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Evidence for Rhythmicity Pacemaker in the Calcification Process of Scleractinian Coral

  • Scientific Reports 6, Article number: 20191 (2016)
  • doi:10.1038/srep20191
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Abstract

Reef-building scleractinian (stony) corals are among the most efficient bio-mineralizing organisms in nature. The calcification rate of scleractinian corals oscillates under ambient light conditions, with a cyclic, diurnal pattern. A fundamental question is whether this cyclic pattern is controlled by exogenous signals or by an endogenous ‘biological-clock’ mechanism, or both. To address this problem, we have studied calcification patterns of the Red Sea scleractinian coral Acropora eurystoma with frequent measurements of total alkalinity (AT) under different light conditions. Additionally, skeletal extension and ultra-structure of newly deposited calcium carbonate were elucidated with 86Sr isotope labeling analysis, combined with NanoSIMS ion microprobe and scanning electron microscope imaging. Our results show that the calcification process persists with its cyclic pattern under constant light conditions while dissolution takes place within one day of constant dark conditions, indicating that an intrinsic, light-entrained mechanism may be involved in controlling the calcification process in photosymbiotic corals.

Introduction

In the marine environment, diel periodicity is mainly governed by light and dark cycles and by tidal cues1 that synchronize a multitude of biological processes in aquatic organisms. Basal metazoan organisms, such as scleractinian corals, offer insights into the origins of the circadian machinery that regulates temporal patterns throughout the animal kingdom. In addition, scleractinian corals are among the most efficient bio-mineralizing organisms in nature, forming vast coral reefs in the shallow waters of the tropical and sub-tropical oceans2. Reef-building corals are furthermore interesting for their symbiosis with dinoflagellates of the genus Symbiodinium sp. (commonly named zooxanthellae), that drive major diurnal changes in their tissue, via their influence on oxygen tension, pH, nutrient fluxes, and other variables3,4,5,6,7. Although there are strong indications of rhythmic behavior in corals8,9, very little is known about the circadian clock mechanisms that control the biology of these symbiotic organisms. Recently, molecular and physiological studies have demonstrated that circadian mechanisms are involved in the control of the host metabolism10,11 and the symbionts photosynthesis12,13,14.

Studies of abiotic impacts on the coral calcification process have focused mainly on seawater temperature15,16,17, carbonate saturation state18,19,20,21, and light22,23,24,25. However, the tuning of the process is not clear. The calcification process is generally linked to the day-night cycle, with higher calcification rates observed during the daytime (so-called Light-Enhanced Calcification26,27,28), although this is still a matter of some debate29. A few studies have suggested that the daily rate of calcification is regulated by an intrinsic rhythm30,31, without specifying the possible mechanism.

The circadian clock is an endogenous chronometer found in most eukaryotes and in photosynthetic bacteria24. The clock drives rhythms that regulate the physiology, biochemistry, and metabolism of the organism25, and is coupled to the environment via synchronizing cues, or zeitgebers (time-givers), such as light and temperature cycles. These environmental cycles allow organisms to maintain robust rhythms with a 24 hours periodicity over a broad range of physiological, temperature, and light regimes26. Circadian rhythms are generally considered to be free running, maintaining a periodicity of ≈24 hours for some time under constant stimuli or in the absence of external diel cues; for example in constant light, constant darkness, or constant temperature. In order to understand if the calcification process in corals is controlled by an endogenous pacemaker, synchronized primarily with light intensity, a series of 48 h experiments were conducted with the coral Acropora eurystoma (Fig. 1) under four light regimes: 1) constant light (LL), two 24 h periodic light regimes consisting of 2) the ambient natural cycle and 3) 10 h/14 h light /dark (LD), and 4) constant darkness (DD). During these different light treatments the calcification rates of the corals were measured. In addition, repeated in-situ86Sr-isotope labeling was performed under the various experimental conditions to assess if mentioned light treatments affect the skeletal extension and skeletal ultrastructures.

Figure 1: Apical branch fragments of Acropora eurystoma.
Figure 1

Results

Relative calcification cycles

The measurements of relative variations in total alkalinity (AT) during successive two-hour incubation periods show that the tropical symbiotic coral A. eurystoma maintained a cyclic and rhythmic pattern of calcification under all light regimes tested (Ambient, LD and LL), with dissolution during night-time and throughout DD (Fig. 2). The rhythmic pattern of calcification cycle under LD treatment (Fig. 2b) was similar to the calcification pattern under ambient light, showing significant maximum during the midday hours in both light periods (repeated measures ANOVA followed by Bonferroni test, F(11, 33) = 521.878, p < 0.005 and F(11, 33) = 163.854, p < 0.0005 for ambient and LD treatments, respectively). This result is in spite of the fact that the artificial light had a constant irradiance and during LD runs light was switched on and off instantaneously compared to gradual irradiance change in nature.

Figure 2: Relative calcification cycle of Acropora eurystoma under different light treatments over 48 hours, negative values represent dissolution.
Figure 2

(a) Ambient natural light (AMB). (b) Light/dark (LD). (c) Constant light (LL). (d) Constant darkness (DD). Asterisks denote significant differences from other time-point measurements within the same treatment, repeated measures ANOVA, with Bonferroni test (P < 0.05). Error bars represent standard error.

The calcification cycle under LL conditions (Fig. 2c) showed a rhythmic calcification pattern with a free run period close to a 24 hours cycle. During the subjective night-time, relative calcification values were low and approached dissolution. The significant calcification maxima occurred at 12:00 (midday) on the first day under LL while on the subsequent day, maximum calcification was observed between 12:00 to 20:00 (repeated measures ANOVA followed by Bonferroni test, F(11, 44) = 24.24, p < 0.005). Calcification of coral fragments kept under the LL treatment increased at the beginning of the second day in the subjective second dawn. In the second subjective night, relative calcification values did not decrease, as they did for ambient and LD (second time-point 20:00), but dropped later in the next measurement time at 0:00 (second subjective midnight). In the third morning, the calcification of the coral fragments kept in the LL treatment rose significantly more than those kept in ambient and LD. Although under LL treatment in the second 24 hours a prolonged calcification pattern was observed, no difference was identified in the overall calcification pattern in the first 24 hours, between the three light treatments (ambient, LD and LL). During DD, only net dissolution was observed and the relative dissolution values were significantly different only between the peak of dissolution on the second day (20:00) and minimum dissolution at midnight (00:00) and midday of the second day (repeated measures ANOVA followed Bonferroni test, F(11, 22) = 7.675, p < 0.005).

Dynamics of skeletal extension visualized by 86Sr label incorporation

Successive growth fronts labeled with 86Sr were visualized with NanoSIMS ion microprobe imaging in sections of skeleton of coral nubbins (Fig. 3). Corals grown under the ambient LD photoperiod (Fig. 3a–c) or under the LD and LL light treatments (Fig. 3d–f) typically exhibited all five 86Sr bands. The labeled growth fronts passed mostly through the Thickening Deposits (TD), which represent the bulk of the skeleton, and sometimes through the Rapid Accretion Deposits (RAD), which are formed on the growing skeletal tips. Labeled RAD were especially visible in the constant light treatment (Fig. 3f), forming a continuous growth front with adjacent TD. These results indicate that both of these ultra-structural components of the skeleton are forming during the 12 hours daytime labeling pulses, both under the LD photoperiod and under the constant light (LL) conditions.

Figure 3
Figure 3

Dynamics of daytime coral skeletal extension of Acropora eurystoma recorded under different light treatments: ambient photoperiod (ac), 12hLight/12hDark ("L" stands for light, 7:00 am to 7:00 pm; "D" stands for darkness, 7:00 pm to 7:00 am), constant light (df) (L/L) and constant darkness (gi) (D/D). Horizontal plot above each set of images shows 86Sr labeling pulses (yellow boxes: 7:00 am to 7:00 pm), 36 h intervals of growth in unlabeled seawater with normal isotopic abundance, and duration of 12Light/12hDark photoperiod, constant light and constant darkness conditions. During the ambient normal photoperiod (a–c) and constant light (d–f) regimes, all 5 labels (L1–L5) are visible. During constant darkness treatments (3 last labelling events) only 3 labeling events are detectable. There is clear distinction between continuous labeling in fast skeleton extension region, which consists mostly of rapid accretion deposits and disrupted, "crescent" labeling in thickening deposits (shingles) region. NanoSIMS 86Sr/44Ca isotope mosaic maps. (a,d,g), SEM images of polished and etched samples. (b,e,h) and NanoSIMS and SEM images overlaid (c,f,i). Yellow dashed arrows (a,d,g) mark fast growing regions where Rapid Accretion Deposits (RAD’s) are mostly located. Red rectangles (f) mark regions where RAD are particularly clearly labeled.

Under the constant light treatment, the 86Sr-labeled RADs formed during the 4th labeling pulse were thicker compared to the adjacent Thickening Deposits (TD) formed in the same time span (Fig. 3d–f). These observations may indicate differences in skeletal accretion rates, with a higher rate of skeletal extension in the RADs compared to the TDs, which should be confirmed via absolute Sr/Ca analysis (similar confirming results in other species Pocillopora damicornis32 and Porites lobata29). Average 12 h daytime extension rates of the Thickening Deposits, measured as the thickness of bands with incorporated 86Sr label, were at 0.58 μm and 0.55 μm for LD and LL, with standard deviation of 0.20 μm and 0.40 μm for LD and LL, respectively. In the constant dark treatment (DD), a maximum of three 86Sr labeled bands were detected in the skeleton of A. eurystoma nubbins (Fig. 3g–i), despite the fact that more than 10 areas in apical corallites were mapped with the NanoSIMS. This result indicates that skeletal extension continued during the first 12 hours daytime 86Sr pulse in the dark (labeling event L3), in at least a few skeletal areas corresponding to Thickening Deposits, and then slowed down and stopped sometime during the next 2 days under the DD treatment.

The scale-like structures (shingles) that form thickening deposits (typical of Acropora species) in specimens cultured under DD differ from those grown in the controlled LD and LL settings. The shingles from skeletons formed in DD are less regular and their surfaces are smoother compared to shingles from the LD and LL specimens, which are regular and their edges are more distinct (Fig. 4). The NanoSIMS maps of elongated skeletal tips (Fig. 3d–f) show distinct spatial distribution-pattern differences in 86Sr label incorporation between RADs and Thickening Deposits (shingles): the labeled regions close to RAD typically form continuous layers whereas in TD region, successive, crescent-like labeled zones are formed along bundles of fibers that project on the skeleton surface as shingles.

Figure 4: Compared skeleton surface textures of thickening deposits (i.e. shingles) in Acropora eurystoma corals cultured for 4.5 days (108 h) in constant light or constant dark conditions.
Figure 4

(ac) Specimen growing in constant darkness (D) during last 3 86Sr labeling pulses. (d–f) Specimen growing in constant light (L) during last 3 86Sr labeling pulses (see Figs 1 and 4). Although shingles (scale-like thickening deposits) are recognizable in both samples, shingles in specimen growing in constant light (d–f) are more regular and have surface with clearly visible fibers. In contrast, shingles in specimen growing in constant darkness (a–c) are irregular and fibers at their surface are smooth.

Discussion

The majority of studies dealing with the calcification mechanism of scleractinian coral have been focused on short term observations with little attention to the calcification process diel variations33. In this study we investigate the calcification of the Red Sea scleractinian coral A. eurystoma during different light regimes treatments, with continuous observations longer than 24 hours. Throughout the constant light treatment (LL), A. eurystoma coral’s fragments exhibited a cyclic pattern over the first 24 hours of the experiment and then exhibited a second cycle during the second day of the experiment, where the high day calcification is prolonged (Fig. 2c). Moreover, during the constant irradiation profile of the LD illumination treatment the coral’s calcification process displayed a cyclic pattern (Fig. 2b). These calcification patterns which were exhibited under LL and LD treatments, demonstrate an interesting cyclic dynamics which is associated with the “Light-enhanced calcification” phenomenon. During exposure to light it is possible that products of photosynthesis by the zooxanthellae may affect the host calcification and act as a major energy fuel for the process4,34. Therefore, it may be the cyclic metabolic activity of the coral symbionts and their photosynthesis pacemaker12,13,14 that drive the cyclic pattern of the coral calcification.

Evidences from precipitation of CaCO3 that were recorded under DD conditions with 86Sr labeling of the Thickening Deposit microstructural components (Fig. 3g–i) show labeling formation that took place only during the first 12 hours of darkness. During DD treatment in the 86Sr labeling, the skeleton extension most likely persisted only during the first 12 hours during DD treatment (labeling event L3, which followed the last regular nighttime – Fig. 3g–i). This fact suggests that skeletal extension persisted until energy reserves that originate from photosynthate translocation by dinoflagellates were depleted. Indeed, previous work reports depletion of photosynthetic carbon reserves within 18–20 hours of constant darkness7. This finding indicates that the calcification process keeps going during the first subjective daytime without external light and without new photosynthate production by the algal symbionts. The SEM images of coral skeleton textures under DD (Fig. 4) clearly support the irregular extension seen with the 86Sr labeling. These textures imply for a possible overall CaCO3 dissolution over precipitation. The disagreement between the skeletal extension visualized with 86Sr labeling during the first 12 hours of prolonged darkness (Fig. 3g–i) and the dissolution pattern indicated from the relative alkalinity depletion (Fig. 2d) could be explained by differences in skeletal density and the fact that skeletal microstructures were not labeled in all growth directions. Calcification is the product of skeletal extension and density increase35, and these precipitation processes may be temporally uncoupled. It is also possible that in the absence of light, the dissolution process masks the low calcification diel cycle (Fig. 2d).

The calcification cyclic patterns during light treatments (Fig. 2a–d) presented here suggest for a link to the algae’s circadian clock, which may influence the host calcification apparatus. However, several evidences indicate for a lower degree of the symbionts involvement in the host calcification process: (a) The growing tips of branching corals show high rates of skeletal extensions, but they are free of zooxanthellae27,36,37; (b) Calcification rates of bleached corals were higher when exposed to light than corals with symbionts that exposed to oxygen and glycerol under dark conditions4; (c) Light has shown to affect the activity of transmembrane ion pumps and channels associated with the calcification mechanism of the symbiotic giant clam Tridacna squamosa38. It seems from those studies that light is important for the calcification mechanism not only as an autotrophic source of energy but as an entrainment (synchronizing) cue. Indeed, up-regulation of related genes associated with calcification has been found in skeletal organic matrix genes39 and also in genes of enzymes which active in the growing tips of branching corals14,40. Hence, the regulation of genes that are associated with the calcification mechanism is likely coordinated by light, and is reflected in diurnal-nocturnal genetic transcription variation. A potential explanation for the light entrainment of the calcification mechanism may be related to an internal pacemaker/circadian clock mechanism. Recent evidences have uncovered the presence of circadian clock molecular components in symbiontic corals and in other members of the phylum Cnidaria, which are counterparts of many other animal clock components related to light41,42,43.

The observations of skeletal formation dynamics based on 86Sr pulse labelling, showed overall similar pattern of skeleton formation during LD and LL light treatments. Both ultra-structural skeletal elements, the Rapid Accretion Deposits (RADs) and the Thickening Deposits (TD)44 were labelled with 86Sr during the subjective 12 h daytime pulses. RAD are characterized as regions of skeletal rapid accretion and are deposits of calcium carbonate crystals embedded in an organic material, while TD are more dense skeletal structures (include less organic material) with a fibrous appearance deposited outside adjacent RAD. Continuity of the 86Sr labeled growth front between RAD and TD microstructures (Fig. 3) indicate that these regions were forming simultaneously during daytime, in agreement with previous work, studying the extension of microstructures in Porites lobata skeleton, using 86Sr pulse-labeling with NanoSIMS analysis29. However, other authors have reported coral skeletal formation along a day-night cycle, based on temporal differences in microstructural density45 or organic matrix incorporation46.

Hence, this paper suggests that light is an entrainment (synchronizing) cue and most likely a gated signal to initiate the calcification process and guarantees that the CaCO3 precipitation will perform with a cyclic pattern. Due to the obligated complex association between the host and the symbiotic photosynthesis process, isolating the calcification process and revealing its composing parts need further studies. Furthermore, the interplay between the Symbiodinium core mechanism clock, which governs its photosynthesis and the host circadian endogenous pacemaker, is still unclear.

Nevertheless, this study demonstrates that the overall coral calcification rhythmicity is consistent with an independent cyclic pattern. The cyclic pattern of the coral calcification during the different constant light treatments, which emerged from results of relative calcification (Total Alkalinity measurements) and the skeletal extension with 86Sr pulse-labeling, most likely indicate the presence of an independent pacemaker (of the host, algae or even a synergistically cue from both animals) that controls the coral calcification process.

Symbiotic corals have a unique challenge in terms of their need to respond not only to external environmental factors but also to metabolite fluxes and intracellular stresses imposed by their symbionts. Therefore, reef-building corals have adapted to life with symbionts by coupling the expression of the calcification process to the circadian clock to effectively pre-empt the photosynthesis cycle47,48,49. Given that corals have maintained a stable partnership with their symbionts, subtle physiological and molecular adaptations are to be expected11. The Acropora calcification rhythmic oscillations with the dependency of light may illustrate the evolutionary flexibility of circadian regulatory systems between the coral and its Symbiodinium internal pacemaker and provide a paradigm for understanding other animal/algal symbioses. Comparison with calcifying symbiotic mollusks, some of which also host Symbiodinium, will be of particular interest.

Methods

Coral collection

Apical branch fragments of scleractinian coral Acropora eurystoma colonies (Fig. 1) approximately 5 cm long were collected by SCUBA diving from 5–6 meters depth at the coral reef near the Inter-University Institute (IUI) in Eilat, Gulf of Aqaba, Red Sea (CITES #38406). The fragments were transferred to an outdoor, shaded running seawater table at the IUI for a month of acclimation before the experiment started.

Relative calcification cycle measurement by total alkalinity method and data analysis

Coral calcification diel cycles were recorded under different light regimes, ambient natural light cycle, 10/14 hours of light/dark (LD), constant light (LL), and constant darkness (DD). Relative calcification values are presented as calcification measurement value relative to the highest value measured during the 48 hours experimental period for each coral fragment, according to equation 1. Calcification was determined from the difference in total alkalinity (AT) measured between the beginning and the end of a two-hour incubation period according to equation 2.

G is calcification rate and Gm is the maximum calcification rate during the 48 hours of incubations, T is the duration of the incubation (i.e. 2 hours) and V is the water volume in the incubation vessel. Maximum calcification (Gm) values that were used for eq. 1 were measurement time 12:00 at the first 24 hours experiment for ambient and LL treatments, measurement time 12:00 at second 24 hours experiment for LD treatment, and measurement time 20:00 at the second 24 hours experiment for DD treatment.

Each incubation period was followed by a two-hour recovery period in running seawater. In this way, the relative calcification cycle was measured during a 48 hours period, with 4 fragments (quadruplicate) included in every treatment. The relative calcification cycle result during light treatments presented in Fig. 2 is the average of the 4 fragments relative calcification.

AT precision is 4.6 ± 0.3 μmol Kg−1. Light intensity was measured using a quantum flat sensor (LI-COR, Lincoln, NE, USA). The LD and LL irradiance level was 180 ± 20 μmol quanta m−2 s−1. Seawater temperature for all treatments was 22 ± 0.5 °C. Each individual coral fragment was incubated in closed 100 ml glass jars. The incubated seawater was sampled and stored in gas tight bottles and stored in a refrigerator (4 °C) until titrated for AT using Gran plot50 on a Titrino plus 848 automated titrator (Metrohm AG).

Skeletal extension rate visualisation by 86Sr pulse-labeling and NanoSIMS imaging

A. eurystoma coral nubbins were labeled for 12 hours in individual glass beakers containing 500 ml of seawater enriched with 10 mg/L dissolved 86SrCO3, which was prepared following the procedures in previous study32. A stream of air was gently bubbled in each beaker with a Pasteur pipet to mix the labeled seawater around the nubbin and to equalize oxygen and CO2 levels. Five successive 12 hours labeling pulses took place under three light regimes to examine the dynamics of skeletal deposition: LD, LL and DD (see also Fig. 3). Two replicate nubbins were labeled for each of the three light treatments. At the end of the fifth labeling pulse, nubbins were snap-frozen at −80 °C to stop metabolic processes. For skeletal analysis, coral tissue was removed from each nubbin using a jet of filtered seawater (Waterpik method) and the skeletons were immersed in NaClO (5%) for 20 minutes to remove residual organic matter. The skeletons were embedded in Körapox resin and sections of the apical corallites parallel to the vertical growing axis were polished. The 86Sr/44Ca distribution was mapped with a NanoSIMS ion microprobe, following established procedures32.

For orientation of the 86Sr labeling with the skeletal microstructure, Scanning Electron Microscopy (SEM) images of mildly etched skeleton were taken using FEI Philips XL 20- instrument. The same SEM was used to visualize the skeletal surface textures of samples cultured under different light treatments. Bleached skeletal branch tips were mounted on SEM stubs, platinum-coated and observed.

Statistical analysis

For statistical analysis, repeated measures ANOVA followed by Bonferroni post hoc test was performed to assess the differences in relative calcification values within different light regimes. All statistical analyses were conducted using SPSS 20.0 (IBM, USA), and the results were considered statistically significant at P < 0.05.

Additional Information

How to cite this article: Gutner-Hoch, E. et al. Evidence for Rhythmicity Pacemaker in the Calcification Process of Scleractinian Coral. Sci. Rep. 6, 20191; doi: 10.1038/srep20191 (2016).

References

  1. 1.

    & In: Aquatic photosynthesis 2nd edn (Princeton University Press, 2007).

  2. 2.

    & Evolution of the coral zooxanthellae symbiosis during the triassic - a geochemical approach. Paleobiology 21, 179–199 (1995).

  3. 3.

    & Assimilation of photosynthetic products of zooxanthellae by a reef coral. Biol. Bull. 137, 506–523 (1969).

  4. 4.

    , & Calcification in bleached and unbleached Montastraea faveolata: evaluating the role of oxygen and glycerol. Coral Reefs 29, 899–907, 10.1007/s00338-010-0638-x (2010).

  5. 5.

    , & A coral polyp model of photosynthesis, respiration and calcification incorporating a transcellular ion transport mechanism. Coral Reefs 32, 779–794, 10.1007/s00338-013-1032-2 (2013).

  6. 6.

    et al. Highly dynamic cellular-level response of symbiotic coral to a sudden increase in environmental nitrogen. MBio 4, e00052–13 (2013).

  7. 7.

    et al. Subcellular investigation of photosynthesis-driven carbon assimilation in the symbiotic reef coral Pocillopora damicornis. MBio 6, e02299–14 (2015).

  8. 8.

    Circadian rhythms in corals, particularly Fungiidae. Biol. Bull. 151, 236–246, 10.2307/1540717 (1976).

  9. 9.

    Light dependent activity patterns among reef corals: Montastrea cavernosa. Biol. Bull. 156, 196–211, 10.2307/1541043 (1979).

  10. 10.

    , , , & Diel ‘tuning’ of coral metabolism: physiological responses to light cues. J. Exp. Biol. 209, 273–283 (2006).

  11. 11.

    et al. Complex diel cycles of gene expression in coral-algal symbiosis. Science 331, 175, 10.1126/science.1196419 (2011).

  12. 12.

    & The effect of temperature compensation on the circadian rhythmicity of photosynthesis in Symbiodinium, coral-symbiotic alga. Sci. Rep. 2, 10.1038/srep00536 (2012).

  13. 13.

    & Influence of the quantity and quality of light on photosynthetic periodicity in coral endosymbiotic algae. Plos One 7, e43264, 10.1371/journal.pone.0043264 (2012).

  14. 14.

    , , , & Photosynthetic circadian rhythmicity patterns of Symbiodium, the coral endosymbiotic algae. Proceedings of the Royal Society B-Biological Sciences 280, 10.1098/rspb.2012.2942 (2013).

  15. 15.

    & Effects of temperature on the mortality and growth of Hawaiian reef corals. Mar. Biol. 43, 201–208 (1977).

  16. 16.

    Seasonal variations in the rates of calcification and productivity in the coral Acropora formosa on a highlatitude reef. Mar. Ecol. Prog. Ser. 15, 135–140 (1984).

  17. 17.

    & Environmental controls on growth of the massive coral Porites. J. Exp. Mar. Biol. Ecol. 245, 225–243 (2000).

  18. 18.

    et al. Effect of calcium carbonate saturation of seawater on coral calcification. Global Planet Change 18, 37–46 (1998).

  19. 19.

    et al. Effect of calcium carbonate saturation on the calcification rate of an experimental coral reef. Global Biogeochemi Cycles 14, 963–974 (2000).

  20. 20.

    & Biocarboante addition promotes coral growth. Limnol. Oceanogr. 44, 716–720 (2001).

  21. 21.

    & The effect of carbonate chemistry on calcification and photosynthesis in the hermatypic coral Acropora eurystoma. Limnol. Oceanogr. 51, 1284–1293, 10.4319/lo.2006.51.3.1284 (2006).

  22. 22.

    The physiology of skeleton formation in corals. I. A method for measuring the rate of calcium deposition by corals under different conditions. Biol. Bull. 116, 59–75 (1959).

  23. 23.

    & Rhythmic variation in calcification and photosynthesis associated with the coral Acropora cervicornis (Lamarck). Proceedings of the Royal Society of London Series B-Biological Sciences 201, 179–189 (1978).

  24. 24.

    Calcification in hermatypic and ahermatypic corals. Science 271, 637–639 (1996).

  25. 25.

    , , & In-situ diel cycles of photosynthesis and calcification in hermatypic corals. Limnol. Oceanogr. 54, 1995–2002, 10.4319/lo.2009.54.6.1995 (2009).

  26. 26.

    & Light-enhanced calcification, and the role of oxidative phosphorylation in calcification of the coral Acropora cervicornis. Proceedings of the Royal Society of London. Series B. Biological Sciences 190, 323–331 (1975).

  27. 27.

    & Does light enhance calcification in hermatypic corals? Mar. Biol. 18, 1–6 (1984).

  28. 28.

    , & The mechanism of calcification and its relation to photosynthesis and respiration in the scleractinian coral Galaxea fascicularis. Mar. Biol. 142, 419–426 (2003).

  29. 29.

    et al. Simultaneous extension of both basic microstructural components in scleractinian coral skeleton during night and daytime, visualized by in situ86Sr pulse labeling. J. Struct. Biol. 185, 79–88 (2014).

  30. 30.

    & In: Coral reefs Ecosystems of the world (ed. ), 109–131 (Elservier, 1990).

  31. 31.

    & Geochemical perspectives on coral mineralization. Reviews in Mineralogy & Geochemistry 54, 151–187 (2003).

  32. 32.

    et al. Pulsed 86Sr-labeling and NanoSIMS imaging to study coral biomineralization at ultra-structural length scales. Coral Reefs 31, 741–752, 10.1007/s00338-012-0890-3 (2012).

  33. 33.

    & Rhythmic variations in calcification and photosynthesis associated with the coral Acropora cervicornis (Lamarck). Proceedings of the Royal Society of London B:Biological Sciences 201, 179–189 (1978).

  34. 34.

    et al. Coral calcification under daily oxygen saturation and pH dynamics reveals the important role of oxygen. Biology open, 10.1242/bio.20147922 (2014).

  35. 35.

    Skeletal development in Acropora cervicornis: I. Patterns of calcium carbonate accretion in the axial corallite. Coral reefs 1, 45–51 (1982).

  36. 36.

    , & Why does the white tip of stony coral grow so fast without zoxanthellae? Mar. Biol. 103, 359–363 (1989).

  37. 37.

    & Role of symbiotic algae (zooxanthellae) in coral calcification. Biol. Bull. 141, 350–363 (1971).

  38. 38.

    et al. Light induces changes in activities of Na+/K+-ATPase, H+/K+-ATPase and glutamine synthetase in tissues involved directly or indirectly in light-enhanced calcification in the giant clam, Tridacna squamosa. Front. Physiol. 6, 10.3389/fphys.2015.00068 (2015).

  39. 39.

    et al. Transcriptomic differences between day and night in Acropora millepora provide new insights into metabolite exchange and light-enhanced calcification in corals. Mol. Ecol. 24, 4489–4504 (2015)

  40. 40.

    & Diurnal and nocturnal transcriptomic variation in the Caribbean staghorn coral Acropora cervicornis. Mol. Ecol. 24, 4460–4473 (2015).

  41. 41.

    et al. Light-responsive cryptochromes from a simple multicellular animal, the coral Acropora millepora. Science 318, 467–470, 10.1126/science.1145432 (2007).

  42. 42.

    et al. Evidence for multiple phototransduction pathways in a reef-building coral. Plos One 7, e50371, 10.1371/journal.pone.0050371 (2012).

  43. 43.

    et al. Profiling molecular and behavioral circadian rhythms in the non-symbiotic sea anemone Nematostella vectensis. Sci. Rep. 5, 11418; 10.1038/srep11418 (2015).

  44. 44.

    Three-dimensional micro- and nanostructural characteristics of the scleractinian coral skeleton: A biocalcification proxy. Acta Palaeontol. Pol. 48, 497–530 (2003).

  45. 45.

    et al. Visualization of sub-daily skeletal growth patterns in massive Porites grown in Sr-enriched seawater. J. Struct. Biol. 180, 47–56 (2012).

  46. 46.

    et al. Immunolocalization of skeletal matrix protein in tissue and mineral of the coral Stylophora pistillata. Pnas 11, 12728–12733 (2014).

  47. 47.

    Organic reef-building: episodes of extinction and symbiosis? Senckenbergiana Lethaea 69, 315–368 (1988).

  48. 48.

    The role of algal symbiosis in reefs through time. Plalios 3, 221–227 (1988).

  49. 49.

    Enigmas in Phanerozoic reef development. Fossil Cnidaria 5, 371–385 (1989).

  50. 50.

    Determination of the equivalence point in potentiometric titrations. Part II. Analyst 77, 661–671 (1952).

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Acknowledgements

This work was supported in part by the European Research Council Advanced Grant 246749 (BIOCARB) to AM and by the MNHN ATM ‘Biomineralization’ program to AM and IDC. NanoSIMS analyses were conducted at the MNHN platform funded by the CNRS and the Region Ile de France. We would like to thank the French Embassy in Israel for their financial support to EGH, and also thank the Interuniversity Institute (IUI) Marine Lab in Eilat for support the experiments conducted at the station. This work represents partial fulfillment of the requirements for a PhD thesis for Gutner-Hoch Eldad at Bar-Ilan University, Faculty of Life Sciences, Israel.

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Affiliations

  1. The Mina & Everard Goodman Faculty of Life Sciences, Bar-Ilan University, 52900 Ramat-Gan, Israel

    • Eldad Gutner-Hoch
    • , Kenneth Schneider
    •  & Oren Levy
  2. Institute of Paleobiology, Polish Academy of Sciences, Twarda 51/55, PL-00-818 Warsaw, Poland

    • Jaroslaw Stolarski
  3. MCAM UMR7245, Sorbonne Universités, Muséum National d’Histoire Naturelle, (CP54) 57 rue Cuvier, 75005 Paris, France

    • Isabelle Domart-Coulon
  4. Department of Earth and Planetary Sciences, Weizmann Institute of Science, P.O.Box 26, 76100 Rehovot, Israel

    • Ruth Yam
    •  & Aldo Shemesh
  5. Laboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique Fédérale de Lausanne (EPFL), CH-1015 Lausanne, Switzerland

    • Anders Meibom
  6. Center for Advanced Surface Analysis, Institute of Earth Sciences, University of Lausanne, Lausanne, Switzerland

    • Anders Meibom

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Contributions

E.G.H. and O.L. designed the research. E.G.H., K.S. and I.D.C. performed the research. E.G.H., J.S. and I.D.C. analyzed the data. E.G.H., K.S., J.S. and O.L. wrote the main manuscript. All authors reviewed and edited the manuscript.

Competing interests

The authors declare no competing financial interests.

Corresponding author

Correspondence to Eldad Gutner-Hoch.

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