A stable ultrastructural pattern despite variable cell size in Lithothamnion corallioides
- Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milan, 20126, Italy
Correspondence: Valentina Alice Bracchi (firstname.lastname@example.org)
Recent advances on the mechanism and pattern of calcification in coralline algae led to contradictory conclusions. The evidence of a biologically controlled calcification process, resulting in distinctive patterns at the scale of family, was observed. However, the coralline calcification process has been also interpreted as biologically induced because of the dependency of its elemental composition on environmental variables. To clarify the matter, five collections of Lithothamnion corallioides from the Atlantic Ocean and the Mediterranean Sea, across a wide depth range (12–66 m), have been analyzed for morphology, anatomy and cell wall crystal patterns in both perithallial and epithallial cells to detect possible ultrastructural changes. L. corallioides shows the alternation of tiers of short-squared and long-ovoid/rectangular cells along the perithallus, forming a typical banding. The perithallial cell length decreases according to water depth and growth rate, whereas the diameter remains constant. Our observations confirm that both epithallial and perithallial cells show primary (PW) and secondary (SW) calcite walls. Rectangular tiles, with the long axis parallel to the cell membrane forming a multi-layered structure, characterize the PW. Flattened squared bricks characterize the SW, with roundish outlines enveloping the cell and showing a zigzag and cross orientation. Long and short cells have different thicknesses of PW and SW, increasing in short cells. Epithallial cells are one to three flared cells with the same shape of the PW and SW crystals. Despite the diverse seafloor environments and the variable L. corallioides growth rate, the cell walls maintain a consistent ultrastructural pattern with unaffected crystal shape and arrangement. A comparison with two congeneric species, L. minervae and L. valens, showed similar ultrastructural patterns in the SW but evident differences in the PW crystal shape. Our observations point to a biologically control rather than an induction of the calcification process in coralline algae and suggest a possible new morphological diagnostic tool for species identification, with relevant importance for paleontological applications. Finally, secondary calcite, in the form of dogtooth crystals that fill the cell lumen, has been observed. It represents a form of early alteration in living collections which can have implications in the reliability of climate and paleoclimate studies based on geochemical techniques.
The subclass Corallinophycidae is spread globally and comprises the crustose coralline algae (CCA), important Mg-calcite calcifiers and habitat builders of rhodolith beds, temperate algal reefs and tropical coralgal reefs (Adey, 1986; Cabioch and Giraud, 1986; Ries, 2006; Caragnano et al., 2009; Bracchi et al., 2014, 2016; Marchese et al., 2020). The complex calcifying process in CCA takes place during their whole life span and involves the entire organism. For this reason, corallines bear witness to past benthic primary production by macroalgae with an excellent fossil record (Basso et al., 2007; Bracchi et al., 2014, 2016; Ragazzola et al., 2020).
Rhodoliths are unattached nodules formed mostly by CCA. Among them, free-living unattached branches usually characterize maerl beds in the northeastern Atlantic Ocean (Henrich et al., 1995; Birkett et al., 1998; Peña and Bárbara, 2008, 2009; Peña et al., 2014) and in the Mediterranean Sea (Huvé, 1956; Jacquotte, 1962; Gambi et al., 2009; Agnesi et al., 2011; Savini et al., 2012; Basso et al., 2017).
In both geographical settings, the most common species are Lithothamnion corallioides (P. Crouan and H. Crouan) P. Crouan and H. Crouan 1867 and Phymatolithon calcareum (Pallas) W. H. Adey and D. L. McKibbin ex Woelkering and L. M. Irvine 1986 (Adey and McKibbin, 1970; Basso et al., 2017; Hernandez-Kantun et al., 2017).
L. corallioides is distributed between the Canary Islands, at roughly 28∘ N, and Scotland, at about 58∘ N (Irvine and Chamberlain, 1994; Wilson et al., 2004), and it is considered one of the most suitable species for paleoclimate reconstruction (Foster, 2001). This species usually forms twig-like structures and is brown to pink or purplish and often sterile, with branch diameters typically in the range of 1–2 mm and with knob-like apices (Irvine and Chamberlain, 1994). Primary production, respiration and calcification in L. corallioides are strongly influenced by seasonality because of the oscillations of temperature and irradiance levels (Adey and McKibbin, 1970; Potin et al., 1990; Martin et al., 2006). L. corallioides shows a favorable response to temperature increase, reaching its maximum primary production during summer (Adey and McKibbin, 1970; Potin et al., 1990). L. corallioides' minimum survival temperature is between 2 and 5 ∘C, while the optimal growth is observed between 13 ∘C (Adey and McKibbin, 1970) and 14 ∘C (Blake and Maggs, 2003). In longitudinal sections, the periodical change in growth rate due to the alternation of seasons generates perithallus banding in Lithothamnion species, as in the long protuberances of L. corallioides. Banding results from an evident alternation of tiers of thick-walled, generally short cells versus thin-walled long cells along the main axis of perithallus growth (Basso, 1995; Basso et al., 1997; Kamenos and Law, 2010, Burdett et al., 2011). Banding has been interpreted as the visible effect of the environment (primarily temperature) on algal growth at different timescales (day, month) (Halfar et al., 2000; Foster, 2001). An alternative explanation would consider banding as the periodical shift between tiers of cells possessing a different wall structure (Nash et al., 2019).
In general, the calcifying process of CCA has been described as the deposition of tangential calcite needles in the outer part of the cell wall (interstitial matrix), followed by the formation of radial needles in the cell wall itself in contact with the plasmalemma. The polysaccharide and fibrillary matrix control both processes (Giraud and Cabioch, 1976; Irvine and Chamberlain, 1994; Adey, 1998; de Carvalho et al., 2017). In L. corallioides, calcification has been described as being composed of tangential rod-shaped crystals in the primary wall (PW) and perpendicular fan-like rods in the secondary wall (SW) (Giraud and Cabioch, 1976). Borowitzka (1984, 1989) proposed that coralline algae have semi-organized calcification, suggesting that their calcification is biologically controlled, as also indicated by Cabioch and Giraud (1986), rather than induced, as more recently supported by de Carvalho et al. (2017) and Nash et al. (2019). Cell wall ultrastructures are recognized as a valuable tool to define the phenotypic expression of genotypic information (Auer and Piller, 2020). The compelling evidence of a biological control over calcification in coralline algae was provided by the identification of family-specific cell wall ultrastructures. Epithallial cells in the genus Lithothamnion show crystal units as thin rectangular blocks (Auer and Piller, 2020). Seasonality, including seawater temperature oscillations and photoperiod, is considered one of the main factors affecting the growth rate and the biomineralization process (Steller et al., 2007; Kamenos and Law, 2010; Vásquez-Elizondo and Enríquez, 2017), which may influence the ultrastructural pattern.
The identification of CCA in present-day integrative taxonomy is based on genetic methods coupling with the morphological description and measurement of diagnostic features (for example: Basso et al., 2015; Caragnano et al., 2018; Costa et al., 2019). Species identification in the fossil record is, on the contrary, merely based on the preservation of morphological taxonomic characters. Consequently, the identification of valuable morphological characters as a tool for the definition of the paleontological species represents an important challenge. CCA are well represented in the fossil record, and L. corallioides has been reported in the Pliocene of Spain (Aguirre et al., 2012) and in the Pleistocene of southern Italy (Bracchi et al., 2014).
This study is aimed at describing the ultrastructural mineralogical features of L. corallioides from different geographic settings (northeastern Atlantic Ocean and Mediterranean Sea) and across a wide bathymetric interval (12–66 m) to test if the ultrastructural pattern is preserved under different environmental conditions and therefore can be considered as an evident sign of a biologically controlled mineralization. Moreover, the identification of a specific ultrastructural pattern could be considered as a valuable tool for species identification to be used also in paleobiology. L. corallioides has been targeted because of its wide distribution, both geographically and bathymetrically, and its occurrence in the fossil record.
For this study, we considered five collections (Fig. 1, Table 1) from two different geographic settings, the Atlantic Ocean and the western Mediterranean Sea, sampled by scuba diving or grabbing at different depths ranging from 12 m in Morlaix Bay (France) down to 66 m in the Pontine Islands (Italy). All specimens have been collected alive. Table 1 reports locations and dates of sampling.
To highlight possible ultrastructural differences among the same genus, two additional collections, already identified as Lithothamnion minervae Basso, 1995, and Lithothamnion valens Foslie, 1909, have been considered. These collections have been sampled alive from the Egadi Islands (Italy), during July 2016, at 103 and 86 m water depth respectively.
All samples have been air dried and sheltered from sunlight. Once dried, they were stored in plastic boxes with silica to avoid any decay and transported to the laboratories of the University of Milano-Bicocca.
The seawater temperature has been extracted from 11 years of monthly reanalysis spanning 1979–2017 from ORAS5 (Ocean Reanalysis System 5), at 0.25∘ horizontal resolution (Zuo et al., 2019), to indicate the seasonal temperate fluctuation (Table 1).
2.1 Coralline sample preparation
Samples have been prepared for scanning electron microscope (SEM) imaging. Altered, badly preserved or encrusted branches have been discarded. Only the branches showing a shiny surface have been picked from all collections, each controlled under a stereo microscope, and cleaned manually by removing epiphytes and other encrustations. Each sample, composed of multiple branches, has been cleaned in an ultrasonic bath in distilled water for 10 min and air-dried. The branches were then placed in small cylindrical plastic boxes with a base diameter of 1′′ (2.54 cm). Branches have been piled up and aligned to obtain multiple layers. The samples were embedded in Epofix resin for SEM analyses, which was stirred for 2 min with a hardener (13 % ), and they were left to harden for 1 d at room temperature. Samples have then been cut normal to the multiple layers by using an IsoMet diamond wafering blade 15HC, along the direction of branch growth. The number of branches per sample are indicated in Table 1. Moreover, two additional samples (L. minervae and L. valens) have been prepared for SEM observations (n=10 branches) by breaking them with a small chisel. Both longitudinal and surface sections have been selected for SEM observations.
2.2 Scanning electron microscope
For SEM imaging, the surfaces of embedded samples have been polished by using different sizes of silicon carbide, cleaned ultrasonically in distilled water for 10 min and air-dried. Samples mounted directly on stub have been simply chrome-coated. SEM images have been taken with a field emission gun scanning electron microscope (SEM-FEG): Zeiss Gemini 500 and a TESCAN VEGA TS 5136XM. Standard magnifications for SEM images were established (∼ 2500X, ∼ 5000X, ∼ 10000X, ∼ 20000X and ∼ 30000X) to describe comparatively and measure growth bands and cells, the morphology of Mg-calcite crystals, and the main features of perithallial and epithallial cell walls. A rigorous control over cell orientation is required to represent, describe and measure in 2D the main features of a 3D structure such as cell calcification (both PW and SW). Longitudinal axial sections of branches are a standard representation for calcareous red algae, allowing for subsequent visual comparison (Woelkerling, 1988; Quaranta et al., 2007; Burdett et al., 2011). Surface tangential sections are useful to describe the epithallial cells. Transverse or oblique sections are useful to describe qualitatively the 3D aspects and organization of calcite crystals composing both PW and SW. Description of the cell wall structure follows the nomenclature of Flajs (1977), presenting the PW and SW calcifications of the wall. Some authors refer to PW as interstitial calcite (Ragazzola et al., 2016) or interfilament calcite (Nash and Adey, 2017; Nash et al., 2013, 2015). Cell dimensions have been measured as reported in Fig. 2 (n=10 per sample) exclusively on longitudinal sections (Fig. 2). Separation among adjacent filaments was not always obvious (Fig. 2c). In such cases, the PW of adjacent cells has been measured in total (green line in Fig. 2c), and then half of the total was attributed to each cell. In the text we use the term ultrastructure to identify the singular crystal in one of the layers of the cell wall and ultrastructural pattern to indicate the combination and mutual organization of crystals in layers of the cell wall.
2.3 Statistical analyses
Spearman and Pearson correlations were used to test the statistical relationship between the cell measurements in both long and short cells, including morphometry and cell wall thickness. The linear correlation between the mean cell lengths and the sampling depths was measured by Pearson's coefficient as well. One-way ANOVA and the Kruskal–Wallis tests respectively followed by the Tukey's test and the Dunn's test for post hoc analysis were used to compare the cell measurements among sampling sites and to provide evidence of the differences between group means and medians. All statistical analyses were run in R 3.6.3 software.
2.4 Growth rates
Growth rates were estimated under light microscope by measuring a linear transect on the longitudinal section and counting the number of growth bands of fourth order (sensu Foster, 2001) crossed by the transect. The growth rate has been calculated by dividing the length of the transect by the number of growth bands.
3.1 Ultrastructures from SEM images
Selected rhodoliths belong to the unattached branches morphotype (Basso, 1998; Basso et al., 2016), never exceeding 3 cm in length (Fig. 1). The diameter of each branch never exceeds 2.5 mm (Fig. 1). The color varies from yellowish white to pink/purplish, with typical knob-like apices (Fig. 1).
Once cut, all samples show the same micromorphology (Fig. 3a–i, Supplement 2), with the constant occurrence of an easily detectable banding due to the alternation of series of short and long cells (Fig. 3a, b) in bands of the fourth order corresponding to 1 year (Foster, 2001). No reproductive structure (conceptacle) was detected.
Along the perithallus, long cells are ovoid to rectangular in shape (Fig. 3c, d, Supplement 2), whereas short cells are more squared (Fig. 3e, f).
Within the long-celled bands, the longest cells were measured in the sample from Morlaix Bay (26.71 ± 1.74 µm), while the less elongated cells were observed in the sample from the Pontine Islands (13.05 ± 0.76 µm) (Table 2, Fig. 4).
Within the short-celled bands, the shortest cells were observed in the sample from Pontine (6.97 ± 0.25 µm), while the longest short cells were from Morlaix Bay (13.90 ± 0.88 µm) (Table 2, Fig. 4). Cell diameter ranges between 7.69 ± 1.07 µm (Santa Caterina shoal) and 11.11 ± 1.79 µm (Morlaix) in long cells and between 8.27 ± 0.48 µm (Pontine) and 9.23 ± 0.70 µm (Egadi) in short cells (Table 2, Fig. 4).
Both long and short cells have PWs and SWs, and the style of mineralization shows a consistent ultrastructural pattern. The PW crystallization observed in longitudinal medial sections (cutting the cell lumen) is composed of elongated crystals appearing as rods (Fig. 5a–c, e), but where longitudinal sections are tangential to the PW, crystals are revealed to be flat rectangular tiles (Figs. 5d, f, 6a). The long axis of the PW tiles is parallel to the cell membrane and may form a multi-layered structure which envelops the cell (Fig. 5e). The dimensions of the tiles are 0.61 ± 0.17 µm in length and 0.05 ± 0.01 µm in height (Fig. 6a). Elongated radial crystals (Fig. 7a, b) in longitudinal sections cutting the cell lumen characterize the SW. Small, roundish units, appearing as being fused together, in places showing an apparent multi-layered structure (Fig. 7b) form such crystals. These elongated crystals are radial to the cell lumen (Fig. 7a–c). Where the cell membrane is lost, the SW can be observed from different orientations, and such apparently elongated crystals are revealed to be thin bricks with rounded margins (Figs. 6b, 7d–f). Bricks are squared, and length and width are 0.63 ± 0.15 µm (Fig. 6b). The bricks form a sort of envelope around the cell (Figs. 6b, 7e, f), showing sometimes a zigzag and cross orientation (Fig. 7g, h).
Different thicknesses characterize the PW and SW of short and long cells (Figs. 3, 5, 7; Table 2, Supplement 2) in longitudinal medial sections. Both PW and SW of short cells are generally thicker than in long cells (Table 2) even if the thickness does not show a correlation with sampling bathymetry. The SW thickness ranges between 1.52 ± 0.65 µm (Pontine) and 2.20 ± 0.45 µm (Elba) in short cells and between 0.57 ± 0.14 µm (Morlaix) and 1.26 ± 0.42 µm (Santa Caterina shoal) in long cells (Table 2).
Both PW and SW show fibrils (Borowitzka, 1982) forming a dense network in support of the mineralization (Fig. 7d).
The epithallus is formed by one to three flared cells in longitudinal sections (Figs. 3g–j, 5f, 7c), always mineralized, with some exceptions in the top distal surface (Fig. 3g–j). The cell wall shows the same ultrastructural features of the perithallial cells, with both PW and SW mineralized (Figs. 3i, j, 5f, 7c).
Based on image analysis and time of collection, the calculated growth rate ranges from 0.10 mm/yr in Pontine to 0.13 mm/yr in both Morlaix and Egadi.
The two additional collections of L. valens and L. minervae (Fig. 8) are characterized by both PW and SW (Fig. 8a, b, e, f). The SW shows, in both species, an ultrastructural pattern like the one described for L. corallioides , with oriented bricks with rounded margins variably orientated, only apparently elongated and radial to the cell lumen in longitudinal sections (Fig. 8b, f). If observed in the cell lumen, where the cell membrane is lost, the SW shows bricks with different orientation and sometimes a zigzag and cross orientation (Fig. 8d, g).
On the contrary, PW shows a different shape and arrangement of crystals which are not characterized by the tiles of L. corallioides observed in Figs. 5d and 6a. Calcite crystals are squatter and more granular (Fig. 8a) or with irregular shape (Fig. 8h). One interesting aspect is that both samples show the occurrence of secondary calcite in the form of dogtooth crystals filling the cell lumen (Fig. 8b, c, e).
3.2 Statistical analyses on morphological parameters
The differences in the long cells' morphometry and wall thickness among sampling sites are statistically significant for each measured parameter (p<0.05; Supplement 1) (Fig. 9). Interestingly, the long-cell length of the deepest sample from Pontine Islands (66 m depth) is lower than the others (p<0.001) (Figs. 4, 9; Supplement), while in the shallowest sample collected in Morlaix (12 m depth) cells are remarkably longer (p<0.001) (Figs. 4, 9; Supplement 1).
In short cells, significant differences result only for cell (Fig. 9) and lumen lengths, as well as cell PW (p<0.05; Supplement). The shortest cells are observed again in the sample from Pontine Islands, differing from the one collected in Morlaix (p<0.01) (Fig. 9; Supplement 1), which stands out for being the highest value. On the contrary, the cell diameter slightly varies among sites, showing significant differences just in long cells (p<0.01; Supplement 1) (Fig. 9), with significantly higher values in Morlaix with respect to Elba island and Santa Caterina. The dimensions of the cell lumen change accordingly because of the positive correlation with the cell dimensions (Supplement 1).
Although banding is reported for all samples, elongation decreases with increasing depth, showing a strong inverse correlation in long cells (p<0.01; r=0.98) (Fig. 9). The same trend is also observed in short cells, although with non-significant values (p=0.09) (Fig. 9).
Properly oriented longitudinal and transverse/oblique sections are required to obtain a precise comparative description of the main morphological features of CCA. Multi-scale approaches are also relevant, among which the ultrastructural pattern may represent a new powerful and strategic diagnostic tool (Figs. 3–7).
Recent studies based on genetic identification exclude the occurrence of other Lithothamnion species in the maerl of Morlaix Bay (Carro et al. 2014; Melbourne et al., 2017). Based on this identification and considering the macroscopic features, the thallus pattern, the microanatomy, the morphology and the morphometry of cell walls (Figs. 3, 5–7, Table 2), we identified the samples from Morlaix Bay as belonging to the species L. corallioides.
We compared the Mediterranean specimens with the Atlantic L. corallioides, and upon corresponding morphology, anatomy and ultrastructure (Figs. 3, 5–7, Table 2), we considered them as conspecific.
The perithallus of L. corallioides clearly shows the alternation of growth bands of third and fourth orders (Fig. 3a, b), in agreement with Foster (2001). Fourth-order bands represent the annual cycling, whereas third-order ones represent seasonal variations and can be firstly distinguished by an evident chromatic change due to the different calcification thickness between long and short cells (Foster, 2001). In our samples, the banding (third and fourth orders) is easily recognizable (Fig. 3), and both long and short cell lengths decrease across depths (Figs. 4, 9), as expected, mirroring a decrease in growth rate, whereas the diameter variation is significantly lower (Fig. 4, Supplement 1).
Giraud and Cabioch (1979) observed that a cell wall fracture in L. corallioides shows a layer of radial calcite crystals (SW) separated from its neighbor by a different sheet composed of tangential crystals (PW). A discontinuity that coincides with the fibrillar matrix observed in sections of decalcified material marks the limits of adjacent cellular filaments (Giraud and Cabioch, 1979). Our results match with the observations of these authors in longitudinal sections (Figs. 3, 5, 7), although the discontinuity between adjacent cells is not easily detectable because of the complete mineralization.
Auer and Piller (2020) built a morphological tree based on the observation of different ultrastructural patterns in epithallial cells, which matches with the phylogenetic tree at family level. For Hapalidiaceae, and in the Lithothamnion-type epithallial ultrastructure, they observed the occurrence of PWs with primary crystals formed along the middle lamella and the SWs with secondary rod-shaped crystals, also presenting fan-like structures. The samples studied in the present work show the PW and SW in both perithallial and epithallial cell walls (Figs. 3, 5, 7). Both are apparently composed of rod-like crystals in longitudinal sections. However, in longitudinal sections that are locally tangential to the PW, the apparent rods are revealed to be the longest and thinnest side of variably oriented rectangular tiles (Figs. 5, 6a). The tiles that envelop the cell (Fig. 5d, f) are the basic ultrastructural elements forming the PW. Differently, apparent rods of the SW are revealed to be squared and relatively flat bricks with rounded margins, as observed at the cell lumen without membrane or exactly at the contact between the SW longitudinal section and cell lumen (Figs. 6b, 7). Crystals in longitudinal sections of the SW are radial to the cell lumen, in agreement with Giraud and Cabioch (1979), and appear formed by small grains fused together (Figs. 3, 7b, f). They can also show a zigzag and cross orientation (Fig. 7g, h) like the fan-delta structure described by Auer and Piller (2020).
Therefore, our findings agree with the results of Auer and Piller (2020), although providing a more detailed description of the ultrastructural pattern of L. corallioides (Fig. 6).
Despite the different environmental conditions, likely occurring at the different sampling sites and depths, the ultrastructures of both PW and SW seem conservative and detectable in all samples. Therefore, the ultrastructures and the ultrastructural pattern are not dependent on environmental controls.
However, L. corallioides shows variable cell elongations (Table 2) and growth rates, both decreasing according to sampling depth (Fig. 9), and a variation in PW and SW thickness, generally greater in short than in long cells, unrelated to depth (Table 2, Supplement 1). These features possibly represent the effect of the different environmental conditions in which it lives that do not affect the ultrastructural pattern.
As defined by Lowenstam (1981), a biologically controlled biomineralization is recognized in organisms with extensive control over their mineral formation, resulting in well-ordered mineral structures with minor size variations and species-specific crystal habits, as we detected in L. corallioides. Despite some analogies with the observations of Nash et al. (2019), our findings demonstrate that the biomineralization process in CCA is biologically controlled (Borowitzka, 1984; Cabioch and Giraud, 1986) rather than induced (de Carvalho et al., 2017; Nash et al., 2019). The two additional samples, L. minervae and L. valens, show distinct styles of PW calcification, and this is extremely interesting for its application in Paleontology. Ultrastructures and ultrastructural pattern possibly represent a powerful tool for morphological species identification. Further investigation is needed to clarify the validity of this hypothesis in other genera and species.
Finally, the occurrence of calcite in the form of dogtooth crystals filling the cell lumen (Fig. 8b, c, e) is an exceptional finding. The voids of the cell lumens allowed for the development of calcite crystals which in terms of shape, size and pattern are completely different from the original ones forming the cell wall calcification. It represents a form of extremely early alteration, possibly diagenesis, in collections that were alive at the time of sampling. The phenomenon of earliest diagenesis, as already observed in Holocene and live Scleractinia corals (Nothdurft and Webb, 2008; Rashid et al., 2020), has implications in the reliability of climate and paleoclimate studies based on geochemical techniques and also when applied to recent collections. Therefore, the possible occurrence of dog-tooth calcite must be carefully checked when selecting coralline algae samples for geochemical investigations.
We define the cell wall ultrastructural pattern of L. corallioides as follows:
perithallus with evident banding as the result of the alternation of series of short-squared and long ovoid/rectangular cells;
epithallus with one to three flared cells;
same and consistent ultrastructural pattern of the cell walls both in perithallus and epithallus, with PW and SW calcite walls always present;
PW characterized by rectangular tiles;
SW characterized by flattened squared bricks with roundish outlines;
long and short cells with similar diameter and with different thickness of the PW and SW, resulting mainly in a thicker PW and SW in short cells.
The variable cell elongation, decreasing according to depth and producing an evident banding, never affects the ultrastructural pattern that maintains the same arrangement also under different growth rates. These findings demonstrate that the CCA calcification process seems to be biologically controlled rather than induced. The comparison with other Lithothamnion species highlights differences in the mineralization pattern of PW. Therefore, the ultrastructure of the cell wall in CCA results in a promising new diagnostic tool for species identification with important potential applications in paleontology. Lastly, an early alteration phenomenon, at the scale of ultrastructures, has been identified for the first time in living coralline algae.
All data of this study are available in this text and in the Supplement.
The supplement related to this article is available online at: https://doi.org/10.5194/bg-18-6061-2021-supplement.
VAB conceived the research, conducted SEM observations, interpreted the results, and wrote and revised the manuscript. DB conceived the research, and wrote and revised the manuscript. GP conducted the statistical analyses and prepared Figs. 4 and 9.
The contact author has declared that neither they nor their co-authors have any competing interests.
Publisher’s note: Copernicus Publications remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
We are grateful to two anonymous reviewers for their fruitful comments on the manuscript. Agostino Meroni is thanked for the extraction of temperature values. For the sample from Pontine Islands, the captain, crew and scientific staff of RV Minerva Uno cruise Strategia Marina Ligure-Tirreno are acknowledged for their efficient and skillful cooperation at sea. The sample from Capo Carbonara has been collected in the framework of the agreement between the University of Milano-Bicocca and the Marine Protected Area of Capo Carbonara for the realization of the monitoring activities of the Marine Strategy Framework Directive.
Giulia Piazza is funded by a doctoral fellowship in Environmental Sciences of the Milano-Bicocca University.
This article is a contribution to the Project MIUR-Dipartimenti di Eccellenza 2018–2022 DISAT-UNIMIB.
This paper was edited by Hiroshi Kitazato and reviewed by two anonymous referees.
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