(Table 1) Composition of lipids in particulate matter and bottom sediments of the Baltic Sea
Fuente:
PANGAEA
Salvato in:
| Autori principali: | , |
|---|---|
| Natura: | Dataset Open Access |
| Lingua: | en |
| Pubblicazione: |
PANGAEA
1982
|
| Soggetti: | |
| Accesso online: | |
| Tags: |
Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
|
| _version_ | 1867171774980947968 |
|---|---|
| author | Bobyleva, Nadezhda V Belyaeva, Alexandra N |
| author_facet | Bobyleva, Nadezhda V Belyaeva, Alexandra N |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Lipid contents in the upper layer of bottom sediments in the Baltic Sea range from 0.37 to 2.66 mg/g (1.2-25.8% Corg). It is shown that the main factors determining composition of lipids in bottom precipitates are relative roles of different sources of lipids in sediments and conditions of sediment accumulation. Runoff of the Daugava River into the Gulf of Riga contributes simple low-polarity lipids. Sterols and certain bound fatty acids originate in living organic matter. Polar lipids are formed by inheritance of complex phospholipids and glycolipids from plankton and/or by formation of polycondensates. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_755698 |
| institution | PANGAEA |
| language | en |
| publishDate | 1982 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Composition of lipids in particulate matter and bottom sediments of the Baltic Sea Bobyleva, Nadezhda V Belyaeva, Alexandra N AK26A-2575; AK26A-2577; AK26A-2589; AK26A-2590; AK26A-2599; AK26A-2618; AK26A-2665; Akademik Kurchatov; AKU26A; Aliphatic alcohols as percentage of lipids; Archive of Ocean Data; ARCOD; Baltic Sea; Calculated; Carbon, organic, fraction; Carbon, organic, total; Chromatographic; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diglycerides of lipids; Eh, Pt-electrode; Elevation of event; Event label; Fatty acid esters of lipids; Fatty acids of lipids; Gulf of Gdansk; Gulf of Riga; Hydrocarbons of lipids; Latitude of event; Lipid organic carbon of total organic carbon; Lipids, polar; Lipids, unidentified; Longitude of event; MULT; Multiple investigations; Oxidation reduction (RedOx) potential; pH; Primary production of carbon; Sedimentation rate per year; Sediment type; Sterols of lipids; Sterol wax esters of lipids; Triglycerides of lipids; Wet chemistry Lipid contents in the upper layer of bottom sediments in the Baltic Sea range from 0.37 to 2.66 mg/g (1.2-25.8% Corg). It is shown that the main factors determining composition of lipids in bottom precipitates are relative roles of different sources of lipids in sediments and conditions of sediment accumulation. Runoff of the Daugava River into the Gulf of Riga contributes simple low-polarity lipids. Sterols and certain bound fatty acids originate in living organic matter. Polar lipids are formed by inheritance of complex phospholipids and glycolipids from plankton and/or by formation of polycondensates. |
| title | (Table 1) Composition of lipids in particulate matter and bottom sediments of the Baltic Sea |
| topic | AK26A-2575; AK26A-2577; AK26A-2589; AK26A-2590; AK26A-2599; AK26A-2618; AK26A-2665; Akademik Kurchatov; AKU26A; Aliphatic alcohols as percentage of lipids; Archive of Ocean Data; ARCOD; Baltic Sea; Calculated; Carbon, organic, fraction; Carbon, organic, total; Chromatographic; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diglycerides of lipids; Eh, Pt-electrode; Elevation of event; Event label; Fatty acid esters of lipids; Fatty acids of lipids; Gulf of Gdansk; Gulf of Riga; Hydrocarbons of lipids; Latitude of event; Lipid organic carbon of total organic carbon; Lipids, polar; Lipids, unidentified; Longitude of event; MULT; Multiple investigations; Oxidation reduction (RedOx) potential; pH; Primary production of carbon; Sedimentation rate per year; Sediment type; Sterols of lipids; Sterol wax esters of lipids; Triglycerides of lipids; Wet chemistry |
| url | https://doi.org/10.1594/PANGAEA.755698 |