Mabs Gilmour
Biographic Data
| ID | 5598406 |
|---|---|
| NAME | Mabs Gilmour |
| GIVEN NAMES | Mabs |
| FAMILY NAME | Gilmour |
| SIGNATURE | GILMOUR M |
| AFFILIATIONS | The Open University |
| VERIFIED | No |
| TOTAL WORKS | 6 |
| TOTAL CITATIONS | 24 |
| WORKS AS AUTHOR | 6 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1999 |
| LATEST PUBLICATION YEAR | 2007 |
| H-INDEX | 2 |
VeriWcation of the Age of the Palaeolithic Cave Art at Creswell Crags
Upon discovery of the Creswell cave art in April 2003, and a systematic survey and study of known images in June of the same year, it was believed on several grounds that the art was clearly of Pleistocene antiquity (Pettitt 2003). The reasoning was as follows: . The sharp line and bright colour of engraved graffiti dating to the 1940s stand in clear contrast to the eroded and dulled nature of the genuine art. Clearly, on the grounds of weatherin…
Verification of the age of the Palaeolithic cave art at Creswell Crags, UK
Paleoclimate reconstruction based on the timing of speleothem growth and oxygen and carbon isotope composition in a cave located in the rain shadow in Israel
High-resolution 230 Th/ 234 U ages and δ 18 O and δ 13 C compositions of speleothems in Ma’ale Efrayim Cave located to the east of the central mountain ridge of Israel enable us to examine the nature of the rain shadow aridity during glacial and interglacial intervals. Speleothem growth occurred during marine glacial isotopic periods, with no growth during the two last marine isotope interglacial intervals and during the peak of the Last Glacial …
Sea–land oxygen isotopic relationships from planktonic foraminifera and speleothems in the Eastern Mediterranean region and their implication for paleorainfall during interglacial intervals
Precise dating of Dansgaard–Oeschger climate oscillations in western Europe from stalagmite data
Calculation of Past Dead Carbon Proportion and Variability by the Comparison of AMS 14 C and Tims U/TH Ages on Two Holocene Stalagmites
Twenty-two radiocarbon activity measurements were made by accelerator mass spectrometry (AMS) on 2 Holocene stalagmites from Belgium (Han-stm1b) and from southwest France (Vil-stm1b). Sixteen thermal ionization mass spectrometric (TIMS) U/Th measurements were performed parallel to AMS analyses. The past dead carbon proportion (dcp) due to limestone dissolution and old soil organic matter (SOM) degradation is calculated with U/Th ages, measured ca…
Verification of the age of the Palaeolithic cave art at Creswell Crags, UK
Calculation of Past Dead Carbon Proportion and Variability by the Comparison of AMS 14 C and Tims U/TH Ages on Two Holocene Stalagmites
Twenty-two radiocarbon activity measurements were made by accelerator mass spectrometry (AMS) on 2 Holocene stalagmites from Belgium (Han-stm1b) and from southwest France (Vil-stm1b). Sixteen thermal ionization mass spectrometric (TIMS) U/Th measurements were performed parallel to AMS analyses. The past dead carbon proportion (dcp) due to limestone dissolution and old soil organic matter (SOM) degradation is calculated with U/Th ages, measured ca…
Calculation of Past Dead Carbon Proportion and Variability by the Comparison of AMS 14 C and Tims U/TH Ages on Two Holocene Stalagmites
Twenty-two radiocarbon activity measurements were made by accelerator mass spectrometry (AMS) on 2 Holocene stalagmites from Belgium (Han-stm1b) and from southwest France (Vil-stm1b). Sixteen thermal ionization mass spectrometric (TIMS) U/Th measurements were performed parallel to AMS analyses. The past dead carbon proportion (dcp) due to limestone dissolution and old soil organic matter (SOM) degradation is calculated with U/Th ages, measured ca…
Paleoclimate reconstruction based on the timing of speleothem growth and oxygen and carbon isotope composition in a cave located in the rain shadow in Israel
High-resolution 230 Th/ 234 U ages and δ 18 O and δ 13 C compositions of speleothems in Ma’ale Efrayim Cave located to the east of the central mountain ridge of Israel enable us to examine the nature of the rain shadow aridity during glacial and interglacial intervals. Speleothem growth occurred during marine glacial isotopic periods, with no growth during the two last marine isotope interglacial intervals and during the peak of the Last Glacial …
Sea–land oxygen isotopic relationships from planktonic foraminifera and speleothems in the Eastern Mediterranean region and their implication for paleorainfall during interglacial intervals
Precise dating of Dansgaard–Oeschger climate oscillations in western Europe from stalagmite data
Verification of the age of the Palaeolithic cave art at Creswell Crags, UK
VeriWcation of the Age of the Palaeolithic Cave Art at Creswell Crags
Upon discovery of the Creswell cave art in April 2003, and a systematic survey and study of known images in June of the same year, it was believed on several grounds that the art was clearly of Pleistocene antiquity (Pettitt 2003). The reasoning was as follows: . The sharp line and bright colour of engraved graffiti dating to the 1940s stand in clear contrast to the eroded and dulled nature of the genuine art. Clearly, on the grounds of weatherin…
Geography (6 works) · Archaeology (5 works) · Cave (5 works) · Geology (4 works) · Geology and Paleoclimatology Research (4 works) · Paleontology (4 works) · Physical geography (4 works) · Glacial period (3 works) · Holocene (3 works) · Oceanography (3 works)