Richard T Jones
Biographic Data
| ID | 3599987 |
|---|---|
| NAME | Richard T Jones |
| GIVEN NAMES | Richard T |
| FAMILY NAME | Jones |
| SIGNATURE | JONES R T |
| AFFILIATIONS | University of Exeter |
| ORCID | 0000-0002-3137-4051 |
| VERIFIED | Yes |
| TOTAL WORKS | 17 |
| TOTAL CITATIONS | 31 |
| WORKS AS AUTHOR | 17 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2002 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 3 |
Rapid laminated clastic alluviation associated with increased Little Ice Age flooding co-driven by climate variability and historic land-use in the middle Severn catchment, UK
The analysis of exceptionally well-preserved visible clastic laminations in deep alluvial sediments at Kempsey, Worcestershire (UK), allows a new high-resolution analysis of late-Holocene flood-history in the largest UK catchment, as well as local human response. At the sample site over 4.5 m of sandy-silt overbank-alluvium accumulated on the floodplain and optically stimulated luminescence (OSL) dating of the upper 2.25 m demonstrates accretion …
Traditional Design Principles of a Groundwater Irrigation System in the Foothills of the Western Ghats of Southwest India
This paper presents the traditional design principles of the suranga water-harvesting system found in an area of semicritical groundwater scarcity in the Dakshin Kannada district of Karnataka and Kasaragod district in the state of Kerala, India. This region is situated in the foothills of the Western Ghats of southern India. Data were derived from a mixed-methods approach that analyzed the structure, technology, governance, organization, and hydr…
Anomalous mid-twentieth century atmospheric circulation change over the South Atlantic compared to the last 6000 years
Determining the timing and impact of anthropogenic climate change in data-sparse regions is a considerable challenge. Arguably, nowhere is this more difficult than the Antarctic Peninsula and the subantarctic South Atlantic where observational records are relatively short but where high rates of warming have been experienced since records began. Here we interrogate recently developed monthly-resolved observational datasets from the Falkland Islan…
Extreme wet conditions coincident with Bronze Age abandonment of upland areas in Britain
An investigation into the age and origin of Suranga in the foothills of the Western Ghats of India
Investigating the maximum resolution of μXRF core scanners
Micro x-ray fluorescence (μXRF) core scanning is capable of measuring the elemental composition of lake sediment at sub-millimetre resolution, but bioturbation and physical mixing may degrade environmental signals at such fine scales. The aim of this research is to determine the maximum possible resolution at which meaningful environmental signals may be reconstructed from lake sediments using this method. Sediment from a coastal lake in the Oute…
Climate and tectonic effects on Holocene development of an alpine lake (Muge Co, SE margin of Tibet)
South-west China is an important area for determining variability of the SW Asian Monsoon; it is, however, also tectonically very active. Palaeolimnological studies in this region generally focus on climate as a direct driver of ecological change, rarely considering the effects of tectonic activity and catchment ontogeny. We present diatom and organic matter data from a Holocene sediment record from Muge Co, an alpine lake located on an active fa…
Asian summer monsoon variability during the late glacial and Holocene inferred from the stable carbon isotope record of black carbon in the sediments of Muge Co, southeastern Tibetan Plateau, China
A sediment core from an alpine lake (Muge Co) from the southeastern margin of the Tibetan Plateau was analyzed for sediment grain size distribution and the carbon isotopic composition of black carbon in order to reconstruct Asian summer monsoon variability over the last 12 ka. Five major climatic stages were identified: (1) From 12 to 10.5 cal. ka BP, a cold and dry climate prevailed, corresponding to the Younger Dryas in the North Atlantic; (2) …
A reply to ‘A meta-database of Holocene sediment cores for England
A meta-database of Holocene sediment cores for England
Detecting climatic signals in an anthropogenically disturbed catchment
Historical and documentary records from the Petit Lac d’Annecy, indicate that human activities have been the dominant ‘geomorphic process’ shaping the catchment during the late Holocene, with deforestation, agriculture and artificial drainage profoundly affecting both the pace and spatial distribution of soil erosion. The impact of past climatic change on the evolution of the catchment is less certain because of the lack of long-term climate reco…
An inter-continental comparison between the environmental histories of two lake catchment systems in montane environments of France and South West China
Controls on lake level in the early to mid Holocene, Hawes Water, Lancashire, UK
This study presents a new interpretation of the evidence for Holocene lake-level changes from Hawes Water in NW England constrained by detailed stratigraphic data, radiocarbon chronology and palaeo-environmental evidence. Lake levels are seen to decline gradually from the start of the Holocene through to 9960 cal. yr BP, in response to lake infilling and the prevailing dry climatic conditions. Low lake levels then persist until 6000 cal. yr BP, p…
Early-Holocene temperature variability inferred from chironomid assemblages at Hawes Water, northwest England
This paper presents the first high-resolution chironomid-inferred mean July air temperature (C-IT) reconstruction for the early Holocene from England. The reconstruction is based on a core recovered from a terrestrialised carbonate bench at Hawes Water, a small hard-water lake in northwest England. The record shows that temperatures rose rapidly after the Younger Dryas with temperatures reaching 14.0°C at the beginning of the Holocene. Over mille…
The Holocene vegetation history of Lake Erhai, Yunnan province southwestern China
A pollen diagram from a 6.62 m sediment sequence in Lake Erhai in northwest Yunnan, China was obtained to examine the roles of climate change and human impact on the development of the Erhai lake-catchment system since 12950 cal. yr BP. The record extends back into the Younger Dryas, where the dominance of Betula and deciduous Quercus points to a relatively cold and wet winter climate. After 11 750 cal. yr BP, a warming climate coupled with enhan…
The late-Holocene history of Gormire Lake (NE England) and its catchment
Sedimentary evidence spanning the last 3500 years from cores taken from the centre of Gormire Lake, Cleveland, northeast England, points to two periods of deforestation and catchment erosion. The first, mainly late Iron Age/Romano-British phase, began c. 200 BC and ended c. AD 600. The second began c. AD 1200, the time of early Monastic activity, and continued into the nineteenth century. The chronology for the core rests on 137 Cs, 210 Pb and 14…
Forestry and Flooding in the Annecy Petit Lac Catchment, Haute-Savoie 1730-2000
Upland environments are particularly vulnerable to the stresses of climate change. The strength and persistence of such forces are not easy to measure and hence comparison of climate impacts with anthropogenic impacts has remained problematic. This paper attempts to demonstrate the nature of human impact on forest cover and flooding in the Annecy Petit Lac Catchment in pre-Alpine Haute Savoie, France, between 1730 and 2000. Local documentary sour…
The Holocene vegetation history of Lake Erhai, Yunnan province southwestern China
A pollen diagram from a 6.62 m sediment sequence in Lake Erhai in northwest Yunnan, China was obtained to examine the roles of climate change and human impact on the development of the Erhai lake-catchment system since 12950 cal. yr BP. The record extends back into the Younger Dryas, where the dominance of Betula and deciduous Quercus points to a relatively cold and wet winter climate. After 11 750 cal. yr BP, a warming climate coupled with enhan…
Early-Holocene temperature variability inferred from chironomid assemblages at Hawes Water, northwest England
This paper presents the first high-resolution chironomid-inferred mean July air temperature (C-IT) reconstruction for the early Holocene from England. The reconstruction is based on a core recovered from a terrestrialised carbonate bench at Hawes Water, a small hard-water lake in northwest England. The record shows that temperatures rose rapidly after the Younger Dryas with temperatures reaching 14.0°C at the beginning of the Holocene. Over mille…
The late-Holocene history of Gormire Lake (NE England) and its catchment
Sedimentary evidence spanning the last 3500 years from cores taken from the centre of Gormire Lake, Cleveland, northeast England, points to two periods of deforestation and catchment erosion. The first, mainly late Iron Age/Romano-British phase, began c. 200 BC and ended c. AD 600. The second began c. AD 1200, the time of early Monastic activity, and continued into the nineteenth century. The chronology for the core rests on 137 Cs, 210 Pb and 14…
Extreme wet conditions coincident with Bronze Age abandonment of upland areas in Britain
Forestry and Flooding in the Annecy Petit Lac Catchment, Haute-Savoie 1730-2000
Upland environments are particularly vulnerable to the stresses of climate change. The strength and persistence of such forces are not easy to measure and hence comparison of climate impacts with anthropogenic impacts has remained problematic. This paper attempts to demonstrate the nature of human impact on forest cover and flooding in the Annecy Petit Lac Catchment in pre-Alpine Haute Savoie, France, between 1730 and 2000. Local documentary sour…
Rapid laminated clastic alluviation associated with increased Little Ice Age flooding co-driven by climate variability and historic land-use in the middle Severn catchment, UK
The analysis of exceptionally well-preserved visible clastic laminations in deep alluvial sediments at Kempsey, Worcestershire (UK), allows a new high-resolution analysis of late-Holocene flood-history in the largest UK catchment, as well as local human response. At the sample site over 4.5 m of sandy-silt overbank-alluvium accumulated on the floodplain and optically stimulated luminescence (OSL) dating of the upper 2.25 m demonstrates accretion …
An investigation into the age and origin of Suranga in the foothills of the Western Ghats of India
Asian summer monsoon variability during the late glacial and Holocene inferred from the stable carbon isotope record of black carbon in the sediments of Muge Co, southeastern Tibetan Plateau, China
A sediment core from an alpine lake (Muge Co) from the southeastern margin of the Tibetan Plateau was analyzed for sediment grain size distribution and the carbon isotopic composition of black carbon in order to reconstruct Asian summer monsoon variability over the last 12 ka. Five major climatic stages were identified: (1) From 12 to 10.5 cal. ka BP, a cold and dry climate prevailed, corresponding to the Younger Dryas in the North Atlantic; (2) …
A reply to ‘A meta-database of Holocene sediment cores for England
A meta-database of Holocene sediment cores for England
Detecting climatic signals in an anthropogenically disturbed catchment
Historical and documentary records from the Petit Lac d’Annecy, indicate that human activities have been the dominant ‘geomorphic process’ shaping the catchment during the late Holocene, with deforestation, agriculture and artificial drainage profoundly affecting both the pace and spatial distribution of soil erosion. The impact of past climatic change on the evolution of the catchment is less certain because of the lack of long-term climate reco…
Forestry and Flooding in the Annecy Petit Lac Catchment, Haute-Savoie 1730-2000
Upland environments are particularly vulnerable to the stresses of climate change. The strength and persistence of such forces are not easy to measure and hence comparison of climate impacts with anthropogenic impacts has remained problematic. This paper attempts to demonstrate the nature of human impact on forest cover and flooding in the Annecy Petit Lac Catchment in pre-Alpine Haute Savoie, France, between 1730 and 2000. Local documentary sour…
The late-Holocene history of Gormire Lake (NE England) and its catchment
Sedimentary evidence spanning the last 3500 years from cores taken from the centre of Gormire Lake, Cleveland, northeast England, points to two periods of deforestation and catchment erosion. The first, mainly late Iron Age/Romano-British phase, began c. 200 BC and ended c. AD 600. The second began c. AD 1200, the time of early Monastic activity, and continued into the nineteenth century. The chronology for the core rests on 137 Cs, 210 Pb and 14…
The Holocene vegetation history of Lake Erhai, Yunnan province southwestern China
A pollen diagram from a 6.62 m sediment sequence in Lake Erhai in northwest Yunnan, China was obtained to examine the roles of climate change and human impact on the development of the Erhai lake-catchment system since 12950 cal. yr BP. The record extends back into the Younger Dryas, where the dominance of Betula and deciduous Quercus points to a relatively cold and wet winter climate. After 11 750 cal. yr BP, a warming climate coupled with enhan…
Early-Holocene temperature variability inferred from chironomid assemblages at Hawes Water, northwest England
This paper presents the first high-resolution chironomid-inferred mean July air temperature (C-IT) reconstruction for the early Holocene from England. The reconstruction is based on a core recovered from a terrestrialised carbonate bench at Hawes Water, a small hard-water lake in northwest England. The record shows that temperatures rose rapidly after the Younger Dryas with temperatures reaching 14.0°C at the beginning of the Holocene. Over mille…
An inter-continental comparison between the environmental histories of two lake catchment systems in montane environments of France and South West China
Controls on lake level in the early to mid Holocene, Hawes Water, Lancashire, UK
This study presents a new interpretation of the evidence for Holocene lake-level changes from Hawes Water in NW England constrained by detailed stratigraphic data, radiocarbon chronology and palaeo-environmental evidence. Lake levels are seen to decline gradually from the start of the Holocene through to 9960 cal. yr BP, in response to lake infilling and the prevailing dry climatic conditions. Low lake levels then persist until 6000 cal. yr BP, p…
Detecting climatic signals in an anthropogenically disturbed catchment
Historical and documentary records from the Petit Lac d’Annecy, indicate that human activities have been the dominant ‘geomorphic process’ shaping the catchment during the late Holocene, with deforestation, agriculture and artificial drainage profoundly affecting both the pace and spatial distribution of soil erosion. The impact of past climatic change on the evolution of the catchment is less certain because of the lack of long-term climate reco…
An investigation into the age and origin of Suranga in the foothills of the Western Ghats of India
Investigating the maximum resolution of μXRF core scanners
Micro x-ray fluorescence (μXRF) core scanning is capable of measuring the elemental composition of lake sediment at sub-millimetre resolution, but bioturbation and physical mixing may degrade environmental signals at such fine scales. The aim of this research is to determine the maximum possible resolution at which meaningful environmental signals may be reconstructed from lake sediments using this method. Sediment from a coastal lake in the Oute…
Climate and tectonic effects on Holocene development of an alpine lake (Muge Co, SE margin of Tibet)
South-west China is an important area for determining variability of the SW Asian Monsoon; it is, however, also tectonically very active. Palaeolimnological studies in this region generally focus on climate as a direct driver of ecological change, rarely considering the effects of tectonic activity and catchment ontogeny. We present diatom and organic matter data from a Holocene sediment record from Muge Co, an alpine lake located on an active fa…
Asian summer monsoon variability during the late glacial and Holocene inferred from the stable carbon isotope record of black carbon in the sediments of Muge Co, southeastern Tibetan Plateau, China
A sediment core from an alpine lake (Muge Co) from the southeastern margin of the Tibetan Plateau was analyzed for sediment grain size distribution and the carbon isotopic composition of black carbon in order to reconstruct Asian summer monsoon variability over the last 12 ka. Five major climatic stages were identified: (1) From 12 to 10.5 cal. ka BP, a cold and dry climate prevailed, corresponding to the Younger Dryas in the North Atlantic; (2) …
A reply to ‘A meta-database of Holocene sediment cores for England
A meta-database of Holocene sediment cores for England
Anomalous mid-twentieth century atmospheric circulation change over the South Atlantic compared to the last 6000 years
Determining the timing and impact of anthropogenic climate change in data-sparse regions is a considerable challenge. Arguably, nowhere is this more difficult than the Antarctic Peninsula and the subantarctic South Atlantic where observational records are relatively short but where high rates of warming have been experienced since records began. Here we interrogate recently developed monthly-resolved observational datasets from the Falkland Islan…
Extreme wet conditions coincident with Bronze Age abandonment of upland areas in Britain
Traditional Design Principles of a Groundwater Irrigation System in the Foothills of the Western Ghats of Southwest India
This paper presents the traditional design principles of the suranga water-harvesting system found in an area of semicritical groundwater scarcity in the Dakshin Kannada district of Karnataka and Kasaragod district in the state of Kerala, India. This region is situated in the foothills of the Western Ghats of southern India. Data were derived from a mixed-methods approach that analyzed the structure, technology, governance, organization, and hydr…
Rapid laminated clastic alluviation associated with increased Little Ice Age flooding co-driven by climate variability and historic land-use in the middle Severn catchment, UK
The analysis of exceptionally well-preserved visible clastic laminations in deep alluvial sediments at Kempsey, Worcestershire (UK), allows a new high-resolution analysis of late-Holocene flood-history in the largest UK catchment, as well as local human response. At the sample site over 4.5 m of sandy-silt overbank-alluvium accumulated on the floodplain and optically stimulated luminescence (OSL) dating of the upper 2.25 m demonstrates accretion …
Geology and Paleoclimatology Research (15 works) · Geography (14 works) · Geology (14 works) · Holocene (11 works) · Oceanography (10 works) · Physical geography (9 works) · Climate change (8 works) · Archaeology (7 works) · Paleontology (7 works) · Drainage basin (6 works)