At 10°C tubificids increased the redox potential of profundal lake sediment at 1–4‐cm depth, with greatest average increases (294 and 241 mV) at 2 and 3 cm. The oxidized layer (> 200 mV) was deepened 0.3–1.6 cm. pH was decreased slightly in the upper 1–2 cm and below this was increased to depths > 14 cm.
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Ronald B. Davis (1974) studied this question.
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