Masashi Tsuchiya

Algivore or phototroph? Plakobranchus ocellatus (Gastropoda) continuously acquires kleptoplasts and nutrition from multiple algal species in nature.

The sea slug Plakobranchus ocellatus (Sacoglossa, Gastropoda) retains photosynthetically active chloroplasts from ingested algae (functional kleptoplasts) in the epithelial cells of its digestive gland for up to 10 months. While its feeding behavior has not been observed in natural habitats, two hypotheses have been proposed: 1) adult P. ocellatus uses kleptoplasts to obtain photosynthates and nutritionally behaves as a photoautotroph without replenishing the kleptoplasts; or 2) it behaves as a mixotroph (photoautotroph and herbivorous consumer) and replenishes kleptoplasts continually or periodically. To address the question of which hypothesis is more likely, we examined the source algae for kleptoplasts and temporal changes in kleptoplast composition and nutritional contribution. By characterizing the temporal diversity of P. ocellatus kleptoplasts using rbcL sequences, we found that P. ocellatus harvests kleptoplasts from at least 8 different siphonous green algal species, that kleptoplasts from more than one species are present in each individual sea slug, and that the kleptoplast composition differs temporally. These results suggest that wild P. ocellatus often feed on multiple species of siphonous algae from which they continually obtain fresh chloroplasts. By estimating the trophic position of wild and starved P. ocellatus using the stable nitrogen isotopic composition of amino acids, we showed that despite the abundance of kleptoplasts, their photosynthates do not contribute greatly to the nutrition of wild P. ocellatus, but that kleptoplast photosynthates form a significant source of nutrition for starved sea slugs. The herbivorous nature of wild P. ocellatus is consistent with insights from molecular analyses indicating that kleptoplasts are frequently replenished from ingested algae, leading to the conclusion that natural populations of P. ocellatus do not rely on photosynthesis but mainly on the digestion of ingested algae.

Cytologic and Genetic Characteristics of Endobiotic Bacteria and Kleptoplasts of Virgulinella fragilis (Foraminifera)

The benthic foraminifer Virgulinella fragilis Grindell and Collen 1976 has multiple putative symbioses with both bacterial and kleptoplast endobionts, possibly aiding its survival in environments from dysoxia (5–45 μmol‐O2/L) to microxia (0–5 μmol‐O2/L) and in the dark. To clarify the origin and function of V. fragilis endobionts, we used genetic analyses and transmission electron microscope observations. Virgulinella fragilis retained δ‐proteobacteria concentrated at its cell periphery just beneath the cell membranes. Unlike another foraminifer Stainforthia spp., which retains many bacterial species, V. fragilis has a less variable bacterial community. This suggests that V. fragilis maintains a specific intracellular bacterial flora. Unlike the endobiotic bacteria, V. fragilis klepto‐plasts originated from various diatom species and are found in the interior cytoplasm. We found evidence of both retention and digestion of kleptoplasts, and of fragmentation of the kleptoplastid outer membrane that likely facilitates transport of kleptoplastid products to the host. Accumulations of mitochondria were observed encircling endobiotic bacteria. It is likely that the bacteria use host organic material for carbon oxidation. The mitochondria may use oxygen available around the δ‐proteobacteria and synthesize adenosine triphosphate, perhaps for sulfide oxidation.

Proton pumping accompanies calcification in foraminifera

Ongoing ocean acidification is widely reported to reduce the ability of calcifying marine organisms to produce their shells and skeletons. Whereas increased dissolution due to acidification is a largely inorganic process, strong organismal control over biomineralization influences calcification and hence complicates predicting the response of marine calcifyers. Here we show that calcification is driven by rapid transformation of bicarbonate into carbonate inside the cytoplasm, achieved by active outward proton pumping. Moreover, this proton flux is maintained over a wide range of pCO2 levels. We furthermore show that a V-type H+ ATPase is responsible for the proton flux and thereby calcification. External transformation of bicarbonate into CO2 due to the proton pumping implies that biomineralization does not rely on availability of carbonate ions, but total dissolved CO2 may not reduce calcification, thereby potentially maintaining the current global marine carbonate production.

Intracellular Isotope Localization in Ammonia sp. (Foraminifera) of Oxygen-Depleted Environments: Results of Nitrate and Sulfate Labeling Experiments

Some benthic foraminiferal species are reportedly capable of nitrate storage and denitrification, however, little is known about nitrate incorporation and subsequent utilization of nitrate within their cell. In this study, we investigated where and how much 15N or 34S were assimilated into foraminiferal cells or possible endobionts after incubation with isotopically labeled nitrate and sulfate in dysoxic or anoxic conditions. After 2 weeks of incubation, foraminiferal specimens were fixed and prepared for Transmission Electron Microscopy (TEM) and correlative nanometer-scale secondary ion mass spectrometry (NanoSIMS) analyses. TEM observations revealed that there were characteristic ultrastructural features typically near the cell periphery in the youngest two or three chambers of the foraminifera exposed to anoxic conditions. These structures, which are electron dense and ~200–500 nm in diameter and co-occurred with possible endobionts, were labeled with 15N originated from 15N-labeled nitrate under anoxia and were labeled with both 15N and 34S under dysoxia. The labeling with 15N was more apparent in specimens from the dysoxic incubation, suggesting higher foraminiferal activity or increased availability of the label during exposure to oxygen depletion than to anoxia. Our results suggest that the electron dense bodies in Ammonia sp. play a significant role in nitrate incorporation and/or subsequent nitrogen assimilation during exposure to dysoxic to anoxic conditions.

Active Bacterial Flora Surrounding Foraminifera (Xenophyophorea) Living on the Deep-Sea Floor

Bacteria form unique ecosystems by coexisting with large organisms. Here we present the first evidence of active flora surrounding xenophyophorea revealed through clone analyses of environmental ribosomal RNA gene sequences. The flora included eight phyla in the xenophyophorean cells with agglutinated test. The major operational taxonomic units were unique from that in the near-surface sediment. This flora appears to be formed by coexistence with xenophyophores.

Evolution of elongation factor-like (EFL) protein in Rhizaria is revised by radiolarian EFL gene sequences.

Elongation factor 1α (EF‐1α) and elongation factor‐like (EFL) proteins are considered to carry out equivalent functions in translation in eukaryotic cells. Elongation factor 1α and EFL genes are patchily distributed in the global eukaryotic tree, suggesting that the evolution of these elongation factors cannot be reconciled without multiple lateral gene transfer and/or ancestral co‐occurrence followed by differential loss of either of the two factors. Our current understanding of the EF‐1α/EFL evolution in the eukaryotic group Rhizaria, composed of Foraminifera, Radiolaria, Filosa, and Endomyxa, remains insufficient, as no information on EF‐1α/EFL gene is available for any members of Radiolaria. In this study, EFL genes were experimentally isolated from four polycystine radiolarians (i.e. Dictyocoryne, Eucyrtidium, Collozoum, and Sphaerozoum), as well as retrieved from publicly accessible expressed sequence tag data of two acantharean radiolarians (i.e. Astrolonche and Phyllostaurus) and the endomyxan Gromia. The EFL homologs from radiolarians, foraminiferans, and Gromia formed a robust clade in both maximum‐likelihood and Bayesian phylogenetic analyses, suggesting that EFL genes were vertically inherited from their common ancestor. We propose an updated model for EF‐1α/EFL evolution in Rhizaria by incorporating new EFL data obtained in this study.

How Has Foraminiferal Genetic Diversity Developed? A Case Study of Planoglabratella opercularis and the Species Concept Inferred from Its Ecology, Distribution, Genetics, and Breeding Behavior

The nature of Planoglabratella opercularis has been revealed through multidisciplinary studies focusing on its ecology, life cycle, growth rate, interbreeding, morphology, natural abundance, distribution, and molecular ecology. Our research is aimed at revealing the processes and mechanisms behind foraminiferal evolution. P. opercularis is a benthic inhabitant of rocky-shore environments, where it crawls on coralline algae. Gametes are not released into the ambient seawater; rather this species forms plastogamic pairs and exchanges gametes inside the shell. Thus, the mobility and dispersal of both individuals and gametes are extremely low. In fact, genetic divergence has likely occurred within each geographic population. Interpopulational breeding experiments revealed breeding incompatibility between gamont specimens from widely separated local populations. The genetic connectivity in P. opercularis is affected by ecological characteristics such as habitat and mobility. Molecular ecological studies have revealed that P. opercularis likely diversified through reproductive isolation resulting from geographical separation following changes in land–ocean distributions.

Compound-specific isotope analysis of benthic foraminifer amino acids suggests microhabitat variability in rocky-shore environments

Abstract The abundance and biomass of benthic foraminifera are high in intertidal rocky‐shore habitats. However, the availability of food to support their high biomass has been poorly studied in these habitats compared to those at seafloor covered by sediments. Previous field and laboratory observations have suggested that there is diversity in the food preferences and modes of life among rocky‐shore benthic foraminifera. In this study, we used the stable nitrogen isotopic composition of amino acids to estimate the trophic position, trophic niche, and feeding strategy of individual foraminifera species. We also characterized the configuration and structure of the endobiotic microalgae in foraminifera using transmission electron microscopy, and we identified the origin of endobionts based on nucleotide sequences. Our results demonstrated a large variation in the trophic positions of different foraminifera from the same habitat, a reflection of endobiotic features and the different modes of life and food preferences of the foraminifera. Foraminifera did not rely solely on exogenous food sources. Some species effectively used organic matter derived from endobionts in the cell cytoplasm. The high biomass and species density of benthic foraminifera found in intertidal rocky‐shore habitats are thus probably maintained by the use of multiple nitrogen resources and by microhabitat segregation among species as a consequence.

A new method for acquiring images of meiobenthic images using the FlowCAM

Graphical abstract