Fig. 1. Delta 18O values of planktic formaminifera in surface sediment samples from the South Atlantic Ocean
Fuente:
PANGAEA
Salvato in:
| Autori principali: | , , |
|---|---|
| Natura: | Dataset Open Access |
| Lingua: | en |
| Pubblicazione: |
PANGAEA
1999
|
| Soggetti: | |
| Accesso online: | |
| Tags: |
Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
|
| _version_ | 1867167689199321088 |
|---|---|
| author | Niebler, Hans-Stefan Hubberten, Hans-Wolfgang Gersonde, Rainer |
| author_facet | Niebler, Hans-Stefan Hubberten, Hans-Wolfgang Gersonde, Rainer |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The d18Ocalcite composition of planktic foraminiferal shells in 59 samples collected from surface sediments between 34°S (south-eastern Subtropical Gyre) and 56°S (Antarctic Zone of the Antarctic Circumpolar Current) and additionally from 20°S (Walvis Ridge) in the South Atlantic Ocean documents the apparent calcification depth of 24 planktic foraminiferal taxa. Based on the d18Ocalcite signal of their shells, four depth related groups of foraminifera are distinguished, calcifying in a depth between 0 and 50 m (Sphaeroidinella dehiscens, Pulleniatina obliquiloculata, Orbulina bilobata, Globigerinoides sacculifer (with and without sac), Globigerinella aequilateralis, Globigerinoides ruber (white), Globigerina bulloides); 0 and 200 m (Globigerinoides conglobatus, Orbulina universa, Neogloboquadrina dutertrei, Turborotalita quinqueloba, Neogloboquadrina pachyderma (dextral and sinistral)); 100 and 250 m (Globorotalia tumida, Globorotalia menardii, Globigerinella calida, Globorotalia inflata); and deeper than 250 m (Globorotalia hirsuta, Globorotalia scitula, Globorotalia crassaformis, Globorotalia truncatulinoides (dextral and sinistral)). We propose a method to reconstruct temperature gradients between various depths in the water column, but most specifically between 30 m and 250 m, using the d18Ocalcite composition of foraminiferal calcite. Changes in past sea-surface water stratification in the temperate southern South Atlantic Ocean and in the Antarctic Circumpolar Current can be reconstructed in particular with G. bulloides, G. truncatulinoides and G. inflata. Modern temperature gradients between 30 m and 250 m water depth are reconstructed accurately within a range between 1.7 and 9.4 °C with a correlation coefficient of 0.77 and a standard deviation of ±1.3 °C. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_55882 |
| institution | PANGAEA |
| language | en |
| publishDate | 1999 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Fig. 1. Delta 18O values of planktic formaminifera in surface sediment samples from the South Atlantic Ocean Niebler, Hans-Stefan Hubberten, Hans-Wolfgang Gersonde, Rainer Agulhas Basin; ANT-IX/4; ANT-VI/3; ANT-VIII/3; ANT-X/4; ANT-X/5; ANT-X/6; Atlantic Indik Ridge; Atlantic Ridge; CTD/Rosette; CTD-RO; DEPTH, sediment/rock; Discovery Seamount; Elevation of event; Event label; Giant box corer; GKG; Globigerina bulloides, δ18O; Globigerinella aequilateralis, δ18O; Globigerinella calida, δ18O; Globigerinita glutinata, δ18O; Globigerinoides conglobatus, δ18O; Globigerinoides ruber white, δ18O; Globigerinoides sacculifer, δ18O; Globigerinoides sacculifer sac, δ18O; Globorotalia crassaformis, δ18O; Globorotalia hirsuta, δ18O; Globorotalia inflata, δ18O; Globorotalia menardii, δ18O; Globorotalia scitula, δ18O; Globorotalia truncatulinoides dextral, δ18O; Globorotalia truncatulinoides sinistral, δ18O; Globorotalia tumida, δ18O; LATITUDE; LONGITUDE; Mass spectrometer Finnigan MAT 251; Meteor Rise; MIC; MiniCorer; MUC; MultiCorer; Neogloboquadrina dutertrei, δ18O; Neogloboquadrina pachyderma dextral, δ18O; Neogloboquadrina pachyderma sinistral, δ18O; Orbulina bilobata, δ18O; Orbulina universa, δ18O; Polarstern; PS12; PS12/557; PS16; PS16/262; PS16/267; PS16/271; PS16/278; PS16/281; PS16/284; PS16/294; PS16/303; PS16/342; PS16/345; PS16/351; PS1654-1; PS1750-7; PS1751-2; PS1752-5; PS1754-2; PS1755-1; PS1756-6; PS1759-1; PS1764-2; PS1777-7; PS1778-1; PS1779-3; PS18; PS18/229; PS18/231; PS18/232; PS18/236; PS18/237; PS18/238; PS18/239; PS18/241; PS18/242; PS18/243; PS18/244; PS18/261; PS18/262; PS18/263; PS18/264; PS18/269; PS2073-1; PS2075-3; PS2076-1; PS2080-1; PS2081-1; PS2082-3; PS2083-1; PS2084-2; PS2085-1; PS2086-3; PS2087-1; PS2103-2; PS2104-1; PS2105-2; PS2106-1; PS21 06AQANTX_4; PS2110-1; PS22; PS22/678; PS22/679; PS22/840; PS22/841; PS22/842; PS22/850; PS22/851; PS22/852; PS22/853; PS22/879; PS22/902; PS22/908; PS22/973; PS22 06AQANTX_5; PS2230-1; PS2231-1; PS2233-1; PS2234-1; PS2235-1; PS2237-1; PS2238-1; PS2239-1; PS2240-1; PS2241-1; PS2242-1; PS2250-6; PS2251-1; PS2256-4; PS2341-1; PS2342-1; PS2343-1; PS2351-1; PS2352-1; PS2353-2; PS2354-1; PS2363-1; PS2367-1; PS2368-1; PS2376-1; Pulleniatina obliquiloculata, δ18O; SFB261; Shona Ridge; Size fraction; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; South Atlantic Ocean; Sphaeroidinella dehiscens, δ18O; Turborotalita quinqueloba, δ18O; Van Heesen Ridge; Walvis Ridge The d18Ocalcite composition of planktic foraminiferal shells in 59 samples collected from surface sediments between 34°S (south-eastern Subtropical Gyre) and 56°S (Antarctic Zone of the Antarctic Circumpolar Current) and additionally from 20°S (Walvis Ridge) in the South Atlantic Ocean documents the apparent calcification depth of 24 planktic foraminiferal taxa. Based on the d18Ocalcite signal of their shells, four depth related groups of foraminifera are distinguished, calcifying in a depth between 0 and 50 m (Sphaeroidinella dehiscens, Pulleniatina obliquiloculata, Orbulina bilobata, Globigerinoides sacculifer (with and without sac), Globigerinella aequilateralis, Globigerinoides ruber (white), Globigerina bulloides); 0 and 200 m (Globigerinoides conglobatus, Orbulina universa, Neogloboquadrina dutertrei, Turborotalita quinqueloba, Neogloboquadrina pachyderma (dextral and sinistral)); 100 and 250 m (Globorotalia tumida, Globorotalia menardii, Globigerinella calida, Globorotalia inflata); and deeper than 250 m (Globorotalia hirsuta, Globorotalia scitula, Globorotalia crassaformis, Globorotalia truncatulinoides (dextral and sinistral)). We propose a method to reconstruct temperature gradients between various depths in the water column, but most specifically between 30 m and 250 m, using the d18Ocalcite composition of foraminiferal calcite. Changes in past sea-surface water stratification in the temperate southern South Atlantic Ocean and in the Antarctic Circumpolar Current can be reconstructed in particular with G. bulloides, G. truncatulinoides and G. inflata. Modern temperature gradients between 30 m and 250 m water depth are reconstructed accurately within a range between 1.7 and 9.4 °C with a correlation coefficient of 0.77 and a standard deviation of ±1.3 °C. |
| title | Fig. 1. Delta 18O values of planktic formaminifera in surface sediment samples from the South Atlantic Ocean |
| topic | Agulhas Basin; ANT-IX/4; ANT-VI/3; ANT-VIII/3; ANT-X/4; ANT-X/5; ANT-X/6; Atlantic Indik Ridge; Atlantic Ridge; CTD/Rosette; CTD-RO; DEPTH, sediment/rock; Discovery Seamount; Elevation of event; Event label; Giant box corer; GKG; Globigerina bulloides, δ18O; Globigerinella aequilateralis, δ18O; Globigerinella calida, δ18O; Globigerinita glutinata, δ18O; Globigerinoides conglobatus, δ18O; Globigerinoides ruber white, δ18O; Globigerinoides sacculifer, δ18O; Globigerinoides sacculifer sac, δ18O; Globorotalia crassaformis, δ18O; Globorotalia hirsuta, δ18O; Globorotalia inflata, δ18O; Globorotalia menardii, δ18O; Globorotalia scitula, δ18O; Globorotalia truncatulinoides dextral, δ18O; Globorotalia truncatulinoides sinistral, δ18O; Globorotalia tumida, δ18O; LATITUDE; LONGITUDE; Mass spectrometer Finnigan MAT 251; Meteor Rise; MIC; MiniCorer; MUC; MultiCorer; Neogloboquadrina dutertrei, δ18O; Neogloboquadrina pachyderma dextral, δ18O; Neogloboquadrina pachyderma sinistral, δ18O; Orbulina bilobata, δ18O; Orbulina universa, δ18O; Polarstern; PS12; PS12/557; PS16; PS16/262; PS16/267; PS16/271; PS16/278; PS16/281; PS16/284; PS16/294; PS16/303; PS16/342; PS16/345; PS16/351; PS1654-1; PS1750-7; PS1751-2; PS1752-5; PS1754-2; PS1755-1; PS1756-6; PS1759-1; PS1764-2; PS1777-7; PS1778-1; PS1779-3; PS18; PS18/229; PS18/231; PS18/232; PS18/236; PS18/237; PS18/238; PS18/239; PS18/241; PS18/242; PS18/243; PS18/244; PS18/261; PS18/262; PS18/263; PS18/264; PS18/269; PS2073-1; PS2075-3; PS2076-1; PS2080-1; PS2081-1; PS2082-3; PS2083-1; PS2084-2; PS2085-1; PS2086-3; PS2087-1; PS2103-2; PS2104-1; PS2105-2; PS2106-1; PS21 06AQANTX_4; PS2110-1; PS22; PS22/678; PS22/679; PS22/840; PS22/841; PS22/842; PS22/850; PS22/851; PS22/852; PS22/853; PS22/879; PS22/902; PS22/908; PS22/973; PS22 06AQANTX_5; PS2230-1; PS2231-1; PS2233-1; PS2234-1; PS2235-1; PS2237-1; PS2238-1; PS2239-1; PS2240-1; PS2241-1; PS2242-1; PS2250-6; PS2251-1; PS2256-4; PS2341-1; PS2342-1; PS2343-1; PS2351-1; PS2352-1; PS2353-2; PS2354-1; PS2363-1; PS2367-1; PS2368-1; PS2376-1; Pulleniatina obliquiloculata, δ18O; SFB261; Shona Ridge; Size fraction; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents; South Atlantic Ocean; Sphaeroidinella dehiscens, δ18O; Turborotalita quinqueloba, δ18O; Van Heesen Ridge; Walvis Ridge |
| url | https://doi.org/10.1594/PANGAEA.55882 |