Mi. Scranton et al., NOCTURNAL METHANE ACCUMULATION IN THE PYCNOCLINE OF AN ANOXIC ESTUARINE BASIN, Limnology and oceanography, 40(4), 1995, pp. 666-672
Diel studies of vertical methane distributions were made on seven date
s during five field expeditions over a period of 3 yr to the permanent
ly anoxic southern basin of the Pettaquamscutt River estuary. On five
occasions, methane concentrations were constant over a diel cycle, ind
icating balanced production and consumption. On two other occasions, m
ethane concentrations varied dramatically between sunset and sunrise,
increasing (and then decreasing) by up to several mu moles per liter b
etween sunset and sunrise in the chlorophyll-rich pycnocline. Our obse
rvations on these two dates require a nocturnal imbalance between meth
ane production and methane oxidation. Data from 1992 suggest that prod
uction exceeds oxidation in the early part of the evening and that oxi
dation exceeds production after around midnight. On other dates, produ
ction and consumption are balanced, although turnover rates could stil
l be high. Methane concentration variations that occurred nocturnally
did not seem to be associated with tidal or advective effects, as comp
arisons were made on density horizons, and very little lateral variabi
lity in methane concentrations was found along a longitudinal transect
of the basin. Methane profiles taken during the day were essentially
identical during each 2-week experiment. In all cases, methane concent
rations in the surface waters above the pycnocline were similar to 0.1
-0.2 mu M and remained constant over the sampling period.