Abstract. Foraminiferans are diverse micro- to macroscopic protists
abundant especially in (sub)tropical seas, often forming characteristic
benthic communities known as “living sands”. Numerous species have
migrated through the Suez Canal to the Mediterranean and one of them, i.e.,
Amphistegina lobifera, turned invasive, gradually outcompeting the indigenous species. At some
places, A. lobifera creates thick seabed sediments, thus becoming an important
environmental engineer. However, little is known about the turnover of its
shells in the invaded ecosystems. Using vital staining, stereomicroscopy,
scanning electron microscopy, and cultivation and DNA fingerprinting, I
investigated the vital status, destruction/decomposition and mycobiota of
A. lobifera in the rhizosphere of the dominant Mediterranean seagrass Posidonia oceanica in an underwater
Maltese meadow (average 284 shells g−1, representing 28.5 % of dry substrate
weight), in comparison with epiphytic specimens and P. oceanica roots. While 78 % of
the epiphytes were alive, nearly all substrate specimens were dead. On
average, 80 % of the epiphytes were intact compared to 21 % of the
substrate specimens. Abiotic dissolution and mechanical damage played only a minor role, but some bioerosion was detected in 18 % and >70 % of the epiphytic and substrate specimens, respectively. Few
bioerosion traces could be attributed to fungi, and the majority probably
belonged to photoautotrophs. The seagrass roots displayed fungal
colonization typical for this species and yielded 81 identified isolates,
while the surface-sterilized substrate specimens surprisingly yielded no
cultivable fungi compared to 16 other identified isolates obtained from the
epiphytes. While the epiphytes' mycobiota was dominated by
ascomycetous generalists also known from terrestrial ecosystems (alongside
with, for example, a relative of the “rock-eating” extremophiles), the roots were
dominated by the seagrass-specific dark septate endophyte Posidoniomyces atricolor and additionally
contained a previously unreported lulworthioid mycobiont. In conclusion, at
the investigated locality, dead A. lobifera shells seem to be regularly bioeroded by endolithic non-fungal organisms, which may counterbalance their accumulation in the seabed substrate.