Frédéric Bouchette
Biographic Data
| ID | 11136283 |
|---|---|
| NAME | Frédéric Bouchette |
| GIVEN NAMES | Frédéric |
| FAMILY NAME | Bouchette |
| SIGNATURE | BOUCHETTE F |
| AFFILIATIONS | Centre National de la Recherche Scientifique |
| ORCID | 0000-0001-9537-3624 |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2010 |
| LATEST PUBLICATION YEAR | 2012 |
| H-INDEX | 0 |
Years of paleostorm activity in the NW Mediterranean Sea in response to Holocene climate events
A high-resolution record of paleostorm events along the French Mediterranean coast over the past 7000 years was established from a lagoonal sediment core in the Gulf of Lions. Integrating grain size, faunal analysis, clay mineralogy and geochemistry data with a chronology derived from radiocarbon dating, we recorded seven periods of increased storm activity at 6300–6100, 5650–5400, 4400–4050, 3650–3200, 2800–2600, 1950–1400 and 400–50 cal yr BP (…
Hydrodynamics in Holocene Lake Mega-Chad
Holocene Lake Mega-Chad (LMC) was the largest late Quaternary water-body in Africa. The development of this giant paleo-lake is related to a northward shift of the isohyetes interpreted as evidence for an enhanced Monsoon (African Humid Period). Numerous preserved coastal features have been described all around the LMC shore. Such features reveal the main paleo-hydrodynamical tendencies. In the context of a closed water-body like LMC, hydrodynami…
No prominent works on this page.
Hydrodynamics in Holocene Lake Mega-Chad
Holocene Lake Mega-Chad (LMC) was the largest late Quaternary water-body in Africa. The development of this giant paleo-lake is related to a northward shift of the isohyetes interpreted as evidence for an enhanced Monsoon (African Humid Period). Numerous preserved coastal features have been described all around the LMC shore. Such features reveal the main paleo-hydrodynamical tendencies. In the context of a closed water-body like LMC, hydrodynami…
Years of paleostorm activity in the NW Mediterranean Sea in response to Holocene climate events
A high-resolution record of paleostorm events along the French Mediterranean coast over the past 7000 years was established from a lagoonal sediment core in the Gulf of Lions. Integrating grain size, faunal analysis, clay mineralogy and geochemistry data with a chronology derived from radiocarbon dating, we recorded seven periods of increased storm activity at 6300–6100, 5650–5400, 4400–4050, 3650–3200, 2800–2600, 1950–1400 and 400–50 cal yr BP (…
Climatology (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Holocene (2 works) · Oceanography (2 works) · Aeolian processes and effects (1 work) · Archaeology (1 work) · Coastal and Marine Dynamics (1 work) · Context (archaeology) (1 work) · Geography (1 work)