Paper No. 7
Presentation Time: 9:45 AM
FORAMINIFERA IN EXTREME ENVIRONMENTS: HOW BENTHIC POPULATIONS RESPOND TO EXPOSURE TO HIGH-[AS], LOW-PH HYDROTHERMAL VENT FLUIDS IN PAPUA NEW GUINEA
MCCLOSKEY, Bryan James1, HALLOCK, Pamela
1, PRICE, Roy
2 and PICHLER, Thomas
2, (1)College of Marine Science, University of South Florida, 140 7th Ave. S, St. Petersburg, FL 33701, (2)Geology, Univ of South Florida, Tampa, FL 33620, bryanm@marine.usf.edu
Several
shallow-water
hydrothermal vents discharge into Tutum
Bay, Ambitle
Island, northeastern Papua
New Guinea. Vent waters feature some
of the
world’s highest naturally-occurring arsenic concentrations ([As]) – up
to
11.8µmol/L, or almost 800X higher than normal seawater. Discharge
by the vents
has been estimated at >1500g As/day into an area approximately 5000m2
with an average depth of 6m. This As is mitigated by mixing with
seawater and
removal of As by incorporation into As-containing iron-oxyhydroxide
precipitates, which form as crusts when hydrothermal fluids mix with
seawater;
crusts contain up to 76,000ppm As. Consequently, [As] are considerably
higher
near vent sites, in porewaters, and near the sediment/water interface,
than in
overlying seawater. Despite the high [As], the biota of the bay does
not show
an obvious severely adverse response; healthy-appearing hard and soft
coral and
fishes abound. The effects on benthic foraminiferal populations,
however, are
more complicated. Benthic foraminifera live in close proximity to pore
waters and
in intimate association with As-rich sediments. The relatively small
sizes of the
foraminifers, their high surface-to-volume ratios, which promotes
diffusive
processes, and the extension of their reticulopodia into high As
microenvironments, all may amplify their exposure. In addition, As ions
may be
incorporated into calcite tests and As-laden sediment grains may be
used by
agglutinated taxa. Foraminiferal abundance and diversity increase with
distance
from the vents, as [As] decrease and porewater pH increases. A sharp
transition
zone between very low abundance and higher, more normal abundance
occurs
140-150m from the vents, defining zones of higher and lower
hydrothermal
influence. Laboratory experiments show that foraminifers are adversely
affected
by [As5+] of 1000ppb and [As3+] of 200ppb, and
that
growth rate and reproduction are also affected by As exposure. The
hydrothermal
system at Tutum Bay
provides an ideal opportunity to examine the effects of arsenic, a
toxin with
implications for human and environmental health, in an environment that
is
minimally impacted by human activities. Furthermore, by examining these
effects
on Foraminifera, we are observing organisms with general utility as
bioindicators of environmental health.