Michael Styllas
Biographic Data
| ID | 6376972 |
|---|---|
| NAME | Michael Styllas |
| GIVEN NAMES | Michael |
| FAMILY NAME | Styllas |
| SIGNATURE | STYLLAS M |
| AFFILIATIONS | Aristotle University of Thessaloniki |
| ORCID | 0000-0003-4385-0008 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 11 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2007 |
| LATEST PUBLICATION YEAR | 2017 |
| H-INDEX | 1 |
Early- to mid-Holocene paleohydrology in northeast Mediterranean
One of the prominent features of northeast Mediterranean (NEM) Holocene climate are recurrent phases of cold and aridity; their impacts on the hydrological cycle remain at large unknown, as few existing paleohydrological records are either restricted to lake-level fluctuations or focus near the ‘8.2 kyr BP’ event. Here, we present the detrital record of Aliakmon River in Lake Loudias between 9500 and 3000 cal. BP. Magnetic susceptibility (MS) exh…
Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece
This study investigates the possibility of Holocene glaciation on Mount Olympus (Greece) with a respective local temperature–precipitation equilibrium line altitude (TP-ELA) at c. 2200 m a.s.l., based on geomorphologic and paleoclimatic evidence. At present, the local TP-ELA is situated above the mountain’s summit ( c. 2918 m a.s.l.), but permanent snowfields and ice bodies survive within Megala Kazania cirque between c. 2400 and c. 2300 m a.s.l.…
Human occupation and geomorphological evolution of the Thessaloniki Plain (Greece) since mid Holocene
Human occupation and geomorphological evolution of the Thessaloniki Plain (Greece) since mid Holocene
Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece
This study investigates the possibility of Holocene glaciation on Mount Olympus (Greece) with a respective local temperature–precipitation equilibrium line altitude (TP-ELA) at c. 2200 m a.s.l., based on geomorphologic and paleoclimatic evidence. At present, the local TP-ELA is situated above the mountain’s summit ( c. 2918 m a.s.l.), but permanent snowfields and ice bodies survive within Megala Kazania cirque between c. 2400 and c. 2300 m a.s.l.…
Human occupation and geomorphological evolution of the Thessaloniki Plain (Greece) since mid Holocene
Geomorphologic and paleoclimatic evidence of Holocene glaciation on Mount Olympus, Greece
This study investigates the possibility of Holocene glaciation on Mount Olympus (Greece) with a respective local temperature–precipitation equilibrium line altitude (TP-ELA) at c. 2200 m a.s.l., based on geomorphologic and paleoclimatic evidence. At present, the local TP-ELA is situated above the mountain’s summit ( c. 2918 m a.s.l.), but permanent snowfields and ice bodies survive within Megala Kazania cirque between c. 2400 and c. 2300 m a.s.l.…
Early- to mid-Holocene paleohydrology in northeast Mediterranean
One of the prominent features of northeast Mediterranean (NEM) Holocene climate are recurrent phases of cold and aridity; their impacts on the hydrological cycle remain at large unknown, as few existing paleohydrological records are either restricted to lake-level fluctuations or focus near the ‘8.2 kyr BP’ event. Here, we present the detrital record of Aliakmon River in Lake Loudias between 9500 and 3000 cal. BP. Magnetic susceptibility (MS) exh…
Geology (3 works) · Holocene (3 works) · Oceanography (3 works) · Paleontology (3 works) · Archaeology (2 works) · Archaeology and ancient environmental studies (2 works) · Geography (2 works) · Geology and Paleoclimatology Research (2 works) · Physical geography (2 works) · Ancient Mediterranean Archaeology and History (1 works)