TY - JOUR
T1 - Ontogenetic dynamics of photosymbiosis in cultured planktic foraminifers revealed by fast repetition rate fluorometry
AU - Takagi, Haruka
AU - Kimoto, Katsunori
AU - Fujiki, Tetsuichi
AU - Kurasawa, Atsushi
AU - Moriya, Kazuyoshi
AU - Hirano, Hiromichi
N1 - Funding Information:
We thank A. Matsuoka for his help with the collection of foraminifers and for useful discussion, M. Enoki for nutrient analyses, and Y. Mino and T. Yuasa for support and advice concerning the experiment. We thank the staffs of the Sesoko Station, Tropical Biosphere Research Center, University of the Ryukyus for their support and for the use of their laboratory facilities. We greatly appreciate the Editor R.W. Jordan, P. Hallock, and an anonymous reviewer for constructive comments that improved our manuscript. We also appreciate development teams of R and GMT software. This study was funded by Japan Society for Promotion of Science KAKENHI Grants ( 13J05477 to H. Takagi and 25740014 to T. Fujiki).
Publisher Copyright:
© 2015 Elsevier B.V.
Copyright:
Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2016/1/1
Y1 - 2016/1/1
N2 - Photosymbiosis is an important ecological strategy that allows the host to thrive in oligotrophic environments, and the photosymbiosis of planktic foraminifers is no exception. Here, we present ontogenetic information about the photosymbiosis of planktic foraminifers that we obtained via analyses of the chlorophyll fluorescence [fast repetition rate (FRR) fluorometry] of symbiotic algae within the host. We cultured two symbiont-bearing planktic foraminifers (Globigerinoides sacculifer and Globigerinella siphonifera Type II) until their natural death, and conducted FRR measurements on individual host-algal consortia through the culture study. Time-series FRR analyses revealed no clear temporal trend in photophysiology but did reveale species specificity. The light-absorption efficiency of the photosynthetic system was significantly higher in Gn. siphonifera than in Gs. sacculifer indicating higher potential to acclimate to low-light environment for Gn. siphonifera. In contrast to the physiology, the chlorophyll a content of foraminifer, a metric of the quantity of symbionts, showed conspicuous ontogenetic changes; the chlorophyll a content, initially less than 30 ng, reached a maximum of more than 140 ng, then it was all digested or lysed at the end of the host's ontogeny. The changes of symbiont biomass and relatively invariant photophysiology indicate dynamic rise and fall of potential photosynthesis of symbiont population during the host's life processes, not just the progressive increase of photosynthesis. Because photosynthesis of symbionts can alter the geochemical composition of the foraminiferal calcifying microenvironment, our results will also contribute to better understanding of the effect of photosynthesis on the foraminiferal tests that are important for paleoecological and paleoceanographic works.
AB - Photosymbiosis is an important ecological strategy that allows the host to thrive in oligotrophic environments, and the photosymbiosis of planktic foraminifers is no exception. Here, we present ontogenetic information about the photosymbiosis of planktic foraminifers that we obtained via analyses of the chlorophyll fluorescence [fast repetition rate (FRR) fluorometry] of symbiotic algae within the host. We cultured two symbiont-bearing planktic foraminifers (Globigerinoides sacculifer and Globigerinella siphonifera Type II) until their natural death, and conducted FRR measurements on individual host-algal consortia through the culture study. Time-series FRR analyses revealed no clear temporal trend in photophysiology but did reveale species specificity. The light-absorption efficiency of the photosynthetic system was significantly higher in Gn. siphonifera than in Gs. sacculifer indicating higher potential to acclimate to low-light environment for Gn. siphonifera. In contrast to the physiology, the chlorophyll a content of foraminifer, a metric of the quantity of symbionts, showed conspicuous ontogenetic changes; the chlorophyll a content, initially less than 30 ng, reached a maximum of more than 140 ng, then it was all digested or lysed at the end of the host's ontogeny. The changes of symbiont biomass and relatively invariant photophysiology indicate dynamic rise and fall of potential photosynthesis of symbiont population during the host's life processes, not just the progressive increase of photosynthesis. Because photosynthesis of symbionts can alter the geochemical composition of the foraminiferal calcifying microenvironment, our results will also contribute to better understanding of the effect of photosynthesis on the foraminiferal tests that are important for paleoecological and paleoceanographic works.
KW - Culture
KW - Fast repetition rate fluorometry
KW - Ontogeny
KW - Photophysiology
KW - Photosymbiosis
KW - Planktic foraminifers
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U2 - 10.1016/j.marmicro.2015.10.003
DO - 10.1016/j.marmicro.2015.10.003
M3 - Article
AN - SCOPUS:84947791684
SN - 0377-8398
VL - 122
SP - 44
EP - 52
JO - Marine Micropaleontology
JF - Marine Micropaleontology
ER -