Abstract. Over the past several decades, jellyfish blooms have
intensified spatially and temporally, affecting functions and services of
ecosystems worldwide. At the demise of a bloom, an enormous amount of
jellyfish biomass sinks to the seabed and decomposes. This process entails
reciprocal microbial and biogeochemical changes, typically enriching the
water column and seabed with large amounts of organic and inorganic
nutrients. Jellyfish decomposition was hypothesized to be particularly
important in nutrient-impoverished ecosystems, such as the Eastern
Mediterranean Sea – one of the most oligotrophic marine regions in the
world. Since the 1970s, this region has been experiencing the proliferation of a
notorious invasive scyphozoan jellyfish, Rhopilema nomadica. In this study, we estimated the
short-term decomposition effects of R. nomadica on nutrient dynamics at the
sediment–water interface. Our results show that the degradation of R. nomadica has led
to increased oxygen demand and acidification of overlying water as well as
high rates of dissolved organic nitrogen and phosphate production. These
conditions favored heterotrophic microbial activity and bacterial biomass
accumulation, and triggered a shift towards heterotrophic biodegrading
bacterial communities, whereas autotrophic picophytoplankton abundance was
moderately affected or reduced. This shift may further decrease primary
production in the water column of the Eastern Mediterranean Sea.
Deoxygenation, acidification, nutrient enrichment, and microbial community
shifts at the sediment–water interface may have a detrimental impact on
macrobenthic communities. Based on these findings, we suggest that
jelly-falls and their decay may facilitate an additional decline in
ecosystem functions and services.