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3 Methaogenic Microbial Communities Asociated with Aquatic Plants 39<br />

Fig. 2. Transfer of carbon via rice<br />

<strong>plant</strong>s to the soil and into CH 4 .<br />

Above After pulse labeling of the<br />

rice <strong>plant</strong>s with 14 CO 2 , radioactivity<br />

transiently accumulates in soil<br />

organic compounds and is ultimately<br />

converted to 14 CH 4 ; below<br />

specific radioactivities indicate<br />

that radioactive compounds are<br />

converted in the sequence lactate>propionate>acetate>CH<br />

4<br />

(taken from Dannenberg and Conrad<br />

1999)<br />

Radioactivity [Bq ml -1 ]<br />

Specific radioactivity [Bq nmol -1 ]<br />

500<br />

400<br />

300<br />

200<br />

100<br />

Experiment #1<br />

lactate<br />

propionate<br />

acetate<br />

CH 4<br />

0<br />

0 2 4 6 8 10 12 14 16<br />

Time [d]<br />

0<br />

0 2 4 6<br />

Besides the more direct effect of photosynthesis through root exudation,<br />

CH 4 production in wetlands is furthermore stimulated by <strong>plant</strong> debris. This<br />

may be decaying roots or dead aboveground <strong>plant</strong> material. In rice fields, for<br />

example, rice straw from the previous season is often plowed under to<br />

improve soil quality. Also, composted <strong>plant</strong> material is used as soil fertilizer.<br />

There are numerous studies which show that addition of such organic matter<br />

dramatically increases CH 4 emission rates (Denier van der Gon 1999).<br />

Decomposition of isotopically labeled rice straw contributes significantly to<br />

production and emission of CH 4 during the early season (Chidthaisong and<br />

Watanabe 1997; Watanabe et al. 1998, 1999)<br />

8<br />

7<br />

6<br />

5<br />

4<br />

3<br />

2<br />

1<br />

Time [d]<br />

A<br />

lactate<br />

propionate<br />

acetate<br />

CO 2<br />

CH 4<br />

B

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