Gert J De Lange
Biographic Data
| ID | 6370802 |
|---|---|
| NAME | Gert J De Lange |
| GIVEN NAMES | Gert J |
| FAMILY NAME | De Lange |
| SIGNATURE | DE LANGE G J |
| AFFILIATIONS | Utrecht University |
| ORCID | 0000-0002-9420-3022 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 3 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2013 |
| LATEST PUBLICATION YEAR | 2019 |
| H-INDEX | 1 |
Trace metal analysis of sediment cores using a novel X-ray fluorescence core scanning method
Paleoenvironmental conditions at Core KC01B (Ionian Sea) through MIS 13–9
Climate of the past 2500 years in the Gulf of Taranto, central Mediterranean Sea
We present a high-resolution isotope stratigraphy based on Globigerinoides ruber (white) over the past 2500 years in the Gulf of Taranto, central Mediterranean. G. ruber (white) reflects summer conditions in the Gulf of Taranto but is influenced by two major surface water masses: the Western Adriatic Current (WAC) and the Ionian Surface Water (ISW) and their variations on a decadal to multicentennial scale. Our analysis of the δ 13 C and δ 18 O o…
Climate of the past 2500 years in the Gulf of Taranto, central Mediterranean Sea
We present a high-resolution isotope stratigraphy based on Globigerinoides ruber (white) over the past 2500 years in the Gulf of Taranto, central Mediterranean. G. ruber (white) reflects summer conditions in the Gulf of Taranto but is influenced by two major surface water masses: the Western Adriatic Current (WAC) and the Ionian Surface Water (ISW) and their variations on a decadal to multicentennial scale. Our analysis of the δ 13 C and δ 18 O o…
Paleoenvironmental conditions at Core KC01B (Ionian Sea) through MIS 13–9
Climate of the past 2500 years in the Gulf of Taranto, central Mediterranean Sea
We present a high-resolution isotope stratigraphy based on Globigerinoides ruber (white) over the past 2500 years in the Gulf of Taranto, central Mediterranean. G. ruber (white) reflects summer conditions in the Gulf of Taranto but is influenced by two major surface water masses: the Western Adriatic Current (WAC) and the Ionian Surface Water (ISW) and their variations on a decadal to multicentennial scale. Our analysis of the δ 13 C and δ 18 O o…
Trace metal analysis of sediment cores using a novel X-ray fluorescence core scanning method
Geology (3 works) · Dominance (genetics (2 works) · Geology and Paleoclimatology Research (2 works) · Mediterranean climate (2 works) · Mediterranean sea (2 works) · Oceanography (2 works) · Stable isotope ratio (2 works) · δ18O (2 works) · Archaeology (1 works) · Archaeology and ancient environmental studies (1 works)