In 1831 Hemprich and Ehrenberg described the colonial ciliate Zoothamnium niveum. More than 150 years later Jörg Ott found a very large ciliate in the mangroves of the Belize. The white color turned out to be a coat of sulfur bacteria.
During two post-doctoral positions at the University of Tübingen, Germany and the Rosenstiel School of Marine and Atmospheric Science, University of Miami, funded by an FWF Erwin Schrödinger-Postdoctoral Fellowship and an Emil-Boral-Postdoctoral Fellowship between 1993-1995 we re-described the host species, for which I got awarded the John O. Corliss Ciliate Systematics Award in 1997.
In the FWF project "Life cycle and interactions of a thiotrophic symbiosis" (2003-2007), we characterized the symbiont Candidatus Thiobius zoothamnicola.
Most importantly, Christian Rinke was able to cultivate the ciliate. This is, to our knowledge, still the only thiotrophic symbioses that can be cultured over several host generations. We developed tiny flow-through aquaria to keep oxygen and hydrogen sulfide concentrations stable. Highest growth rates were found under oxic conditions supplemented with low sulfide concentrations. Interestingly, the host also grew without sulfide but reached only small sizes.
At that time, we did not understand how important this finding was.
In the next FWF project “Thiotrophic mutualism – cooperation goes empirical” (2012-2016) we relocated our field research to the Marine Biology Station in Piran. We are very grateful for their hospitality and continuous support.
We finally unraveled why this ciliate did not die under oxic conditions. We discovered a spectacular polyphenism – two distinct phenotypic growth forms in the ciliate, a symbiotic one and an aposymbiotic one. We showed in a suite of experiments that polyphenism in this mutualism is triggered by chemical conditions and induced by the symbiont’s presence on the dispersing swarmer.
In a follow-up study we exposed the colonies to oxic seawater mimicking waning of sulfide to study the fate of both partners. We found that colonies released some initially present but also newly produced macrozooids until death, but in fewer numbers than when exposed to sulfide. Below you see the mortality of colonies (left) and swarmers (right) with and without sulfide. The symbionts on the colonies proliferated less without sulfide, and became larger and more rod-shaped than symbionts from freshly collected colonies that were exposed to sulfide and oxygen. The symbiotic monolayer was severely disturbed by growth of other microbes and loss of symbionts. We conclude that the response of both partners to the termination of sulfide emission was remarkably quick. The development and the release of swarmers continued until host died and thus this behavior contributed to the continuation of the association.
We investigated this nutritional relationship in pulse-chase experiments using 14C bicarbonate tissue autoradiography, 13C bicarbonate NanoSIMS and correlative TEM. We found that this facultative host is milking and farming the symbiont. Nourishment is accomplished by uptake of released fixed organic carbon from the symbiont but also through digestion of symbionts and a few free-living microbes.
In our current FWF project “Environmental impact on giant ciliate mutualism” (2019-2023) we aim to unravel the mechanisms that have evolved in this mutualism to deal with the notoriously instable environment over short, annual, and longtime scales.