Guillaume Soulet
Biographic Data
| ID | 2789506 |
|---|---|
| NAME | Guillaume Soulet |
| GIVEN NAMES | Guillaume |
| FAMILY NAME | Soulet |
| SIGNATURE | SOULET G |
| ORCID | 0000-0003-2941-6440 |
| VERIFIED | Yes |
| TOTAL WORKS | 6 |
| TOTAL CITATIONS | 17 |
| AUTHOR COUNT | 6 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2013 |
| LATEST PUBLICATION YEAR | 2021 |
| H-INDEX | 2 |
Local Marine Reservoir Age (Δr) Reconstructed Based on the Tsunami Deposit From Pangani Bay (Tanzania)
Quantifying the local marine reservoir age (ΔR) and its change over time is critical for precise radiocarbon calibration of marine samples and for the study of the ocean carbon cycle. ΔR values are scarce for the African coast facing the Indian Ocean, and the few values available were obtained from pre-bomb shells collected during the 19th century. Here, the ΔR value for calibrated year 1110 ± 25 (1σ) CE was reconstructed from radiocarbon dating …
Using Stable Carbon Isotopes to Quantify Radiocarbon Reservoir Age Offsets in the Coastal Black Sea
Constraining radiocarbon ( 14 C) reservoir age offsets is critical to deriving accurate calendar-age chronologies from 14 C dating of materials which did not draw carbon directly from the atmosphere. The application of 14 C dating to such materials is severely limited in hydrologically sensitive environments like the Black Sea because of the difficulty to quantify reservoir age offsets, which can vary quickly and significantly through time, due t…
Assessing the Blank Carbon Contribution, Isotope Mass Balance, and Kinetic Isotope Fractionation of the Ramped Pyrolysis/Oxidation Instrument at Nosams
We estimate the blank carbon mass over the course of a typical Ramped PyrOx (RPO) analysis (150–1000°C; 5°C×min –1 ) to be (3.7±0.6) μg C with an Fm value of 0.555±0.042 and a δ 13 C value of (–29.0±0.1) ‰ VPDB. Additionally, we provide equations for RPO Fm and δ 13 C blank corrections, including associated error propagation. By comparing RPO mass-weighted mean and independently measured bulk δ 13 C values for a compilation of environmental sampl…
A Note on Reporting of Reservoir 14 C Disequilibria and Age Offsets
Reservoir age offsets are widely used to correct marine and speleothem radiocarbon age measurements for various calibration purposes. They also serve as a powerful tracer for carbon cycle dynamics. However, a clear terminology regarding reservoir age offsets is lacking, sometimes leading to miscalculations. This note seeks to provide consistent conventions for reporting reservoir 14 C disequilibria useful to a broad range of environmental science…
Les sédiments de la mer Noire
Il y a environ 21 000 ans, la géographie de l’Europe était bien différente de celle d’aujourd’hui. Une véritable montagne de glace, la calotte fennoscandienne, recouvrait toute l’Europe du Nord depuis les îles britanniques jusqu’à la Sibérie. Le niveau des océans était alors plus bas de 120 mètres. Un fleuve géant, le fleuve Manche, coulait sur une plaine entre la France et l’Angleterre. En Europe centrale, la mer Noire n’était pas connectée à la…
Les sédiments de la mer Noire
Il y a environ 21 000 ans, la géographie de l’Europe était bien différente de celle d’aujourd’hui. Une véritable montagne de glace, la calotte fennoscandienne, recouvrait toute l’Europe du Nord depuis les îles britanniques jusqu’à la Sibérie. Le niveau des océans était alors plus bas de 120 mètres. Un fleuve géant, le fleuve Manche, coulait sur une plaine entre la France et l’Angleterre. En Europe centrale, la mer Noire n’était pas connectée à la…
Assessing the Blank Carbon Contribution, Isotope Mass Balance, and Kinetic Isotope Fractionation of the Ramped Pyrolysis/Oxidation Instrument at Nosams
We estimate the blank carbon mass over the course of a typical Ramped PyrOx (RPO) analysis (150–1000°C; 5°C×min –1 ) to be (3.7±0.6) μg C with an Fm value of 0.555±0.042 and a δ 13 C value of (–29.0±0.1) ‰ VPDB. Additionally, we provide equations for RPO Fm and δ 13 C blank corrections, including associated error propagation. By comparing RPO mass-weighted mean and independently measured bulk δ 13 C values for a compilation of environmental sampl…
A Note on Reporting of Reservoir 14 C Disequilibria and Age Offsets
Reservoir age offsets are widely used to correct marine and speleothem radiocarbon age measurements for various calibration purposes. They also serve as a powerful tracer for carbon cycle dynamics. However, a clear terminology regarding reservoir age offsets is lacking, sometimes leading to miscalculations. This note seeks to provide consistent conventions for reporting reservoir 14 C disequilibria useful to a broad range of environmental science…
Using Stable Carbon Isotopes to Quantify Radiocarbon Reservoir Age Offsets in the Coastal Black Sea
Constraining radiocarbon ( 14 C) reservoir age offsets is critical to deriving accurate calendar-age chronologies from 14 C dating of materials which did not draw carbon directly from the atmosphere. The application of 14 C dating to such materials is severely limited in hydrologically sensitive environments like the Black Sea because of the difficulty to quantify reservoir age offsets, which can vary quickly and significantly through time, due t…
Les sédiments de la mer Noire
Il y a environ 21 000 ans, la géographie de l’Europe était bien différente de celle d’aujourd’hui. Une véritable montagne de glace, la calotte fennoscandienne, recouvrait toute l’Europe du Nord depuis les îles britanniques jusqu’à la Sibérie. Le niveau des océans était alors plus bas de 120 mètres. Un fleuve géant, le fleuve Manche, coulait sur une plaine entre la France et l’Angleterre. En Europe centrale, la mer Noire n’était pas connectée à la…
Les sédiments de la mer Noire
Il y a environ 21 000 ans, la géographie de l’Europe était bien différente de celle d’aujourd’hui. Une véritable montagne de glace, la calotte fennoscandienne, recouvrait toute l’Europe du Nord depuis les îles britanniques jusqu’à la Sibérie. Le niveau des océans était alors plus bas de 120 mètres. Un fleuve géant, le fleuve Manche, coulait sur une plaine entre la France et l’Angleterre. En Europe centrale, la mer Noire n’était pas connectée à la…
A Note on Reporting of Reservoir 14 C Disequilibria and Age Offsets
Reservoir age offsets are widely used to correct marine and speleothem radiocarbon age measurements for various calibration purposes. They also serve as a powerful tracer for carbon cycle dynamics. However, a clear terminology regarding reservoir age offsets is lacking, sometimes leading to miscalculations. This note seeks to provide consistent conventions for reporting reservoir 14 C disequilibria useful to a broad range of environmental science…
Assessing the Blank Carbon Contribution, Isotope Mass Balance, and Kinetic Isotope Fractionation of the Ramped Pyrolysis/Oxidation Instrument at Nosams
We estimate the blank carbon mass over the course of a typical Ramped PyrOx (RPO) analysis (150–1000°C; 5°C×min –1 ) to be (3.7±0.6) μg C with an Fm value of 0.555±0.042 and a δ 13 C value of (–29.0±0.1) ‰ VPDB. Additionally, we provide equations for RPO Fm and δ 13 C blank corrections, including associated error propagation. By comparing RPO mass-weighted mean and independently measured bulk δ 13 C values for a compilation of environmental sampl…
Using Stable Carbon Isotopes to Quantify Radiocarbon Reservoir Age Offsets in the Coastal Black Sea
Constraining radiocarbon ( 14 C) reservoir age offsets is critical to deriving accurate calendar-age chronologies from 14 C dating of materials which did not draw carbon directly from the atmosphere. The application of 14 C dating to such materials is severely limited in hydrologically sensitive environments like the Black Sea because of the difficulty to quantify reservoir age offsets, which can vary quickly and significantly through time, due t…
Local Marine Reservoir Age (Δr) Reconstructed Based on the Tsunami Deposit From Pangani Bay (Tanzania)
Quantifying the local marine reservoir age (ΔR) and its change over time is critical for precise radiocarbon calibration of marine samples and for the study of the ocean carbon cycle. ΔR values are scarce for the African coast facing the Indian Ocean, and the few values available were obtained from pre-bomb shells collected during the 19th century. Here, the ΔR value for calibrated year 1110 ± 25 (1σ) CE was reconstructed from radiocarbon dating …
Geography (4 works) · Geology (4 works) · Chemistry (3 works) · Geology and Paleoclimatology Research (3 works) · Marine and environmental studies (3 works) · Paleontology (3 works) · Radiocarbon dating (3 works) · Archaeology and ancient environmental studies (2 works) · Art (2 works) · Isotope Analysis in Ecology (2 works)