Hydrography and water chemistry of the open Mediterranean Sea
Fuente:
PANGAEA
Salvato in:
| Autori principali: | , |
|---|---|
| Natura: | Dataset Open Access |
| Lingua: | en |
| Pubblicazione: |
PANGAEA
1981
|
| Soggetti: | |
| Accesso online: | |
| Tags: |
Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
|
| _version_ | 1867169496108630016 |
|---|---|
| author | Kremling, Klaus Petersen, Hauke |
| author_facet | Kremling, Klaus Petersen, Hauke |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | On a cruise from the eastern into western Mediterranean Sea in November/December 1978 a total of 126 samples were collected from 8 vertical profiles and 7 coastal stations for trace metal analysis. The sampling, processing and analysis was performed under strict "clean room" conditions. The concentration of the open-sea samples are close to oceanic results gathered under similar conditions. The grand averages from all profiles (± st. dev. of the individual samples) of 0.40 ± 0.16 µg/l Zn, 17.4 ± 7.4 ng/l Cd, 0.21 ± 0.07 µg/l Cu, 0.21 ± 0.13 µg/l Mn and 0.25 ± 0.09 µg/l Fe indicate that a "metal problem" does not exist in the open Mediterranean. A biologically mediated deplition in surface waters or correlation with nutrients have not been observed under the conditions established on this cruise. This is probably due top low primary production and seasonal advection processes prevailing in this sea. The data for manganese show generally higher values in the surface layer (0-75 m) than in deep waters. This could evidently proved in the nearshore profile indicating a terrigenous source for manganese. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_604843 |
| institution | PANGAEA |
| language | en |
| publishDate | 1981 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Hydrography and water chemistry of the open Mediterranean Sea Kremling, Klaus Petersen, Hauke GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M50; M50_390; M50_395; M50_407; M50_409; M50_415; M50_421; M50_424; M50_428; M50_430; M50_432; M50_436; M50_437; M50_440; M50_450; M50_453; Mediterranean Sea; Meteor (1964); Water sample; WS On a cruise from the eastern into western Mediterranean Sea in November/December 1978 a total of 126 samples were collected from 8 vertical profiles and 7 coastal stations for trace metal analysis. The sampling, processing and analysis was performed under strict "clean room" conditions. The concentration of the open-sea samples are close to oceanic results gathered under similar conditions. The grand averages from all profiles (± st. dev. of the individual samples) of 0.40 ± 0.16 µg/l Zn, 17.4 ± 7.4 ng/l Cd, 0.21 ± 0.07 µg/l Cu, 0.21 ± 0.13 µg/l Mn and 0.25 ± 0.09 µg/l Fe indicate that a "metal problem" does not exist in the open Mediterranean. A biologically mediated deplition in surface waters or correlation with nutrients have not been observed under the conditions established on this cruise. This is probably due top low primary production and seasonal advection processes prevailing in this sea. The data for manganese show generally higher values in the surface layer (0-75 m) than in deep waters. This could evidently proved in the nearshore profile indicating a terrigenous source for manganese. |
| title | Hydrography and water chemistry of the open Mediterranean Sea |
| topic | GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; M50; M50_390; M50_395; M50_407; M50_409; M50_415; M50_421; M50_424; M50_428; M50_430; M50_432; M50_436; M50_437; M50_440; M50_450; M50_453; Mediterranean Sea; Meteor (1964); Water sample; WS |
| url | https://doi.org/10.1594/PANGAEA.604843 |