(Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2009
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| _version_ | 1867170986923655168 |
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| author | Vogt, Christoph Knies, Jochen |
| author_facet | Vogt, Christoph Knies, Jochen |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | A new surface sediment sample set gained in the western Barents Sea by the MAREANO program has been analysed for basic clay mineral assemblages. Distribution maps including additional samples from earlier German research cruises to and off Svalbard are compiled. Some trends in the clay mineral assemblages are related to the sub-Barents Sea geology because the Quaternary sediment cover is rather thin. Additionally, land masses like Svalbard and northern Scandinavia dominate the clay mineral signal with their erosional products. Dense bottom water, very often of brine origin, that flows within deep troughs, such as the Storfjorden or Bear Island Trough, transport the clay mineral signal from their origin to the Norwegian-Greenland Sea. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_853649 |
| institution | PANGAEA |
| language | en |
| publishDate | 2009 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region Vogt, Christoph Knies, Jochen ARK-IX/4; ARK-VIII/2; ARK-VIII/3; AWI_Paleo; Barents Sea; BC; Bear Island Trough; Box corer; Center for Marine Environmental Sciences; Chlorite; DEPTH, sediment/rock; Elevation of event; Event label; Giant box corer; GKG; Gravity corer (Kiel type); HE153; HE153/1239-2; HE153/1240-2; HE153/1241-2; HE153/1242-2; HE153/1243-2; HE153/1244-2; HE153/1245-2; HE153/1246-2; HE153/1249-2; HE153/1250-2; HE153/1251-2; HE153/1254-2; HE153/1255-2; HE153/1258-1; HE153/1260-2; HE153/1261-2; HE153/1262-2; HE153/1263-2; HE153/1264-2; HE153/1265-2; HE153/1266-2; HE153/1267-2; HE153/1268-2; HE153/1269-2; HE153/1270-2; HE153/1272-2; HE153/1273-2; HE153/1274-2; HE153/1275-2; HE153/1276-2; HE153/1278-2; HE153/1279-2; HE153/1280-2; HE153/1282-2; HE153/1283-2; HE153/1284-2; HE153/1285-2; HE153/1286-2; HE153/1287-2; HE153/1288-2; HE153/1289-2; HE153/1290-2; HE153/1292-2; Heincke; HM_St01; HM_St02; HM_St03; HM_St04; HM_St05; HM_St06; HM_St07; HM_St08; HM_St09; HM_St11; HM_St12; HM_St13; HM_St14; HM_St15; HM_St16; HM_St17; HM_St18; HM_St19; HM_St20; HM_St21; HM_St22; HM_St23; HM_St24; HM_St25; HM_St26; HM_St27; HM_St28; HM_St29; HM_St30; HM_St31; HM_St32; HM_St33; HM_St34; HM_St35; HM_St36; HM_St37; HM_St38; HM_St39; HM_St40; HM_St41; HM_St42; HM_St43; HM_St44; HM_St45; HM_St625; HM_St627; HM_St629; HM_St631; HM_St633; HM_St635; HM_St639; HM_St643; HM_St645; HM_St647; HM_St649; HM_St651; HM_St653; HM_St655; HM_St657; HM_St659; HM_St661; HM_St663; HM_St665; HM_St667; HM_St669; HM_St671; HM_St673; HM_St675; HM_St677; HM_St679; HM_St681; HM_St690; HM_St692; Illite; Kaolinite; Latitude of event; Longitude of event; MARUM; MUC; MultiCorer; Norwegian Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/040; PS19/045; PS19/050; PS19/055; PS19/070; PS19/078; PS19/080; PS19/081; PS19/082; PS19/084; PS19/086; PS19/090; PS19/091; PS19/094; PS19/098; PS19/100; PS19/101; PS19/102; PS19/104; PS19/105; PS19/108; PS19/110; PS19/111; PS19/112; PS19/116; PS19/117; PS19/119; PS19/124; PS19/126; PS19/132; PS19/134; PS19/136; PS19/143; PS19/246; PS19/249; PS19 ARCTIC91; PS19 EPOS II; PS2111-2; PS2113-1; PS2114-1; PS2115-1; PS2116-1; PS2117-1; PS2119-2; PS2120-1; PS2121-1; PS2122-1; PS2123-3; PS2124-1; PS2125-2; PS2127-1; PS2128-1; PS2129-2; PS2130-2; PS2131-1; PS2132-3; PS2133-1; PS2134-1; PS2136-3; PS2137-4; PS2138-2; PS2142-3; PS2143-1; PS2144-3; PS2147-3; PS2148-1; PS2149-1; PS2150-1; PS2151-1; PS2153-1; PS2213-1; PS2214-1; PS2439-1; PS2440-5; PS2441-1; PS2447-5; PS2448-1; PS2449-3; PS27; PS27/001; PS27/006; PS27/007; PS27/024; PS27/025; PS27/027; Sample ID; SL; Smectite; Svalbard; X-ray diffraction (XRD); Yermak Plateau A new surface sediment sample set gained in the western Barents Sea by the MAREANO program has been analysed for basic clay mineral assemblages. Distribution maps including additional samples from earlier German research cruises to and off Svalbard are compiled. Some trends in the clay mineral assemblages are related to the sub-Barents Sea geology because the Quaternary sediment cover is rather thin. Additionally, land masses like Svalbard and northern Scandinavia dominate the clay mineral signal with their erosional products. Dense bottom water, very often of brine origin, that flows within deep troughs, such as the Storfjorden or Bear Island Trough, transport the clay mineral signal from their origin to the Norwegian-Greenland Sea. |
| title | (Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region |
| topic | ARK-IX/4; ARK-VIII/2; ARK-VIII/3; AWI_Paleo; Barents Sea; BC; Bear Island Trough; Box corer; Center for Marine Environmental Sciences; Chlorite; DEPTH, sediment/rock; Elevation of event; Event label; Giant box corer; GKG; Gravity corer (Kiel type); HE153; HE153/1239-2; HE153/1240-2; HE153/1241-2; HE153/1242-2; HE153/1243-2; HE153/1244-2; HE153/1245-2; HE153/1246-2; HE153/1249-2; HE153/1250-2; HE153/1251-2; HE153/1254-2; HE153/1255-2; HE153/1258-1; HE153/1260-2; HE153/1261-2; HE153/1262-2; HE153/1263-2; HE153/1264-2; HE153/1265-2; HE153/1266-2; HE153/1267-2; HE153/1268-2; HE153/1269-2; HE153/1270-2; HE153/1272-2; HE153/1273-2; HE153/1274-2; HE153/1275-2; HE153/1276-2; HE153/1278-2; HE153/1279-2; HE153/1280-2; HE153/1282-2; HE153/1283-2; HE153/1284-2; HE153/1285-2; HE153/1286-2; HE153/1287-2; HE153/1288-2; HE153/1289-2; HE153/1290-2; HE153/1292-2; Heincke; HM_St01; HM_St02; HM_St03; HM_St04; HM_St05; HM_St06; HM_St07; HM_St08; HM_St09; HM_St11; HM_St12; HM_St13; HM_St14; HM_St15; HM_St16; HM_St17; HM_St18; HM_St19; HM_St20; HM_St21; HM_St22; HM_St23; HM_St24; HM_St25; HM_St26; HM_St27; HM_St28; HM_St29; HM_St30; HM_St31; HM_St32; HM_St33; HM_St34; HM_St35; HM_St36; HM_St37; HM_St38; HM_St39; HM_St40; HM_St41; HM_St42; HM_St43; HM_St44; HM_St45; HM_St625; HM_St627; HM_St629; HM_St631; HM_St633; HM_St635; HM_St639; HM_St643; HM_St645; HM_St647; HM_St649; HM_St651; HM_St653; HM_St655; HM_St657; HM_St659; HM_St661; HM_St663; HM_St665; HM_St667; HM_St669; HM_St671; HM_St673; HM_St675; HM_St677; HM_St679; HM_St681; HM_St690; HM_St692; Illite; Kaolinite; Latitude of event; Longitude of event; MARUM; MUC; MultiCorer; Norwegian Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS19/040; PS19/045; PS19/050; PS19/055; PS19/070; PS19/078; PS19/080; PS19/081; PS19/082; PS19/084; PS19/086; PS19/090; PS19/091; PS19/094; PS19/098; PS19/100; PS19/101; PS19/102; PS19/104; PS19/105; PS19/108; PS19/110; PS19/111; PS19/112; PS19/116; PS19/117; PS19/119; PS19/124; PS19/126; PS19/132; PS19/134; PS19/136; PS19/143; PS19/246; PS19/249; PS19 ARCTIC91; PS19 EPOS II; PS2111-2; PS2113-1; PS2114-1; PS2115-1; PS2116-1; PS2117-1; PS2119-2; PS2120-1; PS2121-1; PS2122-1; PS2123-3; PS2124-1; PS2125-2; PS2127-1; PS2128-1; PS2129-2; PS2130-2; PS2131-1; PS2132-3; PS2133-1; PS2134-1; PS2136-3; PS2137-4; PS2138-2; PS2142-3; PS2143-1; PS2144-3; PS2147-3; PS2148-1; PS2149-1; PS2150-1; PS2151-1; PS2153-1; PS2213-1; PS2214-1; PS2439-1; PS2440-5; PS2441-1; PS2447-5; PS2448-1; PS2449-3; PS27; PS27/001; PS27/006; PS27/007; PS27/024; PS27/025; PS27/027; Sample ID; SL; Smectite; Svalbard; X-ray diffraction (XRD); Yermak Plateau |
| url | https://doi.org/10.1594/PANGAEA.853649 |