Abstract. Photosynthetically active foraminifera are prolific carbonate
producers in warm, sunlit, surface waters of the oceans. Foraminifera have
repeatedly developed mixotrophic strategies (i.e., the ability of an
organism or holobiont to both feed and photosynthesize) by facultative or
obligate endosymbiosis with microalgae or by sequestering plastids
(kleptoplasts) of ingested algae. Mixotrophy provides access to essential
nutrients (e.g., N, P) through feeding while providing carbohydrates and
lipids produced through photosynthesis, resulting in substantial energetic
advantage in warm, sunlit environments where food and dissolved nutrients
are scarce. Our morphological as well as stable carbon isotope data provide,
as of now, the earliest (Mid-Devonian) evidence for photosynthetic activity
in the first advanced, multichambered, calcareous foraminifera,
Semitextularia, from the tropical shelf of the Laurussia paleocontinent. This adaptation
likely influenced the evolutionary radiation of calcareous Foraminifera in
the Devonian (“Givetian revolution”), one of the most important
evolutionary events in foraminiferal history, that coincided with the
worldwide development of diverse calcifying marine communities inhabiting
shelf environments linked with Devonian stromatoporoid coral reefs.