25.06.2013 Views

Ecologie des foraminifères planctoniques du golfe de Gascogne ...

Ecologie des foraminifères planctoniques du golfe de Gascogne ...

Ecologie des foraminifères planctoniques du golfe de Gascogne ...

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

tel-00480660, version 1 - 4 May 2010<br />

Temperature (°C) Oxygen (ml/l) Phosphate (µg at/l) Nitrate (µg at/l ) Species<br />

T°C=0-27°C (optim 3-19°C) (Bé and Tol<strong>de</strong>rlund, 1971); 13,4°C +-7,1 (Bé,<br />

1977); T°C= 2-27°C (optimale <strong>de</strong> 3-19°C) (Pujol, 1980); T°C optimale = 18,8<br />

(T°C <strong>de</strong> calcification). T min = 5,4°C (Peeters, 2000); 9-25°C (optimal = 7-<br />

28°C) (Lombard et al., 2009)<br />

23,5°C +- 4,4 (Bé, 1977) 10-30°C (optim 17-25°C) (Pujol, 1980); 20-29 (11-<br />

12°C) (Lombard et al., 2009)<br />

6,27 +-0,44ml/l (Bé, 1977)<br />

0,742 +-1,15 (Bé, 1977); high<br />

concentrations (Ufkes et al.,<br />

1998)<br />

high concentration<br />

(Ufkes et al 1998)<br />

G. bulloi<strong><strong>de</strong>s</strong><br />

4,88 +-1 ml/l (Bé, 1977) 0,218 +-1,52 (Bé, 1977) G. siphonifera<br />

15-30°C (17-27)(Hilbrecht, 1996) G. calida<br />

1-16°C (optimal 5-10°C) (Pujol, 1980) optimal à 12°C (Bé and Tol<strong>de</strong>rlund,<br />

1971) ; 9,8°C +- 5,4 (Bé, 1977; Hilbrecht, 1996)<br />

18-24°C (Bé and Tol<strong>de</strong>rlund, 1971). 22°C +- 7,55 (Bé, 1977); optimal between<br />

11-25°C (Pujol, 1980)<br />

0-10°C (5-10°C) (Bé, 1977); cold water species (Boltovskoy and Wright, 1976)<br />

T°C= 24,2°C +- 3,5 (Bé, 1977); T optimale = ~23°C (Peeters, 2000, chapitre<br />

5); Tolerance 16 - 31°C (Hemleben et al 1989). Temperature > 14°C (Pujol,<br />

1980); 14-30°C with max of abundance between 21-29°C (Bé and Tol<strong>de</strong>rlund,<br />

1971; Hilbrecht, 1996); 20-29°C (Lombard et al., 2009)<br />

6,615 +-0,3ml/l (Bé, 1977) 0,88 +-0,21 (Bé, 1977) T. quinqueloba<br />

High (similar to T.<br />

quinqueloba values)<br />

0,369 +-1,93 (Bé, 1977) G. glutinata<br />

G. uvula<br />

4,84 +-0,57ml/l (Bé, 1977) 0,193 +-1,57 (Bé, 1977) G. ruber (white)<br />

T°C= 15-30°C (21-29°C) (Pujol, 1980) G. trilobus trilobus<br />

Globigerinoi<strong><strong>de</strong>s</strong> sacculifer preferred warmer waters than G. ruber, was more<br />

abundant at a shallower <strong>de</strong>pth and might be more influenced by light intensity<br />

(Kuroyanagi and Kawahata, 2004) T°C= 15-30°C (21-29°C) (Tol<strong>de</strong>rlund and<br />

Bé, 1971; Pujol, 1980); 20-29°C (Lombard et al., 2009)<br />

0,198 +-1,38(Bé, 1977) G. trilobus sacculifer<br />

10 (optimal 13-20°C) 27°C (Pujol, 1980) G. hirsuta<br />

16,5 +-3,8°C (Bé, 1977); 5-25°C (15-24) (Hilbrecht, 1996); >16°C ? (Cléroux et<br />

al. 2007). 13-17°C (Bé and Hamlin, 1967), but may occur <strong>du</strong>ring winter at 10°C<br />

(Cifelli and Smith, 1970). Max frequencies occur at surface t°C between 20-<br />

22°C (Bradshaw, 1959); prefers homothermal water masses created <strong>du</strong>ring<br />

winter (Coulbourn et al., 1980; Ganssen and Sarnthein, 1982)<br />

22,7+-3,7°C in indian ocean (Bé, 1977) ; between 5 and 10°C (Pujol, 1980); 10-<br />

30°C (15-20°C) (Hilbrecht, 1996); A <strong>de</strong>ep dwelling habitat (Bé, 1969) may be<br />

suggested by the close relation with temperatures at 200 m <strong>de</strong>pth (Hilbrecht,<br />

1996)<br />

20,3 +-2,8°C (Bé, 1977) ; 5-28°C optimale <strong>de</strong> 15-22°C (Pujol, 1980; Hilbrecht,<br />

1996)<br />

5,66 +-0,37ml/l (Bé, 1977)<br />

20,3 +-2,8°C (Bé, 1977) ; 5-28°C optimale <strong>de</strong> 15-22°C (Pujol, 1980) 5,2 +-0,22ml/l (Bé, 1977)<br />

0-18°C; 4,8 +-5,52°C (Bé, 1977); eaux <strong>de</strong> 10-18°C (Bé and Tol<strong>de</strong>rlund, 1971)<br />

ou 6-15°C (Hilbrecht, 1996); low temperatures (Ufkes et al 1998)<br />

0,365 +-0,42 (Bé, 1977); high<br />

concentration (Ufkes et al<br />

1998); Follows 0,3-0,4µMol/l<br />

PO4 concentration line in<br />

seawater (Cléroux et al. 2007)<br />

High concentration<br />

(Ufkes et al 1998)<br />

G.inflata<br />

4,95 +-0,17ml/l (Bé, 1977) 0,222 +-0,88 (Bé, 1977) G. scitula<br />

5,2 +-0,22ml/l (Bé, 1977) 0,191 +-0,36 (Bé, 1977) G. truncatulinoi<strong><strong>de</strong>s</strong> senestre<br />

7,5 +-0,34ml/l (Bé, 1977)<br />

0-18°C; 4,8 +-5,52°C (Bé, 1977); Toptimales= 0-6°C (Pujol, 1980) 7,5 +-0,34ml/l (B é, 1977)<br />

0,191 +-0,36 (Bé, 1977); lives<br />

in phosphate-rich waters<br />

(Cléroux et al. 2007; Mulitza et<br />

al 1999)<br />

1,517 +-0,45 (Bé, 1977); high<br />

concentrations (Ufkes et al<br />

1998)<br />

1,517 +-0,45 (Bé, 1977);<br />

pro<strong>du</strong>ctive zones (Pujol, 1980)<br />

High concentration<br />

(Ufkes et al 1998)<br />

High concentration<br />

(Ufkes et al 1998)<br />

G. truncatulinoi<strong><strong>de</strong>s</strong> <strong>de</strong>xtre<br />

N. pachy<strong>de</strong>rma <strong>de</strong>xtre<br />

pachy<strong>de</strong>rma senestre<br />

23,2+- 3°C (Bé, 1977); 13-33°C (Pujol, 1980) P-D intergra<strong>de</strong>-<strong>du</strong>tertrei<br />

21,7 +-2,4°C (Bé, 1977); 12 - 31°C, its size is correled with T°C and nutrient s<br />

(Hemleben et al., 1989). 10-30°C (17-25) (Pujol, 1980); high temperatures<br />

(Ufkes et al 1998); 20-29°C (Lombard et al., 2009)<br />

16-29°C (max abundance from 20-26°C) (Bé and Tol<strong>de</strong>rlund, 1971; Pujol,<br />

1980)<br />

5,08 +-0,197ml/l (Bé, 1977) 0,152 +-0,98 (Bé, 1977) O. universa<br />

H. pelagica

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!