FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1969082885> ?p ?o ?g. }

• W1969082885 endingPage "120" @default.
• W1969082885 startingPage "77" @default.
• W1969082885 abstract "Lake sediments are natural archives that record the response of a lake to both in-lake processes and catchment disturbance (over a range of timescales). The response (or lack of) of a lake to external forcing is a function of the severity of the disturbance (and its areal extent) but is also strongly mediated by catchment characteristics, such as slope and hydrological connectivity. Many studies of recent lake disturbance have focussed on anthropogenic disruption of geochemical cycles, e.g. acidification and eutrophication, which because of their “ecological” power appear to over-ride catchment filters. Lake sediments also record the variability of natural disturbance regimes themselves (fire, volcanic ash falls, species invasions, and climate) and the consequent lake response but this aspect has received much less attention. The possibility of using lake sediments to address long-term (102 – 103 yr) interactions between e.g., climate, catchment ontogeny and disturbance events (and their synergies) has not been fully explored, largely because of an over-riding emphasis on climate as a direct driver of ecological change.Traditionally, limnology has also focussed on a few key sites (sentinels) but in response to the development of landscape ecology has progressively embraced a regional approach to understanding how lakes respond to external forcing (climate) and disturbance (“lakes in the landscape”). Although the interaction of a lake with its catchment is implicit, i.e. via hydrological and nutrient loading, palaeolimnologists rarely take an explicitly spatial view of this interaction nor have they considered spatial location (i.e. response of a number of lakes within a lake district). Arguably, the inherent spatial variability of terrestrial disturbance has been ignored by palaeolimnologists, largely as a result of focussing on one core from a single lake.This paper reviews the impact of terrestrial disturbance on lakes but also argues for explicit consideration of space and location in determining the resultant temporal variability of the ecological response. The importance of within-lake spatial heterogeneity is also high-lighted (i.e. the major contribution of the littoral zone to both diversity and production). However, any attempt to determine spatially replicated (i.e. at a regional scale), holistic (i.e. whole lake) responses to disturbance will encounter considerable problems associated with dating, loss of temporal resolution and among site comparison. Despite this, it is clear that recent methodological developments in the area of biomarkers, compound specific stable isotopes coupled with progress in dating (age-models), ecological modelling and statistical analysis offer the possibility of undertaking regionally-replicated studies of lake response to natural disturbance, thereby contributing and expanding our understanding of ecosystem dynamics at a range of spatial and temporal scales." @default.
• W1969082885 created "2016-06-24" @default.
• W1969082885 creator A5091255988 @default.
• W1969082885 date "2014-12-01" @default.
• W1969082885 modified "2023-10-10" @default.
• W1969082885 title "Landscape Disturbance and Lake Response: Temporal and Spatial Perspectives" @default.
• W1969082885 cites W1503925742 @default.
• W1969082885 cites W1516608626 @default.
• W1969082885 cites W152123986 @default.
• W1969082885 cites W1542247698 @default.
• W1969082885 cites W1546536320 @default.
• W1969082885 cites W1551747230 @default.
• W1969082885 cites W1578339091 @default.
• W1969082885 cites W1581734714 @default.
• W1969082885 cites W1604853763 @default.
• W1969082885 cites W1789618979 @default.
• W1969082885 cites W1888584566 @default.
• W1969082885 cites W1964804446 @default.
• W1969082885 cites W1965249936 @default.
• W1969082885 cites W1967444696 @default.
• W1969082885 cites W1967938832 @default.
• W1969082885 cites W1968219229 @default.
• W1969082885 cites W1970621702 @default.
• W1969082885 cites W1971261222 @default.
• W1969082885 cites W1972089375 @default.
• W1969082885 cites W1972406678 @default.
• W1969082885 cites W1972876602 @default.
• W1969082885 cites W1973178593 @default.
• W1969082885 cites W1973314888 @default.
• W1969082885 cites W1973760744 @default.
• W1969082885 cites W1973984637 @default.
• W1969082885 cites W1974408340 @default.
• W1969082885 cites W1975715178 @default.
• W1969082885 cites W1975816373 @default.
• W1969082885 cites W1977213583 @default.
• W1969082885 cites W1979635093 @default.
• W1969082885 cites W1981401208 @default.
• W1969082885 cites W1984118990 @default.
• W1969082885 cites W1984881185 @default.
• W1969082885 cites W1986479879 @default.
• W1969082885 cites W1987915061 @default.
• W1969082885 cites W1989777241 @default.
• W1969082885 cites W1989974602 @default.
• W1969082885 cites W1990021520 @default.
• W1969082885 cites W1990161466 @default.
• W1969082885 cites W1992734100 @default.
• W1969082885 cites W1993297108 @default.
• W1969082885 cites W1993880887 @default.
• W1969082885 cites W1996719737 @default.
• W1969082885 cites W1999239456 @default.
• W1969082885 cites W1999687518 @default.
• W1969082885 cites W2000502499 @default.
• W1969082885 cites W2004817877 @default.
• W1969082885 cites W2005930000 @default.
• W1969082885 cites W2007021204 @default.
• W1969082885 cites W2007248874 @default.
• W1969082885 cites W2010436562 @default.
• W1969082885 cites W2011219550 @default.
• W1969082885 cites W2011603555 @default.
• W1969082885 cites W2012520581 @default.
• W1969082885 cites W2012540741 @default.
• W1969082885 cites W2012752863 @default.
• W1969082885 cites W2013090987 @default.
• W1969082885 cites W2014214538 @default.
• W1969082885 cites W2014277592 @default.
• W1969082885 cites W2014419923 @default.
• W1969082885 cites W2014895126 @default.
• W1969082885 cites W2015032635 @default.
• W1969082885 cites W2016839065 @default.
• W1969082885 cites W2017812354 @default.
• W1969082885 cites W2018629693 @default.
• W1969082885 cites W2019051572 @default.
• W1969082885 cites W2019105686 @default.
• W1969082885 cites W2020378270 @default.
• W1969082885 cites W2022464637 @default.
• W1969082885 cites W2024790346 @default.
• W1969082885 cites W2025605550 @default.
• W1969082885 cites W2026197424 @default.
• W1969082885 cites W2027870170 @default.
• W1969082885 cites W2028057568 @default.
• W1969082885 cites W2031700190 @default.
• W1969082885 cites W2031780824 @default.
• W1969082885 cites W2031933088 @default.
• W1969082885 cites W2032084302 @default.
• W1969082885 cites W2035722734 @default.
• W1969082885 cites W2035998037 @default.
• W1969082885 cites W2036318452 @default.
• W1969082885 cites W2038229015 @default.
• W1969082885 cites W2038846312 @default.
• W1969082885 cites W2040614338 @default.
• W1969082885 cites W2040760699 @default.
• W1969082885 cites W2042124695 @default.
• W1969082885 cites W2043469173 @default.
• W1969082885 cites W2043544053 @default.
• W1969082885 cites W2045012006 @default.
• W1969082885 cites W2045287553 @default.
• W1969082885 cites W2045378379 @default.
• W1969082885 cites W2049883827 @default.

• next