Luigi Vigliotti
Biographic Data
| ID | 5636781 |
|---|---|
| NAME | Luigi Vigliotti |
| GIVEN NAMES | Luigi |
| FAMILY NAME | Vigliotti |
| SIGNATURE | VIGLIOTTI L |
| AFFILIATIONS | Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche |
| ORCID | 0000-0002-4160-8958 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 37 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2003 |
| LATEST PUBLICATION YEAR | 2012 |
| H-INDEX | 2 |
A marine/terrestrial integration for mid-late Holocene vegetation history and the development of the cultural landscape in the Po valley as a result of human impact and climate change
Late-Holocene climate variability in the Adriatic Sea (Central Mediterranean)
Planktic and benthic foraminifera assemblages from a set of sediment cores, collected on the Adriatic shelf and the Southern Adriatic deep basin, provide compelling evidence of submillennial-scale environmental changes during the last 6000 years. Repeated peaks in Globigerinoides sacculifer represent warm-dry intervals, including the `Mediaeval Warm Period', the `Roman Age', the late `Bronze Age' and the `Copper Age'. The Last Occurrence (LO) of …
Palaeomagnetic and rock magnetic analysis of Holocene deposits from the Adriatic Sea
We present palaeomagnetic and rock magnetic results from five cores collected in the basin of the Adriatic Sea. Four cores (PRAD2-4; KS02-246; CSS00-23 and CSS00-07) were collected along a shore-parallel transect whereas the fifth core (AMC99-01) was retrieved in the central Adriatic in 250 m water depth, on the floor of the Meso-Adriatic Depression. After alternating field demagnetization, the natural remanent magnetization (NRM) directions show…
Etruscan archaeometallurgy record in sediments from the Northern Tyrrhenian Sea
A marine/terrestrial integration for mid-late Holocene vegetation history and the development of the cultural landscape in the Po valley as a result of human impact and climate change
Late-Holocene climate variability in the Adriatic Sea (Central Mediterranean)
Planktic and benthic foraminifera assemblages from a set of sediment cores, collected on the Adriatic shelf and the Southern Adriatic deep basin, provide compelling evidence of submillennial-scale environmental changes during the last 6000 years. Repeated peaks in Globigerinoides sacculifer represent warm-dry intervals, including the `Mediaeval Warm Period', the `Roman Age', the late `Bronze Age' and the `Copper Age'. The Last Occurrence (LO) of …
Etruscan archaeometallurgy record in sediments from the Northern Tyrrhenian Sea
Palaeomagnetic and rock magnetic analysis of Holocene deposits from the Adriatic Sea
We present palaeomagnetic and rock magnetic results from five cores collected in the basin of the Adriatic Sea. Four cores (PRAD2-4; KS02-246; CSS00-23 and CSS00-07) were collected along a shore-parallel transect whereas the fifth core (AMC99-01) was retrieved in the central Adriatic in 250 m water depth, on the floor of the Meso-Adriatic Depression. After alternating field demagnetization, the natural remanent magnetization (NRM) directions show…
Etruscan archaeometallurgy record in sediments from the Northern Tyrrhenian Sea
Late-Holocene climate variability in the Adriatic Sea (Central Mediterranean)
Planktic and benthic foraminifera assemblages from a set of sediment cores, collected on the Adriatic shelf and the Southern Adriatic deep basin, provide compelling evidence of submillennial-scale environmental changes during the last 6000 years. Repeated peaks in Globigerinoides sacculifer represent warm-dry intervals, including the `Mediaeval Warm Period', the `Roman Age', the late `Bronze Age' and the `Copper Age'. The Last Occurrence (LO) of …
Palaeomagnetic and rock magnetic analysis of Holocene deposits from the Adriatic Sea
We present palaeomagnetic and rock magnetic results from five cores collected in the basin of the Adriatic Sea. Four cores (PRAD2-4; KS02-246; CSS00-23 and CSS00-07) were collected along a shore-parallel transect whereas the fifth core (AMC99-01) was retrieved in the central Adriatic in 250 m water depth, on the floor of the Meso-Adriatic Depression. After alternating field demagnetization, the natural remanent magnetization (NRM) directions show…
A marine/terrestrial integration for mid-late Holocene vegetation history and the development of the cultural landscape in the Po valley as a result of human impact and climate change
Geology (4 works) · Maritime and Coastal Archaeology (4 works) · Archaeology (3 works) · Archaeology and ancient environmental studies (3 works) · Geography (3 works) · Geology and Paleoclimatology Research (3 works) · Holocene (3 works) · Oceanography (3 works) · Benthic zone (2 works) · Foraminifera (2 works)