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Holocene evolution of a lowland Scottish landscape

Kirkpatrick Fleming. Part III, fluvial history

Bibliographic Data

ID12266167
AuthorsRichard Tipping (0000-0002-6915-7095, Nether Kidston Cottage, Nether Kidston Farm, by Peebles EH45 8PJ, Borders Region, Scotland, UK, corresponding author)
Year1995
Volume5
Issue2
Pages184-195
Publication date1995-06-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/095968369500500206
OpenAlexW2155228571
LanguageEN
Citations received6
References cited17

Mapping and radiocarbon dating of fluvial terrace fragments along the greater length of the Kirtle Water resulted in the definition of five major terrace surfaces. Correlations with proxy records of climate change (Part I) and anthropogenic activity (Part II) are made to understand causal mechanisms in fluvial behaviour. The limitations of such correlations are emphasized. The highest terrace (Kirtle I) is thought to be of Devensian Lateglacial age. The remaining four are of Holocene age. An early Holocene gravel aggradation (Kirtle II) may have been sustained from c. 7250 14 C years BC until close to c. 455 cal. BC. The establishment of Alnus on floodplains may have led to channel stability. Incision after c. 3250 cal. BC may have been due to greater discharges at a time of deteriorating climate. Terrace Kirtle III is undated. Prior to aggradation of Terrace Kirtle IV, beginning at around cal. AD 300, a period of lowered fluvial activity and floodplain stability is recorded from c. 850 cal. BC. Anthropogenic activity is thought to be responsible for the diachronous initiation of aggradation of Terrace Kirtle IV. Terrace Kirtle V is late historic in age, but the cause cannot be readily isolated

Aggradation · Archaeology · Diachronous · Floodplain · Fluvial · Geography · Geomorphology · Holocene · Holocene climatic optimum · Physical geography · Radiocarbon dating · Structural basin · Terrace (agriculture · Geological formations and processes · Geology and Paleoclimatology Research · Hydrology and Sediment Transport Processes · Geology · Paleontology

  • The landscape context of the Antonine Wall

    Richard Tipping, Eileen Tisdall•Proceedings of the Society of…•2006

  • River sedimentation and fluvial response to Holocene environmental change in the Yorkshire Ouse Basin, northern England

    Open Access•Mark Patrick Taylor, Mark G Macklin et al.•The Holocene•2000

  • Fluvial sediments, correlations and palaeoenvironmental reconstruction

    Open Access•Andy J Howard, Benjamin Gearey et al.•Journal of Archaeological Science•2009

  • Towards an environmental history of the Bowmont Valley and the northern Cheviot Hills

    Richard Tipping•Landscape History•1998

  • Anthropogenic alluvium

    Open Access•Mark G Macklin, J Lewins et al.•Anthropocene•2014

  • A generic geomorphological approach to archaeological interpretation and prospection in British river valleys

    Open Access•Andy J Howard, Mark G Macklin•Antiquity•1999

  • Late Holocene Paleoecology and Sedimentary History of a Small Lowland Catchment in Central England

    Open Access•Antony G Brown, Antony Brown et al.•Quaternary Research•1985

  • A palaeoecological study of holocene peat bog sections in Germany and The Netherlands, based on the analysis of pollen, spores and macro- and microscopic remains of fungi, algae, cormophytes and animals

    Open Access•Bas Van Geel•Review of Palaeobotany and…•1978

  • Extreme Rainfall and Its Implications for Flood Frequency

    Lindsey Mcewen, Lindsey Jo McEwen•Transactions of the Institute of…•1989

Unique citing works6
Citations per year0,21
Citation span1998 - 2014 (17)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 5
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