Cj. Gobler et al., RELEASE AND BIOAVAILABILITY OF C, N, P, SE, AND FE FOLLOWING VIRAL LYSIS OF A MARINE CHRYSOPHYTE, Limnology and oceanography, 42(7), 1997, pp. 1492-1504
The potential importance of the viral lysis of phytoplankton for nutri
ent and carbon cycling has been acknowledged, but no quantitative asse
ssments of this phenomenon exist. Radiotracer experiments examined the
release and bioavailability of C, N, P, Fe, and Se following viral ly
sis of the ''brown tide'' chrysophyte Aureococcus anophagefferens. Pho
tochemical effects on the dissolved-particulate partitioning and biolo
gical uptake of virally released elements were also investigated. Vira
l lysis of A. anophagefferens released 50% mon C and Se than uninfecte
d control cells to the dissolved phase, while N, P, and Fe remained in
the particulate phase. There was a significant inverse correlation be
tween A. anophagefferens and bacterial densities, as well as an increa
se in particulate organic nitrogen levels in cultures during viral lys
is. These observations indicate that released dissolved organic matter
supported bacterial growth and may be a pathway by which various elem
ents are diverted in microbial food webs. Dissolved nutrients released
by viral lysis were accumulated to varying degrees by natural assembl
ages of marine bacteria and cultured diatoms, and vitally regenerated
N and P relieved diatom nutrient limitation. During a 4-wk incubation,
80% of C and P within cell lysis debris was released to the dissolved
phase, likely due to bacterial activity. Photochemical degradation of
cell lysis debris enhanced dissolved levels of Se (100%) and Fe (50%)
and reduced total dissolved C by 15%. Photochemistry doubled the bioa
vailability of virally released Se to diatoms, while decreasing the bi
oavailability of C to bacteria threefold. The viral lysis of an A. ano
phagefferens bloom in the field could release 40 mu M dissolved organi
c carbon and rapidly transfer other released elements to bacteria. Suc
h occurrences may significantly affect water column chemistry, species
composition, and succession within marine plankton communities.