C J Caseldine
Biographic Data
| ID | 2775462 |
|---|---|
| NAME | C J Caseldine |
| GIVEN NAMES | C J |
| FAMILY NAME | Caseldine |
| SIGNATURE | CASELDINE C J |
| AFFILIATIONS | University of Exeter |
| VERIFIED | No |
| TOTAL WORKS | 6 |
| TOTAL CITATIONS | 20 |
| WORKS AS AUTHOR | 6 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1978 |
| LATEST PUBLICATION YEAR | 2012 |
| H-INDEX | 2 |
Regional climate change from peat stratigraphy for the mid- to late Holocene in central Ireland
A chironomid-based reconstruction of summer temperatures in NW Iceland since AD 1650
Few studies currently exist that aim to validate a proxy chironomid-temperature reconstruction with instrumental temperature measurements. We used a reconstruction from a chironomid percentage abundance data set to produce quantitative summer temperature estimates since AD 1650 for NW Iceland through a transfer function approach, and validated the record against instrumental temperature measurements from Stykkishólmur in western Iceland. The core…
Lacustrine evidence of early-Holocene environmental change in northern Iceland
Early-Holocene warming in Iceland caused rapid glacial ice melt which led to exposed landscapes on which soils developed and floras quickly established. Our chironomid-based records from northern Iceland suggest temperatures were up to 2—2.5°C warmer than present throughout the first two millennia post deglaciation (~10 500 to 8500 cal. BP) while sedimentary and isotopic data indicate the development of soils within the local environment througho…
The Extent of Some Glaciers in Northern Iceland during the Little Ice Age and the Nature of Recent Deglaciation
Lichenometric studies from four glaciers in Northern Iceland are used to determine the dates of their Little Ice Age maxima. In all cases these date to the last half of the nineteenth century and probably marked the maximum Neoglacial extent of the glaciers. Comparison of the pattern of subsequent deglaciation and meteorological records from the area indicates a likely relationship between changes in the mass balance of glaciers in Northern Icela…
Resurvey of the margins of Gljúfurárjökull and the chronology of recent deglaciation (Endurmæling á jaðri Gljúfurárjökuls)
The Stones of Stenness, Orkney
HY 307125. Report of excavations on the Class I henge together with discussion (by E W Marwick) of the folklore surrounding an outlying standing stone, the Stone of Odin, and a catalogue of important 18th and 19th century illustrations of both sites. Excavation of the henge revealed that a ring of twelve stones was originally planned and that a complex stone and timber setting occupied the centre, grooved ware was found in both the central featur…
The Stones of Stenness, Orkney
HY 307125. Report of excavations on the Class I henge together with discussion (by E W Marwick) of the folklore surrounding an outlying standing stone, the Stone of Odin, and a catalogue of important 18th and 19th century illustrations of both sites. Excavation of the henge revealed that a ring of twelve stones was originally planned and that a complex stone and timber setting occupied the centre, grooved ware was found in both the central featur…
The Extent of Some Glaciers in Northern Iceland during the Little Ice Age and the Nature of Recent Deglaciation
Lichenometric studies from four glaciers in Northern Iceland are used to determine the dates of their Little Ice Age maxima. In all cases these date to the last half of the nineteenth century and probably marked the maximum Neoglacial extent of the glaciers. Comparison of the pattern of subsequent deglaciation and meteorological records from the area indicates a likely relationship between changes in the mass balance of glaciers in Northern Icela…
Lacustrine evidence of early-Holocene environmental change in northern Iceland
Early-Holocene warming in Iceland caused rapid glacial ice melt which led to exposed landscapes on which soils developed and floras quickly established. Our chironomid-based records from northern Iceland suggest temperatures were up to 2—2.5°C warmer than present throughout the first two millennia post deglaciation (~10 500 to 8500 cal. BP) while sedimentary and isotopic data indicate the development of soils within the local environment througho…
The Stones of Stenness, Orkney
HY 307125. Report of excavations on the Class I henge together with discussion (by E W Marwick) of the folklore surrounding an outlying standing stone, the Stone of Odin, and a catalogue of important 18th and 19th century illustrations of both sites. Excavation of the henge revealed that a ring of twelve stones was originally planned and that a complex stone and timber setting occupied the centre, grooved ware was found in both the central featur…
Resurvey of the margins of Gljúfurárjökull and the chronology of recent deglaciation (Endurmæling á jaðri Gljúfurárjökuls)
The Extent of Some Glaciers in Northern Iceland during the Little Ice Age and the Nature of Recent Deglaciation
Lichenometric studies from four glaciers in Northern Iceland are used to determine the dates of their Little Ice Age maxima. In all cases these date to the last half of the nineteenth century and probably marked the maximum Neoglacial extent of the glaciers. Comparison of the pattern of subsequent deglaciation and meteorological records from the area indicates a likely relationship between changes in the mass balance of glaciers in Northern Icela…
Lacustrine evidence of early-Holocene environmental change in northern Iceland
Early-Holocene warming in Iceland caused rapid glacial ice melt which led to exposed landscapes on which soils developed and floras quickly established. Our chironomid-based records from northern Iceland suggest temperatures were up to 2—2.5°C warmer than present throughout the first two millennia post deglaciation (~10 500 to 8500 cal. BP) while sedimentary and isotopic data indicate the development of soils within the local environment througho…
A chironomid-based reconstruction of summer temperatures in NW Iceland since AD 1650
Few studies currently exist that aim to validate a proxy chironomid-temperature reconstruction with instrumental temperature measurements. We used a reconstruction from a chironomid percentage abundance data set to produce quantitative summer temperature estimates since AD 1650 for NW Iceland through a transfer function approach, and validated the record against instrumental temperature measurements from Stykkishólmur in western Iceland. The core…
Regional climate change from peat stratigraphy for the mid- to late Holocene in central Ireland
Geology and Paleoclimatology Research (5 works) · Geography (4 works) · Geology (4 works) · Geology (4 works) · Holocene (4 works) · Physical geography (4 works) · Deglaciation (3 works) · Geomorphology (3 works) · Oceanography (3 works) · Archaeology (2 works)