S A G Leroy
Biographic Data
| ID | 7514207 |
|---|---|
| NAME | S A G Leroy |
| GIVEN NAMES | S A G |
| FAMILY NAME | Leroy |
| SIGNATURE | LEROY S A G |
| AFFILIATIONS | Brunel University, UK |
| VERIFIED | No |
| TOTAL WORKS | 9 |
| TOTAL CITATIONS | 5 |
| AUTHOR COUNT | 9 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2006 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 1 |
South Caucasus greening and Neolithisation: What happened 8200 years ago
International audience
Source of Nile sediments in the floodplain at Saqqara inferred from mineralogical, geochemical, and pollen data, and their palaeoclimatic and geoarchaeological significance
QuickLakeH: Rapidly changing large lakes and human response
Late Quaternary Caspian Sea environment: Late Khazarian and Early Khvalynian transgressions from the lower reaches of the Volga River
Dendrochronological evidence for a lower water-table on peatland around 3200-3000 BC from subfossil pine in northern Scotland
Tree-ring analysis of subfossil Pinus sylvestris L., from nine new peatland sites located beyond the species’ current northern limit in Scotland, established a regional chronology called WRATH-9. The chronology has been provisionally dated against Irish pine chronologies and provides the first annual resolution picture of Scots pine expansion from c. 3200 BC and subsequent demise from c. 3000 BC. Pine germination and growth is suggested to be ass…
Dark Nature
Impact of rapid environmental changes on humans and ecosystems
Dark Nature: Responses of humans and ecosystems to rapid environmental changes
Natural and anthropogenic rapid changes in the Kara-Bogaz Gol over the last two centuries reconstructed from palynological analyses and a comparison to instrumental records
Dendrochronological evidence for a lower water-table on peatland around 3200-3000 BC from subfossil pine in northern Scotland
Tree-ring analysis of subfossil Pinus sylvestris L., from nine new peatland sites located beyond the species’ current northern limit in Scotland, established a regional chronology called WRATH-9. The chronology has been provisionally dated against Irish pine chronologies and provides the first annual resolution picture of Scots pine expansion from c. 3200 BC and subsequent demise from c. 3000 BC. Pine germination and growth is suggested to be ass…
Impact of rapid environmental changes on humans and ecosystems
Dark Nature: Responses of humans and ecosystems to rapid environmental changes
Natural and anthropogenic rapid changes in the Kara-Bogaz Gol over the last two centuries reconstructed from palynological analyses and a comparison to instrumental records
Dark Nature
Dendrochronological evidence for a lower water-table on peatland around 3200-3000 BC from subfossil pine in northern Scotland
Tree-ring analysis of subfossil Pinus sylvestris L., from nine new peatland sites located beyond the species’ current northern limit in Scotland, established a regional chronology called WRATH-9. The chronology has been provisionally dated against Irish pine chronologies and provides the first annual resolution picture of Scots pine expansion from c. 3200 BC and subsequent demise from c. 3000 BC. Pine germination and growth is suggested to be ass…
Late Quaternary Caspian Sea environment: Late Khazarian and Early Khvalynian transgressions from the lower reaches of the Volga River
QuickLakeH: Rapidly changing large lakes and human response
Source of Nile sediments in the floodplain at Saqqara inferred from mineralogical, geochemical, and pollen data, and their palaeoclimatic and geoarchaeological significance
South Caucasus greening and Neolithisation: What happened 8200 years ago
International audience
Geology (6 works) · Marine and environmental studies (6 works) · Archaeology and ancient environmental studies (4 works) · Geography (4 works) · Geology and Paleoclimatology Research (4 works) · Paleontology (4 works) · Biology (3 works) · Ecology (3 works) · Pollen (3 works) · Archaeology (2 works)