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Marine Ecosystems Research Department - jamstec japan agency ...

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Japan <strong>Marine</strong> Science and Technology Center<br />

Ocean Observation and <strong>Research</strong> <strong>Department</strong><br />

0<br />

ExcessCO2 [UMOL/KG]<br />

70<br />

DEPTH [M]<br />

DEPTH [M]<br />

500<br />

1000<br />

1500<br />

0<br />

500<br />

1000<br />

1500<br />

20N 25N 30N 35N 40N<br />

CFC-11 [PMOL/KG]<br />

20N 25N 30N 35N 40N<br />

Ocean Data View Ocean Data View<br />

60<br />

50<br />

40<br />

30<br />

20<br />

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50N<br />

30N<br />

Ocean Data View<br />

10N<br />

130E 150E 170E<br />

Fig.15 Distribution of the anthropogenic CO 2 and CFC-11 along 155E in 2003.<br />

CFC- along E line.<br />

(b) We measured nutrients and dissolved oxygen gas<br />

concentrations in seawater during the JARE<br />

Antarctic voyage abroad the R/V Tangaroa in<br />

February . Samples for measurement of some<br />

biogenic dissolved gases in seawater were also collected.<br />

Methane concentrations and stable carbon isotopes<br />

collected during the JARE Antarctic voyage in <br />

were also analyzed.<br />

Distributions of dissolved methane, silicate and<br />

dimethyl sulfide (DMS) concentrations along E<br />

in are shown Fig.-, - and -, respectively.<br />

High concentrations of methane were found on<br />

the continental slope. This distribution is similar to<br />

that of silicate. The water mass with high methane<br />

concentration might be related to surface or shelf<br />

water. The stable carbon isotope ratio of methane suggests<br />

that the methane was not decomposed yet.<br />

Higher DMS concentrations were found around<br />

S in February , which were observed also in<br />

the R/V Hakuho-Maru cruise conducted in January.<br />

However, ratios between DMS, dissolved DMSP and<br />

DIMSP were not same between the cruises. Changes<br />

of the ratios are important to make clear the role of<br />

phyto- and zooplankton for the formation of DMS in<br />

surface seawater.<br />

16-1<br />

Depth [m]<br />

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16-2 0<br />

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CH4 [nmol/kg]<br />

64˚S 62˚S 60˚S 58˚S 56˚S 54˚S<br />

Si [µmol/kg]<br />

66˚S 64˚S 62˚S 60˚S 58˚S 56˚S 54˚S<br />

DMS [nmol/1]<br />

66˚S 64˚S 62˚S 60˚S 58˚S 56˚S<br />

Fig.16 Antarctic Sea during JARE43 observation in 2002.<br />

16-1 Distribution of Methane along 140E.<br />

16-2 Distribution of SiO 2 along 140E.<br />

16-3 Distribution of DMS along 140E.<br />

Ocean Data View<br />

Ocean Data View<br />

Ocean Data View<br />

4.5<br />

4<br />

3.5<br />

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2.5<br />

2<br />

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1<br />

150<br />

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75<br />

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25<br />

0<br />

15<br />

12.5<br />

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7.5<br />

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2.5<br />

0<br />

43

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