Scheda di dettaglio – i prodotti della ricerca
| Dato | Valore |
|---|---|
| Title | The late Pleistocene ostracod record of the crater lake sediments from Lago di Albano (Central Italy): Changes in trophic status, water level and climate |
| Abstract | Four cores (ranging between ca. 9 and ca. 14 m in length) from Lago di Albano in Central Italy were studied for their ostracod content, as well as algal and bacterial pigments, CaCO3 and concentration of organic matter. Cores PALB 94 1E and PALB 94 1C from Site 1, located at the bottom of a steep slope at 70 m water depth, where oxygen concentration is below 6 mg l(-1), spans the Holocene and the late Pleistocene until 28 kyr B. P. (calibrated age). The other cores, PALB 94 6A and PALB 94 6B taken at a depth of 30 m, where oxygen is 7-11 mg l(-1), represent mainly Pleistocene deposits. |
| Source | Journal of paleolimnology 21 (2), pp. 151–169 |
| Keywords | ostracodspigmentspalaeoecologylate PleistoceneCentral Italymaar lakes |
| Journal | Journal of paleolimnology |
| Editor | Kluwer Academic, Boston, Paesi Bassi |
| Year | 1999 |
| Type | Articolo in rivista |
| DOI | 10.1023/A:1008095805748 |
| Authors | Belis, CA; Lami, A; Guilizzoni, P; Ariztegui, D; Geiger, W |
| Text | 407947 1999 10.1023/A 1008095805748 ISI Web of Science WOS 000080287800002 ostracods pigments palaeoecology late Pleistocene Central Italy maar lakes The late Pleistocene ostracod record of the crater lake sediments from Lago di Albano Central Italy Changes in trophic status, water level and climate Belis, CA; Lami, A; Guilizzoni, P; Ariztegui, D; Geiger, W CNR; ETH Zurich; Austrian Acad Sci Four cores ranging between ca. 9 and ca. 14 m in length from Lago di Albano in Central Italy were studied for their ostracod content, as well as algal and bacterial pigments, CaCO3 and concentration of organic matter. Cores PALB 94 1E and PALB 94 1C from Site 1, located at the bottom of a steep slope at 70 m water depth, where oxygen concentration is below 6 mg l 1 , spans the Holocene and the late Pleistocene until 28 kyr B. P. calibrated age . The other cores, PALB 94 6A and PALB 94 6B taken at a depth of 30 m, where oxygen is 7 11 mg l 1 , represent mainly Pleistocene deposits. Ostracod valves were found in the lowermost ca. 3 m of the sequence at Site 1, dated to ca. 28 24 kyr B. P., and throughout the sequence from Site 6 which represents the interval 23 17 kyr B. P. 21 Published version Articolo in rivista Kluwer Academic 0921 2728 Journal of paleolimnology Journal of paleolimnology J. paleolimnol. piero.guilizzoni GUILIZZONI PIERO andrea.lami LAMI ANDREA |