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Article

Chemical Composition and Microstructural Morphology of Spines and Tests of Three Common Sea Urchins Species of the Sublittoral Zone of the Mediterranean Sea

by
Anastasios Varkoulis
1,*,†,
Konstantinos Voulgaris
1,*,†,
Stefanos Zaoutsos
2,
Antonios Stratakis
3 and
Dimitrios Vafidis
1
1
Department of Ichthyology and Aquatic Environment, Nea Ionia, University of Thessaly, 38445 Volos, Greece
2
Department of Energy Systems, University of Thessaly, 41334 Larisa, Greece
3
School of Mineral Resources Engineering, Crete Technical University of Crete, 73100 Chania, Greece
*
Authors to whom correspondence should be addressed.
†
These authors contributed equally to this work.
Animals 2020, 10(8), 1351; https://doi.org/10.3390/ani10081351
Submission received: 19 June 2020 / Revised: 31 July 2020 / Accepted: 2 August 2020 / Published: 4 August 2020
(This article belongs to the Special Issue Marine Animal Population Genetics and Conservation)
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Abstract

:

Simple Summary

Arbacia lixula, Paracentrotus lividus and Sphaerechinus granularis play a key role in many sublittoral biocommunities of the Mediterranean Sea. However, their skeletons seem to differ, both morphologically and in chemical composition. Thus, the skeletal elements display different properties, which are affected not only by the environment, but also by the vital effect of each species. We studied the microstructural morphology and crystalline phase of the test and spines, while also examining the effect of time on their elemental composition. Results showed morphologic differences among the three species both in spines and tests. They also seem to respond differently to possible time-related changes. The mineralogical composition of P. lividus appears to be quite different compare to the other two species. The results of the present study may contribute to a better understanding of the skeletal properties of these species, this being especially useful in predicting the effects of ocean acidification. More specifically, since the skeleton plays a key role for the survival of sea urchins in general, a potential change in any skeletal structure, either morphologically or chemically, may affect these organisms directly while also affecting their ecosystem indirectly.

Abstract

In the Mediterranean Sea, the species Arbacia lixula, Paracentrotus lividus and Sphaerechinus granularis often coexist, occupying different subareas of the same habitat. The mechanical and chemical properties of their calcitic skeletons are affected both by their microstructural morphology and chemical composition. The present study describes the main morphologic features and the possible temporal differences in elemental composition of the test and spines of the three species, while also determining the molar ratio of each element of their crystalline phase. Scanning electron microscopy showed major differences in the ultrastructure of the spines, while minor differences in the test were also noticed. More specifically, the spines of all three sea urchins possess wedges, however A. lixula exhibits bridges connecting each wedge, while barbs are observed in the wedges of S. granularis. The spines of P. lividus are devoid of both microstructures. Secondary tubercles are absent in the test of A. lixula, while the tests and spines of all three species are characterized by different superficial stereom. Energy dispersive x-ray spectroscopy detected that Ca, Mg, S, Na and Cl were present in all specimen. Mg and Mg/Ca showed significant differences between species both in test and spines with S. granularis having the highest concentration. The spines of P. lividus exhibited lowest values between all species. Differences between spines and test were observed in all elements for P. lividus except S. A. lixula exhibited different concentrations between test and spines for Ca, Mg and Mg/Ca, whereas S. granularis for Mg, Cl and Mg/Ca. Finally, temporal differences for Ca were observed in the test of P. lividus and the spines of S. granularis, for Mg in test of S. granularis, for S in the spines of A. lixula and the test and spine of S. granularis, for Na in the test of P. lividus and A. lixula and for Cl and Mg/Ca in the test P. lividus. Powder X-ray diffractometry determined that, out of all three species, the spines of P. lividus contained the least Mg, while the test of the same species exhibited higher Mg concentration compared to A. lixula and S. granularis. The current study, although not labeling the specimens attempts to estimate potential time-related elemental differences among other results. These may occur due to changes in abiotic factors, probably water temperature, salinity and/or pH. Divergence in food preference and food availability may also play a key role in possible temporal differences the skeletons of these species

1. Introduction

Biomineralization in marine invertebrates is a rather common phenomenon, where organisms produce minerals in order to enhance, strengthen and support existing tissue (i.e., teeth, shells, spines). These biominerals tend to have different properties in comparison to their abiotic counterparts [1]. The skeleton of echinoderms is primarily made up of Mg-rich calcite [(Mg, Ca)(CO3)], with small amounts of stable amorphous calcium carbonate (ACC), water and intra-crystalline organic molecules [2]. In contrast to other invertebrates, echinoderms possess a skeleton, which generally contains interconnecting cavities and much open space [3]. This is most noticeable when observing the test and spines of sea urchins.
Sea urchins are also considered drivers of the ecosystem and are important grazers in many sublittoral communities [4,5,6,7,8]. They can remove seagrass meadows and kelp forests, turning them into coralline barrens and thus play an important role in shaping the structure and functioning of many benthic marine biomes, especially rocky-reef ecosystems [9,10]. In the Mediterranean Sea, Paracentrotus lividus (Lamark, 1816), Arbacia lixula (Linnaeus, 1758) and Sphaerechinus granularis (Lamark, 1816) are some of the most common sea urchin species, often coexisting in the same habitat. It has been shown that the grazing activity of these three species can actually alternate the type of an ecosystem both separately and combined [11,12,13,14]. However, not only do they utilize different defensive adaptations, they also have different ecological and biologic features.
The lightweight property of the test originates from the fenestrated structure and relatively high porosity [15]. Thus, it would be thought that the dome shaped structure combined with the single- crystal calcite would make the test rather weak. However, it is far stronger than expected, because of the organic nature of biominerals. It is in fact many times stronger than calcareous rocks and mollusk shells [13]. Normal calcite is extremely brittle, in contrast to the strength to weight ratio of biomineralized calcite in sea urchins, which is by far higher compared to any other type of calcite [16,17].
The main weakness of a high-magnesium (Mg) calcite endoskeleton is that it may be vulnerable to CO2-driven ocean acidification, however there are studies that support that the epidermis and structural properties of the crystal can mitigate these effects [18,19,20]. The solubility of Mg-calcite increases with increase of Mg content in the crystal [21,22,23]. Calcite that contains more than approximately 12% weight fraction MgCO3 is considered more soluble than aragonite [20]. Since the sea urchin skeleton is rich in Mg2+ content, which in turn is responsible for the high solubility of the mineral form [20,23,24], sea urchins are likely to be particularly vulnerable to the effects of ocean acidification. The fact that the skeletal elements (test, teeth, etc.) play a key role [24,25,26,27], in the survival of sea urchins could make this taxon even more susceptible to the effects of ocean acidification, since it may increase the pressure of predation on these organisms.
It is reported that depending on the environment and other factors such as the vital effect, different species have different Mg concentrations. For example, Lytechinus variegatus and Heterocentrotus mammilatus being warm water species, have a higher amount of Mg substituted for Ca into their skeletal parts in the range of 4 mol% to 10 mol%, while cold water species, like the extreme example Sterechinus antarcticus, have only about 2 mol% to 3 mol% Mg content [28]. However, the Mg content of different skeletal elements of the same species also varies. For example, the Mg concentration of the test of L. variegatus ranges from 9.6 wt% to 11.3 wt% MgCO3, while the spines of the same species only contain 5.5 wt% to 8.3 wt% MgCO3. Finally, the mouth parts of the same species exhibit Mg concentrations of 8.3 wt%–13.4 wt% MgCO3 [16,23,29,30,31,32].
All three species utilize their test and spines as their main defensive skeletal structures, but their shape and chemical composition differ. Thus, their tolerance against the effects of ocean acidification may vary. The aim of the present study is to determine test and spines chemical composition of these three common Mediterranean species. This will help to indirectly evaluate the extent of vulnerability to ocean acidification for the skeleton of each species, but, more important, to assess the danger, that climate change poses, regarding the sublittoral benthic communities of the Mediterranean.

2. Materials and Methods

2.1. Sampling Site and Study Period

The study was performed on three species of sea urchins, namely, Paracentrotus lividus (Lamarck, 1816), Sphaerechinus granularis (Lamarck, 1816) and Arbacia lixula (Linnaeus, 1758) and took place in the Gulf of Pagasitikos, which is located in the central-western region of the Aegean Sea. It is a semi -enclosed shallow water basin (mean depth is 69 m) in which the water masses are cold and homogeneous in winter (12.6 °C) and highly stratified in the summer (27.5 °C) [32]. In the sampling area (Agios Stephanos 39°18’12.7” N 22°56’26.7” E) the seabed consists mainly of soft substrate with sparse meadows of Zostera marina (Linnaeus, 1753) and patches of rocks, dominated by communities of photophilic algae. Samples were collected seasonally (November 2017, February 2018, May 2018 and August 2018) by scuba diving at depths between 1 and 12 m. Concurrently, the seawater temperature and salinity was recorded monthly with an autographic conductivity temperature depth recorder, CTD (SeaBird, Bellevue, WA, USA), (Figure 1).

2.2. Microstructural Morphology and Elemental Analysis

Five individuals of each species from each sampling date were examined they were first dissected in order to acquire spines from the middle section of the interambulacral zones and interambulacral plates near the peristome. The plates and spines were then cleaned of internal organs using a 1% bleach treatment in distilled water for 30 min and dried at 60 °C for 3 days [33]. Specimens were coated in carbon by a Q150R Plus-rotary pumped coater carbon thread evaporator, reducing picture clarity in comparison to a gold coating, but enabling Energy-Dispersive X-Ray Spectroskopy (Figure 2). The samples were examined and imaged by SEM JEOL JSM 6510. For the cross-section of the spines, the middle part of the shaft was selected. Five observations for each species were carried out to determine the number of wedges. To study the chemical composition of the spines and tests, an EDS analysis was carried out by a JEOL JSM 6510 scanning electron microscope, equipped with an Oxford Link ISIS 300 system. Each measurement lasted 240 sec and was made in a 0.102 mm area. The characterization of the various stereom was carried out according to Smith, 1980.

2.3. X-ray Powder Diffraction Analysis

An X-ray diffraction analysis (XRD) of the studied samples was performed on a D8 Advance—BrukerAXS diffractometer using CuKα radiation in order to determine the crystalline phase both quantitatively and qualitatively. Interambulacral plates and spines from all individuals of each species were triturated in an agate mortar until a fine state (<40 μm). Afterwards 1 g of powder was placed in a standard cuvette and was mounted in the X-ray diffractometer. Measurements were carried out by a LynxEye detector with Ni-filter, operated at the voltage of 35 kV and the intensity of 35 mA, at a 2θ scanning range of 4–70°; analyses were made at a step of 0.02° and a speed of 0.2 s per step. The evaluation of data were carried out with the Diffracplus EVA–BrukerAXS software. Identification of the experimental data were performed by fitting the diffraction pattern using the JCPDS (joint committee on powder diffraction standard) database.

2.4. Statistical Analysis

Data of the elemental percentage compositions of each species were checked for normality (Kolmogorov–Smirnov) analysis of variance (one-way ANOVA) was used both for temporal elemental comparisons and for elemental comparison between species, followed by suitable post hoc tests (Tukey), where needed [34]. Data that did not follow a normal distribution or were not homogenous were analyzed by the Kruskal–Wallis one-way-analysis. Significant differences were further examined using post hoc tests (Dunn’s test). The variance of the group means for ANOVA (F value) and the variance of the group means for Kruskal–Wallis (H value) are reported together with the probability value (p), in order to give a more detailed observation regarding the variation among group means. For the elemental comparisons between tests and spines of each species Mann–Whitney U test was used. Statistical analyses were performed using the GraphPad Prism statistics software package (GraphPad Prism 5.0, GraphPad Software, San Diego, CA, USA).

3. Results

3.1. Morphology of Tests and Spines

3.1.1. Arbacia Lixula

The black sea urchin is usually attached on rocks or other hard substrate and does not use any type of cover (Figure 3a). Externally the spines are made of radial and longitudinal dense wedges, also called septa, which encircle the inner central stereom. The wedges are connected with each other via another type of skeletal microstructure called bridges (Figure 3b). The cross-section of the spine is a single layer of wedges along the inner surface, while the rest of the area is covered by the porous zone. The inner stereom of the spines of A. lixula seems to be of labyrinthic type, with irregular meshwork, while the outer cortex consists of solid imperforate stereom without pores (Figure 3c). The plates of the test bear the primary tubercles, where the base of the primary spines fit, like a ball—socket joint. Secondary tubercles seem to be absent in this species. As Smith (1980) [15] noted the outer surface of the plate is covered by a well-developed, compact, perforate stereom layer. Most of the pores, which are cylindrical shaped, seem to be located perpendicularly to the surface, thus the superficial stereom layer is characterized as mainly simple perforate (Figure 3d). The perforate stereom layer generally is a fairly thick layer, usually thicker than the average maximum diameter of the pores that perforate it and the main characteristic is that the pores are unbranched and mainly perpendicular to the surface, as in the case of the outer stereom surface of A. lixula.

3.1.2. Paracentrotus Lividus

The purple sea urchin is typically found on hard substrate (e.g., rocks), where it covers itself with various materials (e.g., pebbles, mollusk shells, etc.) by holding them between its spines (Figure 4a). The wedges of the spine seem to be very close to each other, with very little to no gap in between. Furthermore, no skeletal microstructures are observed on the wedges, which are in turn smooth in texture (Figure 4b). On the transverse view, the 17 triangular wedges seem to take up all the inner space of the spine, while the porous zone seems to be relatively limited (Figure 4c). Multiple tubercles are visible on the plates of the test, where the spines are attached with a ball–socket type connection, while secondary tubercles seem to cover much of the free space of the test. The outer surface of the test is covered by a thin layer of unorganized mesh of trabeculae, which forms a dense labyrinthic stereom. It appears as a three-dimensional tangle of interconnected trabeculae. These trabeculae are rather thick, while all intersections have prominent thorns. (Figure 4d). The labyrinthic stereom is the main architectural design used by most echinoids. The primary characteristic is the isotropic arrangement of the trabeculae, which ensures that the stereom is equally strong in all directions.

3.1.3. Sphaerechinus Granularis

The violet sea urchin is typically found on soft substrate (e.g., sand), many times concealed in algal meadows, camouflaging itself with soft materials like leaves or algae (Figure 5a). The inner stereom of the spines is surrounded by wedges, which are characterized by rough surface, where rows of 3–5 barbs can be distinguished (Figure 5b). The transverse view unveils the porous zone, which is encircled inside the rectangular wedges. The outer stereom seems to process parallel galleries running in one direction and no pore alignment is parallel to this direction. These galleries can be characterized as parallel trabeculae rods interconnected with struts. The inner stereom consists of “tube-like” structures with seemingly equally arranged pores. The surface is perforated by numerous closely spaced pores with a relatively large diameter. Thus, the superficial layer of the stereom seems to be composed of the radiating layer is galleried, whereas the medulla is laminar. There are 32 wedges around the porous zone, which extend over half of the inner surface of the spine, forming four concentric layers (Figure 5c). The plates of the test contain tubercles where the spines are attached, while secondary tubercles are also visible. The outer layer of the plate consists of a mesh of trabeculae, which creates a perforate stereom layer between tubercles. This layer seems to be thicker than the diameter of the pores, which perforate it. The pores are circular shaped and irregularly arranged. Since they are sinuous and branched an irregular perforate stereom occurs (Figure 5d).

3.2. Elemental Analysis

3.2.1. Calcium

Statistical differences between test and spines were observed in A. lixula (p = 0.03) and P. lividus (p = 0.0003), with the spines containing higher concentrations of calcium. Ca concentrations between test and spine showed no differences for S. granularis.

Spines

Comparison between species showed statistical differences between P. lividus and the other two species (Kruskal–Wallis H test, H = 13.767, p = 0.001) (Table 1). Temporal differences in the Ca content of the spines were only observed in S. granularis (F = 3.553, p = 0.038). Highest values occurred in samples collected in summer (45.88 wt% ± 2.28 wt%), while lowest in autumn (34.23 wt% ± 9.5 wt%) (Table 2; Figure 6). The spines of both A. lixula and P. lividus showed no significant temporal differences.

Test

No statistical differences were observed in the Ca content between the three species (Table 1). The test of P. lividus, exhibited significantly lower values in Autumn (F = 9.036, p = 0.001), compared to all others with a value of 21.09 wt% ± 16.89 wt% (Table 2; Figure 6). No temporal differences were observed in Ca of the test for A. lixula and S. granularis.

3.2.2. Magnesium

The tests of all species showed significantly more Mg content compared to the spines (p = 0.0001 for all species).

Spines

The Mg content of spines was significantly different among the three species (Kruskal–Wallis H test, H = 39.674, p = 0.0001). P. lividus exhibited significantly lower values compared to the other two species with a value of 0.31 wt% ± 0.09 wt% (Table 1). No statistical differences were observed in the temporal concentrations of the three species (Table 2; Figure 6).

Test

The three species exhibited significant differences in Mg content (Kruskal–Wallis H test, H = 8.19, p = 0.0168). Highest values were observed in the test of S. granularis (2.44 wt% ± 0.6 wt%) and lowest in P. lividus (2.15 wt% ± 0.66 wt%). Temporal differences occurred only for S. granularis (F = 6.206, p = 0.0053) (Table 2). More specifically, samples collected in autumn exhibited lower values (1.72 wt% ± 0.73 wt%) compared to the others (Figure 6). A. lixula and P. lividus showed no temporal differences regarding the Mg content in the test.

3.2.3. Sulfur

The spines seem to have higher S concentrations compared to the tests in all three species (A. lixula, p = 0.025; P. lividus, p = 0.017; S. granularis, p = 0.0001).

Spines

No significant differences were observed among the three species (Table 1), while temporal differences occurred in A. lixula (F = 4.847, p = 0.013) and S. granularis (F = 11.311, p = 0.01) (Table 2). Lowest values for A. lixula were observed in samples collected during winter (0.51 wt% ± 0.11 wt%), while highest occurred in autumn (1.002 wt% ± 0.17 wt%). S. granularis showed lowest S concentrations during samples collected in winter (0.49 wt% ± 0.05 wt%) and highest during summer (0.76 wt% ± 0.06 wt%) (Figure 6). P. lividus exhibited no significant temporal differences.

Test

The three species showed no statistical differences regarding the S concentration in their tests. Temporal differences were observed only in S. granularis (Kruskal–Wallis H test, H = 8.056, p = 0.044) with lowest values occurring during the sample collection winter (0.32 wt% ± 0.1 wt%) and highest during spring (0.54 wt% ± 0.05 wt%) (Table 2; Figure 6). No significant temporal differences were observed in the S content of the test of A. lixula and P. lividus.

3.2.4. Sodium

Statistical differences between test and spines were only observed in P. lividus (p = 0.002) with the test containing higher Na concentration than the spine. No significant differences were observed among the three species regarding both the tests and spines (p = 0.57).

Spines

There were no significant temporal differences in the Na concentration of the spines of all three species (Table 2; Figure 6).

Test

Temporal differences occurred both in A. lixula (F = 3.546, p = 0.03) and P. lividus (F = 11.368, p = 0.0003) (Table 2). A. lixula exhibited higher values (3.45 wt% ± 2.22 wt%) in the samples that were collected in winter compared to the others. Post hoc test showed that highest values for P. lividus occurred during autumn sampling (2.79 wt% ± 1 wt%) (Figure 6), while no significant differences were observed among the other sampling periods. S. granularis showed no significant temporal differences in the Na concentration of the test.

3.2.5. Chlorine

P. lividus (p = 0.0001) and S. granularis (p = 0.0002) showed statistical differences between test and spines, with the test exhibiting higher concentrations compared to the spines in both species, while Cl content of A. lixula did not vary between test and spines. No significant differences were observed between species in the spines (p = 0.13) or the test (p = 0.09) (Table 1).

Spines

No significant differences were observed in the three species regarding the temporal effects. (A. lixula: F = 1.503, p = 0.25; P. lividus: Kruskal–Wallis H test, H = 3.387, p = 0.33; S. granularis: Kruskal–Wallis H test, H = 0.42, p = 0.93) (Table 2; Figure 6).

Test

P. lividus was the only species that showed significant temporal differences (F = 16.404, p = 0.0001) (Table 2). Higher values were recorded in samples collected during autumn (3.06 wt% ± 1.11 wt%) compared to all others (Figure 6). A. lixula and S. granularis exhibited no temporal differences regarding the Cl concentration of the test.

3.2.6. Mg/Ca Ratio

The Mg/Ca ratio was significantly higher in the tests of all three species compared to the spines (A. lixula, p = 0.0001; P. lividus, p = 0.0001; S. granularis, p = 0.0001).

Spines

Significant differences were observed among the three species (Kruskal–Wallis H test, H = 40.538, p = 0.0001) (Table 1). P. lividus exhibited lowest values compared to the other two species, with a value of (0.006 wt% ± 0.002 wt%). No temporal differences were observed for all species (Table 2; Figure 6).

Test

The Mg/Ca ratio varied significantly among the three species (Kruskal–Wallis H test, H = 6.08, p = 0.047) (Table 1). More specifically, statistical differences were observed between A. lixula (0.054 wt% ± 0.005 wt%) and S. granularis (0.066 wt% ± 0.025 wt%), but not between P. lividus and the other two species. Temporal differences occurred only in P. lividus (F = 12.576, p = 0.0002) (Table 2). Highest values were observed during the samples that were collected in autumn (0.08 wt% ± 0.01 wt%), compared to the other three s (Figure 6). No significant temporal differences were observed in the Mg/Ca ratio of the test of A. lixula and S. granularis.

3.3. X-ray Powder Diffraction

The phase composition of the samples is given in Table 3. It was shown that all the spines and tests of all three species consist of some form of magnesian calcite and a small percentage of halite (NaCl) (Figure 7, Table 3). A. lixula and S. granularis had roughly the same quantities of magnesium in their crystalline phases both in the spine and the test. P. lividus had the highest values of magnesium in the test and the lowest in the spine, more specifically double the amount of magnesium was found in the test of P. lividus, whereas half of it was found in the spines, compared to A. lixula and S. granularis. Halite took up 3% of the composition of all samples except for the spines of S. granularis, which consisted of 4% NaCl.

4. Discussion

The three investigated species are commonly found in the Mediterranean Sea, often coexisting in the same habitat [35]. However, S. granularis was mainly found in soft substrate in contrast to A. lixula and P. lividus, which were attached on hard substrates (mainly rocks) (Figure 3a, Figure 4a, Figure 5a). Various morphologic differences were observed regarding their ultrastructure, both in their spines and tests. The spines of P. lividus seem to be deprived of any skeletal microstructures (e.g., bridges, barbs) and are characterized by a smooth texture, whereas both other sea urchins are acquired with spines, which are characterized by rough textures due to bridges between wedges (A. lixula) and barbs (S. granularis). The spines of P. lividus are also shown to be the most compact with the wedges located very close to each other, whereas the wedges of A. lixula and S. granularis are more distant (Figure 3b, Figure 4b, Figure 5b). Observing the cross- section of the spines the main difference is that the porous zone seems to be relatively narrow in P. lividus. Since the sections of all spines were taken from the middle of the shaft, the porous zone may change in terms of surface width in different regions of the spine. Lauer et al. (2017) [36] concluded that the porosity of the spine increases from base to tip. The fact that the present study reported a very limited porous zone in the spine of P. lividus may be related to the fact that the cross section was taken from the middle of the shaft. It may occupy a wider area towards the tip. A. lixula the least number of wedges (14–15), followed by P. lividus (17), with S. granularis having the most and narrowest wedges (32) (Figure 3c, Figure 4c, Figure 5c). Note that the samples may still be filled with organic tissue which is most visible of the cross section of the spine of A. lixula. A. lixula was the only species that showed variety in the measurements of the number of wedges. A. lixula exhibited an outer imperforated cortex with an inner labyrinthic stereom regarding the spines. The cross-section of the spines of S. granularis showed two types of stereom, an outer galleried and an inner laminar stereom. Finally, the tests of the three sea urchins differ from one another, in that P. lividus and S. granularis present lines of secondary tubercles, which are absent in the test of A. lixula. In addition, when viewed in higher magnifications, different structures of stereom are visible (Figure 3d, Figure 4d, Figure 5d).
Such morphologic characteristics may play a role in the differentiation of the mechanical properties of the skeletons of the three species, since they change the structure and shape of both the test and spines the superficial surface of the plates of both A. lixula and S. granularis are characterized of perforate stereom. Wainwright et al. (1976) [37] showed that this type of stereom increases the resistance of the plate to bending stress. Another important function of this stereom is the increased protection against surface abrasion [15]. On the other hand, P. lividus exhibited a type of dense labyrinthic stereom. The labyrinthic stereom is the main architectural design used by most echinoids. The primary characteristic is the isotropic arrangement of the trabeculae, which ensures that the stereom is equally strong in all directions. Regarding the spines Grossmann and Nebelsick 2013 [38], report that the advantage of laminar stereom in the spines is that it has a low density and thus can be constructed relatively quickly compared to other types. They also concluded that the more chaotic distribution of struts in the labyrinthic stereom may serve to hinder the proliferation of cracks. Lastly in the spines of the three investigated species the septa seem to be the ones responsible for the mechanical stiffness while the porous zone towards the center of the spine is characterized of lower mechanical quality [39]. Mechanical tests with regard to the microstructural morphology should be carried out in order to better estimate the role of stereom differentiation in sea urchins. EDS analysis showed that spines and test are mainly composed of the same elements, but in different concentrations (Table 1; Figure 2). P. lividus exhibited significant differences between test and spines in all element concentrations except for S. A. lixula showed significant differences between the two investigated skeletal structures in Ca, Mg and Mg/Ca and S. granularis in Mg, Cl, Mg/Ca. Differences in the elemental concentrations between species occurred in Mg and Mg/Ca ratio both in the spines and tests while the only other significant differences were shown to be in Ca concentrations of the spines (Table 2). Possible temporal variations of the elemental concentrations were also observed, mostly in the test of P. lividus in Ca, Na, Cl and the Mg/Ca ratio. The spines of the same species showed to significant temporal differences. Regarding A. lixula significant differences were recorded in Na in the test and in S in the spines. Finally, the test of S. granularis exhibited different temporal concentrations in Mg and S, while the spines in Ca and S.
Changes in the chemical elements affected by time may be explained by various reasons, such as changes in abiotic factors (e.g., temperature, salinity, etc.), time-related diet changes or a combination of them. Hermans et al. (2011) [40] concluded that Mg/Ca ratio in the skeleton of sea urchins is defined by salinity levels, while also regulated by the presence of intrastereom organic matrix. Byrne et al. (2014) [33] showed that temperature also alters the Mg content in the skeleton of sea urchins. Kobuk et al. (2019) [41] showed that the Mg/Ca ratio is also regulated by food intake. P. lividus, being an opportunistic generalist, utilizes apostatic feeding, which allows it to switch from a preferred, but rare resource to a less preferred, but abundant one [42]. The same pattern may be true to a lesser extent for S. granularis, while A. lixula seems to have the most stable elemental composition throughout time. Finally, according to Hermans et al. (2011), the interstereom organic matrix seems to largely account for the fact that spines and tests have different elemental compositions.
As Figure 1 suggests, temperature in the selected sampling site reached highest values in summer, but also in September, while salinity apparently followed an antiproportional pattern, with lowest values recorded in summer. Since the elemental composition of the spines and tests of the investigated species does not follow a trend similar to temperature or salinity, it is indicated that other factors (e.g., vital effect, dietary preferences, etc.) also play key role. To explain the possible temporal differences in elemental composition observed in these species, more factors must be taken into account. Thus, further research should be conducted in order to shed more light in to how the chemical composition of the skeletons of these species changing according to time and also in to why P. lividus shows more variety in the elemental composition between test and spine, compared to the other two species (Table 1).
XRD analysis showed that the tests of S. granularis and A. lixula consist of the same form of magnesian calcite, whereas P. lividus seems to have twice the amount of Mg in the test. The spines of P. lividus are made up of a Mg-calcite with a lesser amount of magnesium compared to the spines of the other two species, more specifically about two times less (Table 3, Figure 7). Drozdov et al. (2016) [27] reported the presence of halite in the crystal of the skeleton of sea urchins in concentrations of 1% to 2%. The present study also reports the same mineral in concentrations of 3%–4%, however under no circumstances does this prove the biomineralization of halite by echinoderms. It is likely that this result occurred due to contamination (impurity from sea water, sample treatment with NaClO, etc.). Ma et al. (2009) [43] showed that Mg content in the grinding tooth increases towards the tip, and they hypothesized that higher Mg content enhances the mechanical hardness of the calcite. However, the hardness of the calcite is not the only factor affecting the durability of the skeleton under mechanical pressure. Microstructural features also play a significant role in the tenacity of the skeletal elements under tension. Mg content, however, also increases the solubility of the Mg-calcite [20,44,45,46]. This is the main reason organisms like sea urchins, which are now mainly relying on their mechanically durable, Mg-rich calcitic skeleton, may face the heaviest consequences of the ocean acidification effects. Elemental analysis showed that the tests have a higher Mg:Ca ratio than the spines, which may make the test more vulnerable to dissolution due acidification. Furthermore, EDS results showed that S. granularis has the highest Mg concentrations both in the test and the spine, while also having the highest Mg:Ca ratio in both skeletal structures. However, XRD results determined that the test of P. lividus has the highest content of Mg in the calcite. In both methods the spine of P. lividus was found to have the lowest percentage of Mg. It should be noted that the difference between the results of XRD and EDS analysis is to be expected, since the first method deals only with the concentrations of Mg and Ca in the compound biomineral (Mg-CaCO3), while the latter describes the concentration of the chemical elements in the investigated skeletal parts in general. However, live sea urchins utilize their physiology in order to adapt to different environmental conditions, which means that Mg content in the calcite alone is not a valid indicator to assess the effects of ocean acidification [18]. In any case ocean acidification effects will vary with species. The absence of urchins around some vent sites (pH 7.6–7.8), indicates that this level of acidification may prevent survival of sea urchins potentially due to vulnerability of a weaker skeleton to predation. However, this trend differs among sea urchin species as shown in a recent study where Arbacia lixula was particularly abundant at vent sites, while Paracentrotus lividus was not [47,48,49].

5. Conclusions

Morphologic differences in the skeletal elements of the three species hint to different mechanical properties. P. lividus seems to be more affected by time-related changes, compared to the other two species. Mg is the only element, which was never affected by time, in all three species. The lowest Mg content was founded in the spines of P. lividus ranging from 0.22% to 0.4%. The solubility of Mg-rich calcite increases with higher concentration of Mg, which could mean that the spine of P. lividus is the least vulnerable skeletal element, while the test may be the most susceptible to ocean acidification. These observations may play a decisive role for the balance of the ecosystems, where these species coexist. However, more research must be conducted to evaluate how ocean acidification will affect the Mediterranean sublittoral benthic ecosystems. It should be noted that the experiments in the present study were not conducted with regard to seasonal growth since the specimens were not labeled. Thus, the results are preliminary and do not determine the effect of seasonality. More research should be conducted in order to estimate the effects of season in the chemical composition of the skeleton of the investigated species.

Author Contributions

Conceptualization, A.V., K.V. and D.V.; methodology, A.V., K.V., S.Z. and A.S.; software, A.V. and K.V.; formal analysis, D.V.; data curation, A.V. and K.V.; writing—original draft preparation, A.V. and K.V.; writing—review and editing, A.V., K.V. and D.V.; visualization, D.V.; supervision, D.V. All authors have read and agreed to the published version of the manuscript.

Funding

This research was not funded.

Conflicts of Interest

The authors declare no conflicts of interest.

References

  1. Lowenstam, H.A.; Weiner, S. On Biomineralization; Oxford University Press: New York, NY, USA, 1989. [Google Scholar]
  2. Seto, J.; Ma, Y.R.; Davis, S.A.; Meldrum, F.; Gourrier, A.; Kim, Y.Y.; Schilde, U.; Sztucki, M.; Burghammer, M.; Maltsev, S.; et al. Structure-property relationships of a biological mesocrystal in the adult sea urchin spine. Proc. Natl. Acad. Sci. USA 2012, 109, 3699–3704. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  3. Su, X.; Kamat, S.; Heuer, A.H. The structure of sea urchin spines, large biogenic single crystals of calcite. J. Mater. Sci. 2000, 35, 5545–5551. [Google Scholar] [CrossRef]
  4. Lawrence, J.M. On the Relationships between Marine Plants and Sea Urchins. In Oceanography and Marine Biology; CRC press: Boca Raton, FL, USA, 1975. [Google Scholar]
  5. Tegner, M.J.; Dayton, P.K. Sea urchin recruitment patterns and implications of commercial fishing. Science 1977, 196, 324–326. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  6. Sala, E.; Boudouresque, C.F.; Harmelin-Vivien, M. Fishing, trophic cascades, and the structure of algal assemblages: Evaluation of an old but untested paradigm. Oikos 1998, 82, 425–439. [Google Scholar] [CrossRef]
  7. Tsirintanis, K.; Sini, M.; Doumas, O.; Trygonis, V.; Katsanevakis, S. Assessment of grazing effects on phytobenthic community structure at shallow rocky reefs: An experimental field study in the North Aegean Sea. J. Exp. Mar. Biol. Ecol. 2018, 503, 31–40. [Google Scholar] [CrossRef]
  8. Bonaviri, C.; Vega Fernández, T.; Fanelli, G.; Badalamenti, F.; Gianguzza, P. Leading role of the sea urchin Arbacia lixula in maintaining the barren state in southwestern Mediterranean. Mar. Biol. 2011, 158, 2505–2513. [Google Scholar] [CrossRef]
  9. Shears, N.T.; Babcock, R.C. Marine reserves demonstrate top-down control of community structure on temperate reefs. Oecologia 2002, 132, 131–142. [Google Scholar] [CrossRef]
  10. Guidetti, P.; Terlizzi, A.; Boero, F. Effects of the edible sea urchin, Paracentrotus lividus, fishery along the Apulian rocky coast (SE Italy, Mediterranean Sea). Fish. Res. 2004, 66, 287–297. [Google Scholar] [CrossRef]
  11. Vafidis, D.; Antoniadou, C.; Kyriakouli, K. Reproductive cycle of the edible sea urchin Paracentrotus lividus (E chinodermata: Echinoidae) in the Aegean Sea. Water 2019, 11, 1029. [Google Scholar] [CrossRef] [Green Version]
  12. Antoniadou, C.; Vafidis, D. Population structure and morphometric relationships of Paracentrotus lividus (Echinodermata: Echinoidae) in the south Aegean Sea. Cah. Biol. Mar. 2009, 50, 293–301. [Google Scholar]
  13. Bulleri, F. Grazing by sea urchins at the margins of barren patches on Mediterranean rocky reefs. Mar. Biol. 2013, 160, 2493–2501. [Google Scholar] [CrossRef]
  14. Agneta, D.; Badalmenti, F.; Ceccherelli, G.; Di Trapani, F.; Bonaviri, C.; Gianguzza, P. Role of two co-occurring Mediterranean sea urchins in the formation of barren from Cystoseira canopy. Estuar. Coast. Shelf Sci. 2015, 152, 73–77. [Google Scholar] [CrossRef] [Green Version]
  15. Smith, A.B. Stereom Microstructure of the Echinoid Test; Special Papers in Palaeontology: London, UK, 1980; pp. 1–81. [Google Scholar]
  16. Weber, J.; Greer, R.; Voight, V.; White, E.; Rustum, R. Unusual strength properties of echinoderm calcite related to structure. J. Ultrastruct. Res. 1969, 26, 355–366. [Google Scholar] [CrossRef]
  17. Weiner, S. Organization of extracellularly mineralized tissues: A comparative study of biological crystal growth. Crc. Crit. Rev. Biochem. 1986, 20, 365–408. [Google Scholar] [CrossRef]
  18. Dubois, P. The skeleton of postmetamorphic echinoderms in a changing world. Biol. Bull. 2014, 226, 223–236. [Google Scholar] [CrossRef] [Green Version]
  19. Emerson, C.E.; Reinardy, H.C.; Bates, N.R.; Bodnar, A.G. Ocean acidification impacts spine integrity but not regenerative capacity of spines and tube feet in adult sea urchins. R. Soc. Open Sci. 2017, 4, 170140. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  20. Andersson, A.J.; Mackenzie, F.T.; Bates, N.R. Life on the margin: Implications of ocean acidification on Mg-calcite, high latitude and cold-water marine calcifiers. Mar. Ecol. Prog. Ser. 2008, 373, 265–273. [Google Scholar] [CrossRef]
  21. Orr, J.C.; Fabry, V.J.; Yool, A. Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms. Nature 2005, 437, 681–686. [Google Scholar] [CrossRef]
  22. Dupont, S.; Dorey, N.; Thorndyke, M. What meta-analysis can tell us about vulnerability of marine biodiversity to ocean acidification? Estuar. Coast. Shelf Sci. 2010, 89, 182–185. [Google Scholar] [CrossRef]
  23. Smith, A.M.; Clark, D.E.; Lamare, M.D.; Winter, D.J.; Byrne, M. Risk and resilience: Variations in magnesium in echinoid skeletal calcite. Mar. Ecol. Prog. Ser. 2015, 561, 1–16. [Google Scholar] [CrossRef] [Green Version]
  24. Albéric, M.; Caspi, E.N.; Bennet, M.; Ajili, W.; Nassif, N.; Azaïs, T.; Berner, A.; Fratzl, P.; Zolotoyabko, E.; Bertinetti, L.; et al. Interplay between Calcite, Amorphous Calcium Carbonate, and Intracrystalline Organics in Sea Urchin Skeletal Elements. Cryst. Growth Des. 2018, 18, 2189–2201. [Google Scholar] [CrossRef] [Green Version]
  25. Albéric, M.; Stifler, C.A.; Zou, Z.; Sun, C.; Killian, C.E.; Valencia, S.; Mawass, M.; Bertinetti, L.; Gilbert, P.U.; Politi, Y. Growth and regrowth of adult sea urchin spines involve hydrated and anhydrous amorphous calcium carbonate precursors. J. Struct. Biol. 2018, 1, 100004. [Google Scholar] [CrossRef] [PubMed]
  26. Drozdov, A.L.; Sharmankina, V.V.; Zemnukhova, L.A.; Polyakova, N.V. Chemical composition of spines and tests of sea urchins. Biol. Bull. Russ. Acad Sci. 2016, 43, 521–531. [Google Scholar] [CrossRef]
  27. Kanold, J.M.; Guichard, N.; Immel, F.; Plasseraud, L.; Corneillat, M.; Alcaraz, G.; Brummer, F.; Marin, F. Spine and test skeletal matrices of the Mediterranean sea urchin Arbacia lixula- a comparative characterization of their sugar signature. FEBS J. 2015, 282, 1891–1905. [Google Scholar] [CrossRef] [PubMed]
  28. Magdans, U.; Gies, H. Single crystal structure analysis of sea urchin spine calcites: Systematic investigations of the Ca/Mg distribution as a function of habitat of the sea urchin and the sample location in the spine. Eur. J. Miner. 2004, 16, 261–268. [Google Scholar] [CrossRef]
  29. Bischoff, W.D.; Bishop, F.C.; Mackenzie, F.T. Biogenically produced magnesian calcite: Inhomogeneities in chemical and physical properties: Comparison with synthetic phases. Am. Mineral. 1983, 68, 1183–1188. [Google Scholar]
  30. Carpenter, S.J.; Lohmann, K.C. Ratios of modern marine calcite: Empirical indicators of ocean chemistry and precipitation rate. Geochim. Cosmochim. Acta 1992, 56, 1837–1849. [Google Scholar] [CrossRef] [Green Version]
  31. Chave, K.E. Aspects of the Biogeochemistry of Magnesium 1. Calcareous Marine Organisms. J. Geol. 1954, 62, 266–283. [Google Scholar] [CrossRef]
  32. Petihakis, G.; Triantafyllou, G.; Pollani, A.; Koliou, A.; Theodorou, A. Field data analysis and application of a complex water column biogeochemical model in different areas of a semi-enclosed basin: Towards the development of an ecosystem management tool. Mar. Environ. Res. 2005, 59, 493–518. [Google Scholar] [CrossRef]
  33. Byrne, M.; Smith, A.M.; West, S.; Collard, M.; Dubois, P.; Graba-Landry, A.; Dworjanyn, S.A. Warming Influences Mg2+ Content, While Warming and Acidification Influence Calcification and Test Strength of a Sea Urchin. Enviromental Sci. Technol. 2014, 48, 12620–12627. [Google Scholar] [CrossRef]
  34. Zar, J.H. Biostatistical Analysis, 5th ed.; Northern Illinois University: DeKalb, IL, USA, 2010. [Google Scholar]
  35. Martinez-Pita, I.; Sanchez-Espagna, A.I.; Garcia, F.J. Gonadal growth and reproduction in the sea urchin Sphaerechinus granularis (Lamarck 1816) (Echinodermata: Echinoidea) in Southern Spain. Sci. Mar. 2008, 72, 603–611. [Google Scholar]
  36. Lauer, C.; Grun, T.B.; Zutterkirch, I.; Jemmali, R.; Nebelsick, J.H.; Nickel, K.G. Morphology and porosity of the spines of the sea urchin Heterocentrotus mamillatus and their implications on the mechanical performance. Zoomorphology 2017, 137, 139–154. [Google Scholar] [CrossRef]
  37. Wainwright, S.A.; Biggs, W.D.; Currey, J.D.; Gosline, J.M. Mechanical Design in Organisms; Princeton University Press: Princeton, NJ, USA, 1976. [Google Scholar]
  38. Grossmann, J.N.; Nebelsick, J.H. Comparative morphological and structural analysis of selected cidaroid and camarodont sea urchin spines. Zoomorphology 2013, 132, 301–315. [Google Scholar] [CrossRef]
  39. Moureaux, C.; Pérez-Huerta, A.; Compère, P.; Zhu, W.; Leloup, T.; Cusask, M.; Dubois, P. Structure, composition and mechanical relations to function in sea urchin spine. J. Struct. Biol. 2010, 170, 41–49. [Google Scholar] [CrossRef]
  40. Hermans, J.; Borremans, C.; Willenz, P.; Andre´, L.; Dubois, P. Temperature, salinity and growth rate dependences of Mg/Ca and Sr/Ca ratios of the skeleton of the sea urchin Paracentrotus lividus (Lamarck): An experimental approach. Mar. Biol. 2010, 157, 1293–1300. [Google Scholar] [CrossRef]
  41. Kołbuk, D.; Dubois, P.; Stolarski, J.; Gorzelak, P. Effects of seawater chemistry (Mg2+/Ca2+ ratio) and diet on the skeletal Mg/Ca ratio in the common sea urchin Paracentrotus lividus. Mar. Env. Res. 2019, 145, 22–26. [Google Scholar] [CrossRef] [Green Version]
  42. Boudouresque, C.F.; Verlaque, M. Ecology of Paracentrotus lividus. In Edible Sea Urchins: Biology and Ecology; Lawrene, J.M., Ed.; Elsevier: Amsterdam, The Netherlands, 2001. [Google Scholar]
  43. Ma, Y.; Aichmayer, B.; Paris, O.; Fratzl, P.; Meibom, A.; Metzler, R.A.; Politi, Y.; Adaddi, L.; Gilbert, P.U.; Weiner, S. The grinding tip of the sea urchin tooth exhibits exquisite control over calcite crystal orientation and Mg distribution. Proc. Natl. Acad. Sci. USA 2009, 106, 6048–6053. [Google Scholar] [CrossRef] [Green Version]
  44. Walter, L.M.; Morse, J.W. Mg-calcite stabilities: A re-evaluation. Geochim. Cosmochim. Acta 1984, 48, 1059–1069. [Google Scholar] [CrossRef]
  45. Bischoff, W.D.; Mackenzie, F.T.; Bishop, F.C. Stabilities of synthetic Mg-calcites in aqueous solution: Comparison with biogenic materials. Geochim. Cosmochim. Acta 1987, 51, 1413–1423. [Google Scholar] [CrossRef]
  46. Morse, J.W.; Andersson, A.J.; Mackenzie, F.T. Initial responses of carbonate-rich shelf sediments to rising atmospheric pCO2 and “ocean acidification”: Role of high Mg-calcites. Geochim. Cosmochim. Acta 2006, 70, 5814–5830. [Google Scholar] [CrossRef]
  47. Asnaghi, V.; Chiantore, M.; Mangialajo, L.; Gazeau, F.; Francour, P.; Alliouane, S.; Gattuso, J.P. Cascading effects of ocean acidification in a rocky subtidal community. PLoS ONE 2013, 8, 61978. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  48. Hall-Spencer, J.M.; Rodolfo-Metalpa, R.; Martin, S.; Ransome, E.; Fine, M.; Turner, S.M.; Rowley, S.J.; Tedesco, D.; Buia, M.C. Volcanic carbon dioxide vents reveal ecosystem effects of ocean acidification. Nature 2008, 454, 96–99. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  49. Calosi, P.; Rastrick, S.P.S.; Graziano, M.; Thomas, S.C.; Baggini, C.; Carter, H.A.; Hall-Spencer, J.M. Distribution of sea urchins living near shallow water CO2 vents is dependent upon speciesacid−base and ion-regulatory abilities. Mar. Pollut. Bull. 2013, 73, 470–484. [Google Scholar] [CrossRef] [PubMed] [Green Version]
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Figure 1. Diagrams showing monthly variations of temperature (°C) and salinity (PSU) in the sampling site.
Figure 1. Diagrams showing monthly variations of temperature (°C) and salinity (PSU) in the sampling site.
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Figure 2. EDS spectra of A. lixula (a) test and (b) spine.
Figure 2. EDS spectra of A. lixula (a) test and (b) spine.
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Figure 3. Black sea urchin Arbacia lixula. (a) General in situ view of the aboral side; (b) longitudinal section of the shaft of the spine (×100), with enlarged image showing bridges connecting two wedges (×650); (c) transverse section of the spine (×160), with enlarged image showing the porous zone (×350); (d) section of the test from the peristomal region (×16), with enlarged image showing the stereom of the outer surface of the plate (×600). Br—bridges, Pt—primary tubercles.
Figure 3. Black sea urchin Arbacia lixula. (a) General in situ view of the aboral side; (b) longitudinal section of the shaft of the spine (×100), with enlarged image showing bridges connecting two wedges (×650); (c) transverse section of the spine (×160), with enlarged image showing the porous zone (×350); (d) section of the test from the peristomal region (×16), with enlarged image showing the stereom of the outer surface of the plate (×600). Br—bridges, Pt—primary tubercles.
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Figure 4. Purple sea urchin Paracentrotus lividus. (a) General in situ view of the aboral side; (b) longitudinal section of the shaft of the spine (×100), with enlarged image showing a wedge of the spine (×550); (c) transverse section of the spine (×100), with enlarged image showing the inner part of the spine. Notice that no porous zone is present; (d) section of the test from the peristomal region (×16), with enlarged image showing the stereom of the outer surface (×600). St—secondary tubercles; Pt—primary tubercles.
Figure 4. Purple sea urchin Paracentrotus lividus. (a) General in situ view of the aboral side; (b) longitudinal section of the shaft of the spine (×100), with enlarged image showing a wedge of the spine (×550); (c) transverse section of the spine (×100), with enlarged image showing the inner part of the spine. Notice that no porous zone is present; (d) section of the test from the peristomal region (×16), with enlarged image showing the stereom of the outer surface (×600). St—secondary tubercles; Pt—primary tubercles.
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Figure 5. The purple sea urchin Sphaerechinus granularis. (a) General in situ view of the aboral side; (b) longitudinal section of the shaft of the spine (×100), with enlarged image showing rows of barbs on a wedge (×1100); (c) transverse section of the spine (×140), with enlarged image showing the porous zone (×400); (d) section of the test from the peristomal region (×16), with enlarged image showing the stereom of the outer surface. Bar—barbs, Pt—primary tubercles, St—secondary tubercles.
Figure 5. The purple sea urchin Sphaerechinus granularis. (a) General in situ view of the aboral side; (b) longitudinal section of the shaft of the spine (×100), with enlarged image showing rows of barbs on a wedge (×1100); (c) transverse section of the spine (×140), with enlarged image showing the porous zone (×400); (d) section of the test from the peristomal region (×16), with enlarged image showing the stereom of the outer surface. Bar—barbs, Pt—primary tubercles, St—secondary tubercles.
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Figure 6. Temporal wt% concentrations of Ca, Mg, S, Na, Cl and Mg/Ca ratio in the spines and tests of the three species.
Figure 6. Temporal wt% concentrations of Ca, Mg, S, Na, Cl and Mg/Ca ratio in the spines and tests of the three species.
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Figure 7. Representative powder XRD pattern of test and spines of P. lividus.
Figure 7. Representative powder XRD pattern of test and spines of P. lividus.
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Table
Table 1. One-way ANOVA and Kruskal–Wallis results for the elemental concentrations of spines and tests between A. lixula, P. lividus and S. granularis. Significant differences (p < 0.05) are highlighted in bold. (F—variance of the group means for ANOVA; H—variance of the group means for Kruskal–Wallis; p: probability value).
Table 1. One-way ANOVA and Kruskal–Wallis results for the elemental concentrations of spines and tests between A. lixula, P. lividus and S. granularis. Significant differences (p < 0.05) are highlighted in bold. (F—variance of the group means for ANOVA; H—variance of the group means for Kruskal–Wallis; p: probability value).
Chemical ElementspF or H
CaTest0.5861H = 1.069
Spine0.001H = 13.767
MgTest0.0168H = 8.19
Spine0.0001H = 39.674
STest0.172H = 3.511
Spine0.3389F = 1.103
NaTest0.3323H = 2.204
Spine0.5761F = 0.5568
ClTest0.0952H = 4.705
Spine0.1356H = 3.996
Mg/CaTest0.047H = 6.08
Spine0.0001H = 40.538
Table
Table 2. Results of one-way ANOVA and Kruskal–Wallis test regarding the temporal variations of each element in the spines and test of A. lixula, P. lividus and S. granularis. Significant differences (p < 0.05) are highlighted in bold. (F—variance of the group means for ANOVA; H—variance of the group means for Kruskal–Wallis; p: probability value).
Table 2. Results of one-way ANOVA and Kruskal–Wallis test regarding the temporal variations of each element in the spines and test of A. lixula, P. lividus and S. granularis. Significant differences (p < 0.05) are highlighted in bold. (F—variance of the group means for ANOVA; H—variance of the group means for Kruskal–Wallis; p: probability value).
Chemical ElementsA. lixulaP. lividusS. granularis
pF or HpF or HpF or H
CaTest0.7543F = 0.40090.001F = 9.0360.479F = 3.280
Spine0.07F = 2.840.19F = 1.7380.038F = 3.553
MgTest0.2766F = 1.4090.207F = 1.70.0053F = 6.206
Spine0.479F = 0.8650.11F = 2.2690.1286F = 2.193
STest0.379H = 3.0810.145H = 5.3890.044H = 8.056
Spine0.013F = 4.8470.13F = 2.150.01F = 11.311
NaTest0.03F = 3.5460.0003F = 11.3680.618F = 2.996
Spine0.772H = 1.1190.4678H = 2.5420.6366F = 0.58
ClTest0.103F = 2.4240.0001F = 16.4040.4529H = 2.621
Spine0.2518F = 1.5030.3357H = 3.3870.93H = 0.4222
Mg/CaTest0.7294F = 0.43730.0002F = 12.5760.1653F = 1.931
Spine0.5873F = 0.66220.419F = 0.99830.0587F = 3.055
Table
Table 3. Data of an X-ray powder diffraction of tests and spines of the three species.
Table 3. Data of an X-ray powder diffraction of tests and spines of the three species.
SampleChemical Composition of Crystalline Phase
A. lixulaTestMagnesian calcite (Mg0.06Ca0.94)CO3, NaCl
spineMagnesian calcite (Mg0.064Ca0.936)CO3, NaCl
P. lividusTestMagnesian calcite (Mg0.129Ca0.871)CO3, NaCl
spineMagnesian calcite (Mg0.03Ca0.97)CO3, NaCl
S. granularisTestMagnesian calcite (Mg0.06Ca0.94)CO3, NaCl
spineMagnesian calcite (Mg0.06Ca0.94)CO3, NaCl

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Varkoulis, A.; Voulgaris, K.; Zaoutsos, S.; Stratakis, A.; Vafidis, D. Chemical Composition and Microstructural Morphology of Spines and Tests of Three Common Sea Urchins Species of the Sublittoral Zone of the Mediterranean Sea. Animals 2020, 10, 1351. https://doi.org/10.3390/ani10081351

AMA Style

Varkoulis A, Voulgaris K, Zaoutsos S, Stratakis A, Vafidis D. Chemical Composition and Microstructural Morphology of Spines and Tests of Three Common Sea Urchins Species of the Sublittoral Zone of the Mediterranean Sea. Animals. 2020; 10(8):1351. https://doi.org/10.3390/ani10081351

Chicago/Turabian Style

Varkoulis, Anastasios, Konstantinos Voulgaris, Stefanos Zaoutsos, Antonios Stratakis, and Dimitrios Vafidis. 2020. "Chemical Composition and Microstructural Morphology of Spines and Tests of Three Common Sea Urchins Species of the Sublittoral Zone of the Mediterranean Sea" Animals 10, no. 8: 1351. https://doi.org/10.3390/ani10081351

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