The effects of PAH contamination and grazing on the abundance and composition of microphytobenthos in salt marsh sediments (Pass Fourchon, LA, USA): II: The use of plant pigments as biomarkers
A. Bennett et al., The effects of PAH contamination and grazing on the abundance and composition of microphytobenthos in salt marsh sediments (Pass Fourchon, LA, USA): II: The use of plant pigments as biomarkers, EST COAST S, 50(3), 2000, pp. 425-439
A field study was conducted in 1996 and 1997 that examined effects of tempo
ral and spatial variability of polycyclic aromatic hydrocarbons (PAHs), mac
ro-epifaunal abundance, and dissolved inorganic nutrients on the abundance
and composition of microphytobenthos in salt marsh sediments in Pass Fourch
on, LA (U.S.A.). Plans pigment biomarkers were used to monitor seasonal pat
terns in benthic microalgal abundance and composition across a PAH contamin
ation gradient created by past produced-wafer pumping. The microphytobenthi
c community at Pass Fourchon was primarily composed of diatoms and cyanobac
teria, as indicated by the carotenoid biomarkers fucoxanthin and zeaxanthin
, respectively. Microphytobenthic abundance showed no consistent pattern of
variation across stations or seasons; chlorophyll a concentrations general
ly ranged from 0.2 to 15.9 mu g g dry sediment(-1). Significantly higher co
ncentrations of dissolved inorganic nitrogen (DIN) were observed in porewat
ers at the highly contaminated (high PAHs) station; ammonium had the highes
t range (160 to 8500 mu M at Station la). Higher DIN concentrations were li
kely due to rapid remineralization of microphytobenthic detritus at the hig
hly contaminated station. Microphytobenthic response to enhanced DIN availa
bility was likely hindered by PAH toxicity and/or macro- and meiobenthic gr
azing effects. In September of each study year, significant seasonal increa
ses in total PAH concentration in surface sediments were observed at the co
ntaminated sire (Station 1a). Examination of PAH isomer ratios indicates th
is seasonal pattern was likely due to physical mixing events (i.e. storms)
and not to changes in PAH inputs or preferential remineralization of certai
n PAHs. (C) 2000 Academic Press.