Quaternary Research, 54, 394–403.CrossRefGoogle Scholar
, , , et al. (2002). Synchronicity between marine and terrestrial responses to millennial-scale climatic variability during the last glacial period in the Mediterranean region. Climate Dynamics, 19, 95–105.Google Scholar
(1979). Geomorphic thresholds: the concept and its applications. Institute of British Geographers, Transactions, 4, 485–515.CrossRefGoogle Scholar
and (1965). Time, space and causality in geomorphology. American Journal of Science, 263, 110–119.CrossRefGoogle Scholar
and (1973). Implications of complex response of drainage systems for Quaternary alluvial stratigraphy. Nature, 243, 99–100.Google Scholar
, , and (2004). Landslides and climate change in the Italian Dolomites since the late glacial. Catena, 55, 141–161.CrossRefGoogle Scholar
Starkel, L. (1995). Palaeohydrology of the temperate zone. In Global Continental Palaeohydrology, ed. , , and . Chichester: Wiley, pp. 23–257.Google Scholar
Stocking, M. A. (1984). Rates of erosion and sediment yield in the African environment. In Challenges in African Hydrology and Water Resources (Proceedings of the Harare Symposium, 1984). IASH Publication 144, pp. 85–293.
, , and (1995). The GISP2 δ18 climate record of the past 16 500 years and the role of the sun, ocean and volcanoes. Quaternary Research, 44, 341–354.CrossRefGoogle Scholar
, and (1999). Landscape openness and pollen records: a simulation approach. The Holocene, 9, 409– 421.CrossRefGoogle Scholar
(2001). Landscape sensitivity in time and space: an introduction. Catena, 42, 83–98.CrossRefGoogle Scholar
(2004). Landscape sensitivity to rapid environmental change: a Quaternary perspective with examples from tropical areas. Catena, 55: 107–124.CrossRefGoogle Scholar
and (2001). Landscape sensitivity: principles and applications in cool temperate environments. Catena, 42, 81–386.CrossRefGoogle Scholar
and (1980). Some aspects of the geomorphological interpretation of Quaternary alluvial sediments in Sierra Leone. Zeitschrift für Geomorphologie, N.F., Supplementband, 36, 140–161.Google Scholar
and (1995). Geomorphic response to rapid climatic and hydrologic change during the Late Pleistocene and Early Holocene in the humid and sub-humid tropics. Quaternary Science Reviews, 14, 193–207.CrossRefGoogle Scholar
Thomas, M. F. and Thorp, M. B. (2003). Paleohydrological reconstructions for tropical Africa since the Last Glacial Maximum: evidence and problems. In Paleohydrology: Understanding Global Change, ed. and . Chichester: Wiley, pp. 67–192.Google Scholar
, , and (2001). Late Quaternary stream sedimentation in the humid tropics: a review with new data from NE Queensland, Australia. Geomorphology, 39, 53–68.CrossRefGoogle Scholar
and (1992). The timing of alluvial sedimentation and floodplain formation in the lowland humid tropics of Ghana, Sierra Leone, and western Kalimantan (Indonesian Borneo). Geomorphology, 4, 409–422.CrossRefGoogle Scholar
, , , et al. (2001). Redating the onset of burning of Lynch's Crater (North Queensland): implications for human settlement in Australia. Journal of Quaternary Science, 16, 767–771.CrossRefGoogle Scholar
and (2001). Editorial: the response of rivers to climate change. Quaternary International, 79, 1–3.CrossRefGoogle Scholar
and (2001). Registration of abrupt climatic changes within fluvial systems: insights from numerical modelling experiments. Global and Planetary Change, 28, 129–144.CrossRefGoogle Scholar
and (2001). The sensitivity of Scottish rivers and upland valley floors to recent environmental change. Catena, 42, 251–273.CrossRefGoogle Scholar
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