FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2087224292> ?p ?o ?g. }

• W2087224292 endingPage "343" @default.
• W2087224292 startingPage "317" @default.
• W2087224292 abstract "In the Solway Firth — Morecambe Bay region of Great Britain there is evidence for heightened hillslope instability during the late Holocene (after 3000 cal. BP). Little or no hillslope geomorphic activity has been identified occurring during the early Holocene, but there is abundant evidence for late Holocene hillslope erosion (gullying) and associated alluvial fan and valley floor deposition. Interpretation of the regional radiocarbon chronology available from organic matter buried beneath alluvial fan units suggests much of this geomorphic activity can be attributed to four phases of more extensive gullying identified after 2500–2200, 1300–1000, 1000–800 and 500 cal. BP. Both climate and human impact models can be evoked to explain the crossing of geomorphic thresholds: and palaeoecological data on climatic change (bog surface wetness) and human impact (pollen), together with archaeological and documentary evidence of landscape history, provide a context for addressing the causes of late Holocene geomorphic instability. High magnitude storm events are the primary agent responsible for gully incision, but neither such events nor cooler/wetter climatic episodes appear to have produced gully systems in the region before 3000 cal. BP. Increased gullying after 2500–2200 cal. BP coincides with population expansion during Iron Age and Romano-British times. The widespread and extensive gullying after 1300–1000 cal. BP and after 1000–800 cal. BP coincides with periods of population expansion and a growing rural economy identified during Norse times, 9–10th centuries AD, and during the Medieval Period, 12–13th centuries AD. These periods were separated by a downturn associated with the ‘harrying of the north’ AD 1069 to 1070. The gullying episode after 500 cal. BP also coincides with increased anthropogenic pressure on the uplands, with population growth and agricultural expansion after AD 1500 following 150 years of malaise caused by livestock and human (the Black Death) plagues, poor harvests and conflicts on the Scottish/English border. The increased susceptibility to erosion of gullies is a response to increased anthropogenic pressure on upland hillslopes during the late Holocene, and the role of this pressure appears crucial in priming hillslopes before subsequent major storm events. In particular, the cycles of expansion and contraction in both population and agriculture appear to have affected the susceptibility of the upland landscape to erosion, and the hillslope gullying record in the region, therefore, contributes to understanding of the timing and spatial pattern of human exploitation of the upland landscape." @default.
• W2087224292 created "2016-06-24" @default.
• W2087224292 creator A5036918112 @default.
• W2087224292 creator A5039005417 @default.
• W2087224292 creator A5053605703 @default.
• W2087224292 date "2007-02-01" @default.
• W2087224292 modified "2023-09-25" @default.
• W2087224292 title "Hillslope gullying in the Solway Firth — Morecambe Bay region, Great Britain: Responses to human impact and/or climatic deterioration?" @default.
• W2087224292 cites W176718986 @default.
• W2087224292 cites W1967000984 @default.
• W2087224292 cites W1974709917 @default.
• W2087224292 cites W1977866788 @default.
• W2087224292 cites W1978527652 @default.
• W2087224292 cites W1981481261 @default.
• W2087224292 cites W1982166719 @default.
• W2087224292 cites W1986592825 @default.
• W2087224292 cites W1989519958 @default.
• W2087224292 cites W1993560193 @default.
• W2087224292 cites W2003690126 @default.
• W2087224292 cites W2012950352 @default.
• W2087224292 cites W2013250053 @default.
• W2087224292 cites W2030345906 @default.
• W2087224292 cites W2032744251 @default.
• W2087224292 cites W2046595013 @default.
• W2087224292 cites W2056084380 @default.
• W2087224292 cites W2059081346 @default.
• W2087224292 cites W2062736045 @default.
• W2087224292 cites W2064842054 @default.
• W2087224292 cites W2070532724 @default.
• W2087224292 cites W2073111626 @default.
• W2087224292 cites W2075633931 @default.
• W2087224292 cites W2077665638 @default.
• W2087224292 cites W2078972583 @default.
• W2087224292 cites W2082054562 @default.
• W2087224292 cites W2082368633 @default.
• W2087224292 cites W2085235266 @default.
• W2087224292 cites W2085252040 @default.
• W2087224292 cites W2087022258 @default.
• W2087224292 cites W2088794870 @default.
• W2087224292 cites W2089265791 @default.
• W2087224292 cites W2092850099 @default.
• W2087224292 cites W2093211846 @default.
• W2087224292 cites W2093737614 @default.
• W2087224292 cites W2120438128 @default.
• W2087224292 cites W2120539354 @default.
• W2087224292 cites W2124246698 @default.
• W2087224292 cites W2128596919 @default.
• W2087224292 cites W2131493982 @default.
• W2087224292 cites W2155228571 @default.
• W2087224292 cites W2155899960 @default.
• W2087224292 cites W2158338725 @default.
• W2087224292 cites W2160657028 @default.
• W2087224292 cites W2160832659 @default.
• W2087224292 cites W2167671750 @default.
• W2087224292 cites W2280624662 @default.
• W2087224292 cites W2330485362 @default.
• W2087224292 cites W2332441345 @default.
• W2087224292 cites W3171227962 @default.
• W2087224292 cites W4243293535 @default.
• W2087224292 cites W4243881205 @default.
• W2087224292 cites W4252757771 @default.
• W2087224292 cites W4252773028 @default.
• W2087224292 doi "https://doi.org/10.1016/j.geomorph.2005.12.014" @default.
• W2087224292 hasPublicationYear "2007" @default.
• W2087224292 type Work @default.
• W2087224292 sameAs 2087224292 @default.
• W2087224292 citedByCount "73" @default.
• W2087224292 countsByYear W20872242922012 @default.
• W2087224292 countsByYear W20872242922013 @default.
• W2087224292 countsByYear W20872242922014 @default.
• W2087224292 countsByYear W20872242922015 @default.
• W2087224292 countsByYear W20872242922016 @default.
• W2087224292 countsByYear W20872242922017 @default.
• W2087224292 countsByYear W20872242922018 @default.
• W2087224292 countsByYear W20872242922019 @default.
• W2087224292 countsByYear W20872242922020 @default.
• W2087224292 countsByYear W20872242922021 @default.
• W2087224292 countsByYear W20872242922022 @default.
• W2087224292 countsByYear W20872242922023 @default.
• W2087224292 crossrefType "journal-article" @default.
• W2087224292 hasAuthorship W2087224292A5036918112 @default.
• W2087224292 hasAuthorship W2087224292A5039005417 @default.
• W2087224292 hasAuthorship W2087224292A5053605703 @default.
• W2087224292 hasConcept C100134115 @default.
• W2087224292 hasConcept C100970517 @default.
• W2087224292 hasConcept C111368507 @default.
• W2087224292 hasConcept C127313418 @default.
• W2087224292 hasConcept C140345934 @default.
• W2087224292 hasConcept C144024400 @default.
• W2087224292 hasConcept C149923435 @default.
• W2087224292 hasConcept C151730666 @default.
• W2087224292 hasConcept C205649164 @default.
• W2087224292 hasConcept C2779343474 @default.
• W2087224292 hasConcept C2908647359 @default.
• W2087224292 hasConcept C69823785 @default.
• W2087224292 hasConceptScore W2087224292C100134115 @default.
• W2087224292 hasConceptScore W2087224292C100970517 @default.
• W2087224292 hasConceptScore W2087224292C111368507 @default.

• next