- Original Article
- Open Access
The sedimentary dynamics of Sabellaria alveolata bioconstructions (Ostia, Tyrrhenian Sea, central Italy)
Journal of Palaeogeography volume 9, Article number: 2 (2020)
Sabellaria alveolata (Linnaeus 1767) is a polychaete able to build bioconstructions of different thickness, size and patchiness, in intertidal and subtidal environments. Its biological features have been the object of numerous studies worldwide. The worm reefs are formed by millions of tubes built by sand and shells (whole or in fragments) bonded together with a strong glue produced by the worm itself. Hence, Sabellaria alveolata represents a sedimentological asset for the coastal protection, since it contributes to create natural barriers against storm waves and erosion, and supplies the beach with new sandy deposits. This work shows a multidisciplinary approach to studying a bioconstruction of Sabellaria alveolata along the Latium coast (Ostia, Tyrrhenian Sea, central Italy), proposing image analysis as a novel technique to investigate worm reefs, along with classical sedimentological/ecological tools. The Sabellaria bioconstructions have been analysed at different scales of observation, suggesting the more appropriate strategies to develop a reliable model illustrating the different growth steps of these bioconstructions.
Bioconstructions are fundamental for the conservation of biodiversity on our planet since they favour the creation of complex and heterogeneous habitats. The study of the parameters that regulate reef formation and their persistence is a field of research of great relevance and scientific interest, since it involves the complex interactions between the biosphere and geosphere (Geobiology, sensu Nealson and Ghiorse 2001).
Polychaetes of the genus Sabellaria create large and persistent bioconstructions in shallow-marine environments, especially in temperate water (Naylor and Viles 2000; Fournier 2010 and references therein). Sabellariid worm reefs have been found along the coasts of all oceans and in the Mediterranean Sea. Worm reefs of the genus Phragmatopoma are widespread along the American Atlantic coasts (Multer and Milliman 1967; Zale and Merrifield 1989). Along the Pacific coast of America, the presence of sub-tidal reefs built by Sabellaria is reported from North America (Posey et al. 1984), Mexico and Chile (Fournier 2013). Bioconstructions of Sabellariidae polychaetes have also been described from India (Achary 1969, 1974), Malaysia (Ribero and Polgar 2012), and New Zealand (Ekdale and Lewis 1993). Sabellaria alveolata (Linnaeus 1767) and Sabellaria spinulosa (Leukhart 1849) are the most common species along the coasts of northern Europe, locally building massive reefs (Gruet 1986; Holt et al. 1998; Dubois et al. 2003; Braithwaite et al. 2006).
Sabellaria is present in the Mediterranean area with two species: S. alveolata and S. spinulosa. In Italy, scattered mound-shaped reefs and large bioconstructions of S. alveolata occur along the Lazio coast from Circeo to the north of Civitavecchia (Nicoletti et al. 2001), in Liguria along the coast of Genoa (Delbono et al. 2003), and along the south-western Sicilian coast near Agrigento and Trapani (Molinier and Picard 1953; Sparla et al. 1992). S. spinulosa is mainly associated with isolated and ephemeral bioconstructions. The only exception in the Mediterranean Sea is represented by the large reef of S. spinulosa, along the northern Gargano coast (Lisco et al. 2017; Gravina et al. 2018).
From an ecological point of view, the role of Sabellaria reefs seems to be very important, because they provide a massive increase in the available space for other species; they also accumulate organic deposits that can be important sources of food for other organisms, thus promoting the increase of local biodiversity (Holt et al. 1998; Pandolfi et al. 1998; Desroy et al. 2011). From a sedimentological point of view, Sabellaria bioconstructions play an important role in the protection of the coasts; indeed, they prevent the erosion of the beach by stabilizing the sediments involved in the bioconstructions (Naylor and Viles 2000). Massive Sabellaria bioconstructions derive from the aggregation of thousands of tubes (Wust 2011; Fournier 2013) that the worm builds by incorporating particles already present in the sedimentary environment (whole sand and/or shell or their fragments) and cementing them together using an adhesive protein that is produced by the worm itself (Gruet et al. 1987). Several papers focus on the particle size range of the sands that the worms such as Sabellaria and Phragmatopoma use to build their bioconstructions. All previous authors studied the grain-size distribution of the sands that are captured by the worms, after mechanically crushing or manually disjointing the bioconstructions samples.
Multer and Milliman (1967; Table 1) already observed that Phragmatopoma lapidosa builds its tubes using sand grains with diameters between 125 μm and 500 μm. Analysing Sabellaria alveolata tubes, Gruet (1984) suggested that the particle dimension in the tubes seems to be mainly conditioned by the building organ size and, subsequently, by the worm age. More recently, many authors (Naylor and Viles 2000 among others) evaluated the grain-size range of the particles that are captured in the tubes of S. alveolata, achieved variable results (Table 1) and qualitatively discussed the possibility that composition and morphology of the available sandy grains can play a role during the tube construction.
The aim of this paper is to provide a detailed analysis of textural and mineralogical parameters of Sabellaria alveolata bioconstructions. This study focuses on the Latium coastal area (Ostia, Tyrrhenian Sea, central Italy) where former ecological studies (Taramelli Rivosecchi 1961; Nicoletti et al. 2001; La Porta et al. 2006; La Porta and Nicoletti 2009) reported massive large worm bioconstructions built by this taxon. The largest worm bioconstruction of the Ostia area has been analysed with a multiscale and interdisciplinary approach, using classical ecological and sedimentological monitoring procedures for the evaluation of: (1) the spatial distribution of the worm tubes; (2) the location of sectors with grains that are trapped directly by the worm (tube area) and with grains that are casually located between adjacent tubes (intertube area); (3) the grain-size distribution of sands in tube and intertube areas; (4) the grain size, composition and morphology of sands that are available in the present-day beach environment. The final dataset will enable to establish the textural and mineralogical features of the sands that are directly trapped by the worm.
Furthermore, the structure of the bioconstruction has been investigated without modifying its original morphology analysing, i.e., the relationships between the physical parameters can be quantitatively defined (e.g., the number of worm tubes and the range of tube dimension variability); and, how growth or decline of the worm bioconstruction can be recorded at a microscopic scale. Finally, a general model for the seasonal evolution of the bioconstruction is suggested also considering the role of the worm reefs for the coastal protection.
Geological and geomorphological setting
Ostia is located along the Latium coastal area (Tyrrhenian Sea), about 30 km southwest of Rome, central Italy. Late Quaternary morpho-sedimentary evolution of this area is the result of both the complex interaction between tectonic/volcanic processes and sea-level changes and the Tiber delta migration phases (Bellotti et al. 1994; Bellotti et al. 1997; Giraudi 2004; Praturlon 2008; Milli et al. 2013). The present-day Tiber delta area contains a large channel (Fiumara Grande) that flows into the Tyrrhenian Sea at the northwest of the Ostia beach (Fig. 1). An artificial small channel, called Canale dei Pescatori (excavated during the second century AD; Bellotti et al. 1994), flows into the sea a few hundred meters towards the east from the main Sabellaria alveolata bioconstruction, which is the object of this study. From the Fiumara Grande to the Canale dei Pescatori, the Ostia beach shows a longitudinal littoral transport, mainly oriented towards the southeast. The local tidal range is very small (< 0.5 m) and the depth of wave base is about 7 m, being the significant annual wave height of about 4 m (Ferrante et al. 1993). This sector of the Ostia beach has been deeply modified with interventions (1990 to 2003) of coastal defence and nourishment (Capelli et al. 2007). A submerged barrier runs parallel to the coastline (at a distance of about 150 m from it) and is placed with base at − 4 m and crest at − 1.8 m of water depth. The beach nourishment was carried out in the internal/protected basin using a thick layer of sand and gravel with grain size between 0.08 mm and 120 mm. Only the upper layer (1 m thick) contains sands with grain size from 0.3 mm to 1.3 mm (D50 = 0.5 mm; Franco et al. 2004).
Field and laboratory procedures are here described following a scale order. Largest-scale monitoring procedures have involved about 20,000 m2 of bioconstruction and adjacent beach sub-environments; smallest-scale measurements have been carried out on the morphometric parameters of single sand grains (with diameters in the order 100 μm).
Survey and sampling
The study area is the Sabellaria alveolata bioconstruction located in the coastal area between “Porto Turistico di Roma” and “Lega Navale” sites (Fig. 1). Surveys and samplings were carried out by scuba diving on seasonal basis during autumn 2013, spring 2014, summer 2014, and winter 2014 (and a qualitative monitoring in autumn 2017). An ecological and sedimentological survey was conducted to define the geometrical parameters of the entire bioconstruction. The ecological monitoring of bioconstructions concerned the evaluation of the relative abundances of both polychaetes and other taxa associated with the bioconstruction, through the comparison of the number of the species that inhabit the rocky bottoms and the sandy ones nearby (Bonifazi et al. 2019). The sedimentological surveys focused on the observation of the physical state of the bioconstructions (area, thickness, depth reached, prevailing morphology, etc.), mainly through detailed underwater photographic documentation (Fig. 2a–d). During the surveys, several sampling campaigns were carried out. Fifteen bioconstruction samples (3 replicates for 5 seasons) were collected, 20 × 20 × 20 cm3 in size (Fig. 2a), along the central and highest part of the bioconstruction, at different water depths (1 m, 2 m, and 3 m) across different seasons. 4 samples of incoherent sands have been collected at different water depths (between 0 and 5 m of water depth) along a transect perpendicular to the coastline (Fig. 1). Standard procedures for present-day marine sediments samplings were used (Poppe et al. 2000), collecting 200–400 g at the water-sediment interface. Finally, in order to investigate the spawning period and to detect the larval peaks in the sea-water, monthly planktonic samples were collected at Marina di San Nicola, about 40 km north from Rome (41.931°N, 12.110°E), from April 2015 to March 2016 (April 2015, May 2015, June 2015, July 2015, August 2015, September 2015, October 2015, November 2015, January 2016 and March 2016). These campaigns were carried out near the coastline because Sabellaria larvae are concentrated close to the coast (Dubois et al. 2007). A plankton net, 30 cm in diameter, circular mouth and 20 μm mesh size was used. The net was towed by a scuba diver at a distance of 200 m from the coastline, maintaining a speed of 1.5 knots (~ 0.77 m/s) and covering a total distance of 1500 m.
The collected samples were frozen immediately after sampling and, later, placed in the oven to dry them before being prepared in the laboratory. Samples used for microscope and image analyses were washed with distilled water and then cemented with epoxy resins. Decimetric slices of this coherent material were obtained to carry out high resolution macrophoto and thin sections for petrographic analyses. High resolution images of the slices, digitized thin sections and microscope photos (at × 2.5 magnification) were used to produce maps of the main structural and textural features of the tubes arrangement. ImageJ©, ArcGIS©, Gradistat© were used to evaluate size and shape of the grains trapped in the bioconstruction (see below). The procedure of disaggregation of the bioconstruction samples is a difficult operation, but it is necessary to perform standard granulometric analyses. The mechanical breakage of the grains and the friction actions between clasts can create a certain percentage of fine-grained particles that are not part of the primary texture. Moreover, the incomplete disaggregation of the tubes causes an increase in the coarse fraction. Samples of S. alveolata bioconstructions were disaggregated using a solution of hydrogen peroxide (33%) in water with proportion of 1 to 4. This procedure disjoined the individual tubes and eliminated the aggregates of granules, without creating appreciable quantities of fine sediments. Sieving analyses on these incoherent materials were carried out using a ½ phi mesh sieve column. Classical petrographic analysis on the bioconstruction was carried out on thin sections at the binocular microscope while the mineralogical composition of beach sands was carried out on the modal class interval counting more than 300 grains for each visual field.
For each sampled block, the density of the worm tubes was measured for ecological analysis purposes, by using a visual estimation technique, counting each tube visible on the sample surface. For the recognition of Sabellaria larvae, all the collected samples were immediately fixed in 10% neutral buffered formalin, and then the samples were retained through a sieve of 20 μm mesh and preserved in 70% ethanol. Sabellaria larvae were sorted and identified under an optical microscope (Zeiss Axiolab) and counted under a dissecting microscope (Leica WILD M3B).
Image analysis procedures
The analyses of the sedimentological features of the bioconstruction were carried out on samples impregnated with resin to observe the actual structure of the tubes and to distinguish tube and intertube areas. Digital images of the thin sections were scanned using a slide scanner (Polaroid model Spintscan 4000) which is modified to accommodate the glossy thin sections and two polarizing sheets of light. The images under plane-polarized light were analysed with ImageJ© to calculate the total porosity (the porosity due to the presence of the circular tube voids and the irregular intergranular porosity), density of the tubes and, finally, the diameter variations of the tubes. Classes of diameters were calculated only for sub-circular tubes (Aspect Ratio = major axis/minor axis < 2). After detailed optical microscope analysis aimed to recognize main mineralogical classes, each sand grain has been easily classified in agreement to its size, shape, composition and position within the structure using microscope photos on thin section. ArcGIS© maps were used to calculate composition percentages, while the ImageJ© facilities were mainly applied to the grain-size distributions and morphometric analyses.
The results will be shown according to the different scales of observations, from the seasonal monitoring surveys to the microscopic morphometric analysis. This order strictly reflects also the temporal succession of the stages of this study.
Monitoring the bioconstruction: morphology and main ecological features
The Ostia bioconstruction was measured for the first time during the fall season 2013 (end of September; Fig. 2a). The monitoring analysis focused on a particularly well-developed portion of the bioconstruction (Fig. 1c) that extends parallel to the coast between some easily identifiable points. It stands on the crest of the submerged longitudinal barrier and on the interior side of it. Small-scale (0.2 m in width and 0.1 m in height) bioconstructions occur in the internal basin and in the open-sea sector and progressively disappear at 4 m of water depth. On the crest of the barrier, there is a compact bioconstruction that continuously develops parallel to the coastline; in its maximum extension, it reaches more than 3 m above the sea bottom; its actual thickness is lower being the difference between the man-made barrier height (locally, 2 m in height). The difficulties related to the recognition of its actual base do not allow a quantitative evaluation of the bioconstruction height, but, where the contact between the bioconstruction and the underlying barrier is visible, its thickness was often more than 1 m.
During the monitoring of early March 2014, the bioconstruction showed no detectable significant changes (Fig. 2b): total area was constant and only the roughness of the bioconstruction morphology appeared slightly increased probably related with newly formed set of tubes.
In June 2014, the bioconstruction showed a slight to moderate degeneration, highlighted by the recruitment of mussels (Fig. 2c). Mussels occupied the localized sectors of the bioconstruction, eroding the bioconstruction but without changing the general morphologies. Furthermore, the contact between the bioconstruction with the underlying coastal defence was more exposed.
The stasis/decline phase in the growth of the bioconstruction remained unchanged even in early August 2014 (Fig. 2d). The sectors with flat-regularized surfaces in the bioconstruction and areas of man-made barrier without a bioconstruction cover were widespread but the sectors with mussels seemed unchanged.
The last monitoring had been carried out during the autumn of 2017 in order to verify the persistence of the bioconstruction after 3 years and to qualitatively describe the bioconstruction but without sampling. The survey showed a bioconstruction that is growing again, covering the whole submerged barrier, in a continuous and compact way, with large hummocks and rough mounds (Fig. 3).
Mean values of the Sabellaria tube density measured on samples from the surveys of years 2013–2014 using the visual counting technique are shown in Table 2. The highest tube density value was measured in August 2014 with 34,800 ± 1100 tubes/m2; conversely, the lowest tube density value was measured in September 2013 with 21,450 ± 800 tubes/m2.
Plankton samples collected from April 2015 to March 2016 showed large variations in larval abundance throughout the year, even though Sabellaria larvae were detected in all monthly surveys. The number of Sabellaria larvae showed an increase from late spring to summer months; however, the larval peak was identified during the autumn months, from early October to late November (Fig. 4).
Image analysis on the bioconstruction samples
The evolution of the structure of the Ostia Sabellaria alveolata bioconstruction over time can be easily defined using qualitative description, mainly related to the morphology of the bioconstruction. Nevertheless, by a rigorous geometric point of view, the changes in the large-scale morphology of the bioconstruction are very complex to describe. To overcome this difficulty, in this study, the measurement of some simple small-scale descriptor parameters (tube density, variability of the tube diameter, porosity) is taken as a record of seasonal changes in the bioconstruction.
The density of the tubes
The density value is here defined as the number of tubes/unit area calculated on thin sections (about 8 cm2 × 16 fields) of the bioconstruction (Fig. 5). The density values measured in this way vary seasonally. The average value is approximately 83,000 tubes/m2 with a range varying from 157,100 ± 42,000 tubes/m2 in autumn to 43,000 ± 14,600 tubes/m2 in winter (Fig. 6). The number of tubes is very high in the autumn samples, but it is quite constant during other seasons (the differences are equal to the standard deviation). The seasonal significance of the number of tubes per unit area (/m2) is obviously not univocal and the tube diameters and their variability need to be considered as well. Discrepancies between density values obtained with different methods are treated in the “Discussion” section.
The variability of tube diameters
The worm tube dimensions measured on a large number of thin sections are very variable (Fig. 5). Nevertheless, this variability seems to follow simple regularities with the succession of the seasons (Fig. 6). Maximum diameters are recorded in March 2014 (about 5300 μm) while they are constant in the other seasons (about 3000 μm). In September 2013 and March 2014, the classes of small diameter appear frequently. Minimum and mean diameters gradually and regularly increase from September 2013 to August 2014. The range of the different classes of diameters seems to be seasonally-influenced too (Fig. 6): this range is high in March 2014 (~ 170 μm < d < ~ 5300 μm), and low in August 2014 (~ 820 μm < d < ~ 3100 μm).
The measure of the porosity (n = Vv/VT, i.e. void volume/sample volume) was performed on the high-resolution photos of the decimetric (impregnated and glossy) slices of the bioconstruction samples. The porosity is calculated by ImageJ© for the grey levels related with the resin color. Therefore, these values indicate the total porosity of the bioconstruction (sum of the voids occupied by the worm, the intergranular and intragranular porosity) and vary from 28% to 37%, without recording a regular seasonal variability.
The microstructure of the worm tubes
Analysing the structure of the bioconstruction in more detail (Fig. 7), it is always possible to recognize the empty circular void that represents the area occupied by the worm when it was alive. The variability of this void has been discussed in the previous section. The grains closest to the void (tube) appear to be placed around it, with a surprising regular tangential order (Fig. 7). Outside the tube (intertube), sand grains are arranged in a more chaotic way.
These two different areas can be distinguished in all samples (Fig. 8). Often, the distinction between tube and intertube sectors can be confirmed observing the sudden changes in grain size too (Fig. 8a). Locally, it is possible to recognize sets of tubes characterized by very small diameters (between 200 μm and 400 μm), with a regularly-spaced structure that repeats itself in space (Fig. 8b). The tube area is reduced to a single thin layer composed of about 15–20 sand grains. In the thin sections that are parallel to the general development of the tubes, the area occupied by the worm is clearly recognisable as a linear feature; it is limited by grains oriented parallel to the tube wall. In areas not far from the tube, the grain size appears to increase rapidly and, here, no preferential orientation is observed (Fig. 8c). Textural analyses under the microscope show that the general structure of the bioconstruction is influenced by the tube growth. Tubes grow next to each other and form a grossly ordered and porous structure that can include also the sand of intertube area.
The internal part of some tubes can be filled by sands (Fig. 9). The number of these filled tubes is always very low. There is not a remarkable variation of their occurrence in different seasons. September 2013 and March 2014 contain the lowest number of filled tubes (2 in each season) while June 2014 and August 2014 have 3 and 5 filled tubes respectively.
Diameters of particles that form the tube and intertube sectors allow them to obtain an indirect granulometric distribution for each part of the bioconstruction (Fig. 10). The range of the granulometric distribution seems to be reliable. The sands located between adjacent tubes (intertube) seem to be less sorted in grain size than the sands directly trapped by the worm (tube). Nevertheless, the fiftieth percentile of the grain-size distribution (D50) has the same dimension in the two sectors, being D50 = 207 ± 48 μm in the tubes and D50 = 204 ± 37 μm in the intertube sectors.
The grain-size analysis carried out by physically sieving the sand samples collected from different water depths (0.0 m, − 1.5 m, − 3.5 m, and − 5.0 m) are shown in Fig. 11a. The D50 is variable, slightly varying between 311 μm and 499 μm, but is always higher than the fiftieth percentile of the sediment distribution that is trapped in the worm tubes (about 200 μm). The distribution is always unimodal. Sorting is related to moderately classified sand. The value of Kurtosis indicates a leptokurtic distribution. Skewness values are generally close to zero and therefore approximately symmetric, with the exception of the sample collected at 1.5 m depth, tail towards coarse sediments, where the Skewness value is instead negative.
The physical grain-size analyses were carried out also on 3 bioconstruction samples taken at 2 m of water depth after complete disaggregation procedures (Fig. 11b). The sediments have a D50 that is slightly variable between 241 μm and 332 μm. The distribution is unimodal only for one sample (O1-OS_14C in Fig. 11b). Sorting corresponds to moderately classified sand; the value of Kurtosis indicates a mesokurtic distribution; the Skewness value is close to zero (symmetric Sk). For the other two samples (O2-OS_14C and O3-OS_14C), the distribution is mainly bimodal, and therefore, the statistical parameters cannot be considered representative.
The morphometric analyses of the bioconstruction sands have been conducted to quantitatively compare the shape of the grains of the tube and intertube (Fig. 12). The mean value of Aspect Ratio measured in the tube grains is always slightly higher than in the intertube sands (2.37 ± 0.54 for the tube and 1.94 ± 0.20 for the intertube; Fig. 13a). The mean Circularity value calculated on the grains composing the tubes is 0.64 ± 0.05 while the grains of the intertube areas have a mean Circularity value of 0.67 ± 0.05 (Fig. 13b).
To compare the minerals that form the tube and the intertube sectors of the bioconstruction with those that are available in the surrounding beachface and shoreface environments, their composition has been established using a quantitative approach.
The main mineral phases of sands trapped in the bioconstruction have been recognised in thin section (Fig. 14). The lithic fragments are very abundant and mainly derive from the erosion of metamorphic and effusive magmatic rocks (rhyolites); lithoclasts of micritic limestones have been recognised too. Quartz is very abundant and is present as crystalline quartz, polycrystalline, flint and chalcedony. Feldspars are represented by both potassium feldspars and plagioclases. Plagioclases sometimes appear to be heavily seriticized, while potassium feldspars can occur in the form of a microcline with perthitic mixing. Amphiboles with the diopsidic composition, pyroxenes with pleochroism in shades of green, and micas are observed among the colored minerals. Finally, carbonate bioclasts are abundant too. They occur both as entire (foraminifera) and in fragments (mainly molluscs and sea urchin spines). Many serpulid tubes have been recognised.
The mineralogical composition has been obtained by classifying sands on microscope high-resolution images of thin sections. Compositional maps have been compiled distinguishing tube and intertube sectors (Fig. 15).
The petrographic and mineralogical characterization of the beach sands has been carried out with a stereo microscope on the modal class interval (125–500 μm). The sands coming from the beachface and shoreface contain the same mineral phases of the sands that are trapped in the bioconstruction. Counting more than 300 grains in every observation field, a quantitative modal composition of these sands has been obtained.
The composition of tube or intertube bioconstruction and beach sands has been compared using the classical Folk (1974) triangular diagram. In agreement to this classification, all sands are defined as lithic arenites and there is no obvious difference between the composition of sands that are trapped by the worm in the tube, or that are located between adjacent tubes, or that are available in the sedimentary environment.
The discussion of results focuses on three main topics that are interconnected at various temporal and spatial scales: (1) the origin of seasonal phases of the bioconstruction; (2) how the textural features of the bioconstruction can record these changes; (3) the significance of mineralogical features of the sands that form the worm bioconstruction. These aspects are discussed following a scale-dependent order.
Record of seasonal changes of the Sabellaria alveolata bioconstruction
The monitoring survey of one of the most impressive worm bioconstructions of the Latium coast shows that it is subjected to seasonal phases of growth (autumn and winter) and stasis (spring and summer) that alternate leaving the bioconstruction in general good conditions (Figs. 2 and 3). It is very challenging to seasonally measure the dimension of the bioconstruction since it develops on a man-made barrier. The state of the bioconstruction can be better monitored by qualitatively describing the roughness of main hummocks and mounds. To verify these observations in a more quantitative way, samples of bioconstruction have been collected and analysed from an ecological and sedimentological point of view. The number of tubes has been evaluated with two simple methods (Table 2): (1) by visual counting and (2) in thin sections under a binocular microscope. Obviously, the microscopic analysis leads to a more accurate evaluation for the tube number allowing an easier recognition of small tubes.
Many procedures for the calculation of the tube density are based on the visual counting methods carried out in laboratory or even with ROV (Remotely Operated Vehicle) observations (Gubbay 2007). This kind of procedure can induce errors also in the interpretation of growth and stasis stages: in thin section, the maximum number of tubes corresponds to September 2013, while the visual counting recognizes a minimum number of tubes in the same month. For the ecological approaches, the value of density is related to the number of living worms in a given volume of the bioconstruction. However, this data is not directly related with the physical parameters of the bioconstruction (volume, porosity, number of tubes, etc.) that are the focus of this study.
The density of tubes (number of tubes in a given area) is strongly dependent from their dimensions. Moreover, the tube dimensions (the diameter of the circular void occupied by the worm) in different seasons have been accurately measured (Fig. 6). These data are interesting, since they record the effective recruitment stages of the Sabellaria alveolata bioconstruction: young worms are associated with small tubes and the old ones occupy large tubes. A large variability of the tube dimensions is associated with the growth periods of the bioconstruction (autumn and winter) that are characterized by the abundance of small-diameter tubes (young individuals). A narrow range of diameter variability and the abundance of large diameters are records of a stasis stage of the bioconstruction (spring and summer). Young individuals regularly grow from autumn to summer and this process is recorded by the continuous increase of minimum and mean diameters from September 2013 to August 2014 (Fig. 6). Older individuals live in the largest measured tubes (more than 5 mm in diameter), and these dimensions are also the maximum diameters reported in the literature (Fournier 2013). It means that these individuals survived to some seasonal changes of different years, because 4–5 years is the average life span of these worms (Gruet 1984).
This interpretation is supported by the Sabellaria larvae monitoring data. The larval peak measured in this area occurs from early October to late November (Fig. 4) even if the presence of larvae at different development stages for most of the year, including the early trochophore, suggests a protracted spawning season. These results are in partial accordance with those of Gruet and Lassus (1983) and Dubois et al. (2007) reported along the Northern Atlantic coasts: these authors observed two distinct different periods of high larval density, in April and from early September to early October.
The data suggest that the growth and stasis stages are not related with fixed seasonal spawning periods. On the other hand, these different stages are not dependent from the energy of marine action, as recently suggested by Lisco et al. 2017 for Sabellaria spinulosa bioconstructions, as the stasis coincides with the period of relatively low energy of storm waves. Probably, the stasis periods (spring and summer) are induced by the effect of mussel recruitment that starts before June and by the anthropic disturbance during the entire summer, since the Ostia Lido is one of the most popular beaches of the Latium coast. More ecological studies are needed to find a reliable origin for the decline periods of this bioconstruction. The model of the seasonal changes has been summarised in Fig. 16, where the main stages are recorded in the bioconstruction, also at a microscopic scale, as: (1) number of worm tubes; (2) relative abundance of small and large tubes; (3) actual range of the variability of tube diameters.
Textural features of the Sabellaria alveolata bioconstruction
As mentioned in the introduction, many authors have estimated the grain size of sands that are trapped by different taxa of worms to build their tubes (see different methods in Table 1). If sieving analyses are carried out on disaggregated fragments of the bioconstruction, the results will record the granulometric distribution of tube and intertube sediments. Carefully isolating single tubes before sieving analyses possibly helps to obtain more representative data for the actual grain size of sediments that the worm traps (Naylor and Viles 2000). Meanwhile, using the image analysis approach on thin sections and obtaining high-resolution photos can help to calculate single grain-size distributions for the different tube and intertube sectors of the bioconstruction and help to compare them with the grain size of sands available in the beach sub-environments. This method also allows investigating those sediments trapped by small or young worms that could be the most abundant population in some seasons.
Table 3 shows the results of the granulometric distribution of sands coming from: (1) bioconstruction samples impregnated with resin (image analysis); (2) beach sub-environments; (3) disaggregated bioconstruction fragments (physical sieving analysis). In agreement with previous researches, our results show that Sabellaria alveolata seems to select sands on the basis of their grain sizes (see Gruet 1984). In particular, the worm seems to trap the finer fraction of the sands in the beachface and shoreface environments. This result is remarkable for the role of Sabellaria alveolata bioconstruction in the coastal protection. It is generally accepted that the worm reef forms physical barriers for the action of storm waves, tides and currents, and increases the cohesion in the soft sediment at sea-bottom (Fournier 2013). The abundance of relatively fine-grained sediments in the bioconstruction structure shows that the Sabellaria alveolata bioconstructions are also important as temporary repository during the high-energy storm events of autumn and winter. The fine-grained fraction is the first granulometric range that disappears in the retreating sandy beaches and typically recorded by negative Skewness values. Probably, during large storm-wave events, the worms trap the fine-grained sands saved from the erosion and the transport toward the shelf or alongshore. These sands return to the beach during seasonal decline periods.
The result of grain-size analyses shows also that sands forming the tubes are more sorted than sands that occupy the intertube sectors of the bioconstruction even if these different parts of the bioconstruction seem to contain sands with the same fiftieth percentile (D50 tube = D50 intertube). This result is related to the way in which each worm selects the grains to build its tube. The diameter of the particles that can be potentially inserted in the tube bioconstruction is related to the size of the organ that physically traps the sands, as suggested by Gruet (1984). If the bioconstruction is characterized by worms of a specific age range, the trapped sands would be limited to a specific grain-size class. To prove this relationship in a quantitative way, a comparison between the diameters of the worm tube, which is selected dependently from its age, and the D50 values of the tube sands has been performed. The correlation between these two measured parameters is linear/positive even if its correlation degree is low (Fig. 17), confirming the hypothesis of Gruet (1984).
The main morphometric parameters of the grains directly trapped by the worm are measured with an aim to quantitatively demonstrate, for the first time, that Sabellaria alveolata is able to select particles with some particular coefficients of the grain shape, as suggested in many previous papers (see Fournier 2010 and references therein). Comparing grains of the tube and grains of the intertube sectors of the bioconstruction (Fig. 13) shows that Sabellaria alveolata actually prefers selecting elongated particles. These particles are often made up of bioclasts (foraminifera and molluscs). La Porta et al. (2006) suggested that bioclasts are very abundant in the tubes, since the shell fragments can be eroded and put in suspension in a very easy way during storm-wave events.
The porosity of the Sabellaria alveolata bioconstruction is variable between 28% and 37%. These values are low if compared with present-day carbonate bioconstructions which have porosity values variable between 40% and 70% (Ahr 2008). In the worm bioconstructions, the largest voids shape the interior of the tubes, after the death of the organism, but they could be filled by sands over time, during successive evolutive stages (Fig. 9). This kind of low porosity could guarantee a greater resistance of the worm bioconstruction in the absence of carbonate cement.
Mineralogical features of the Sabellaria alveolata bioconstruction
All samples can be defined as lithic arenites according to Folk (1974) and there are no differences between sands from the bioconstruction (tube and intertube) and sands of the surrounding shallow-marine environments. This result obviously implies that Sabellaria alveolata is not able to select grains on the basis of their mineralogical composition, as suggested by the literature data. At the same time, however, that is in apparent contrast with data showing the abundance of bioclasts for the construction of the tube. To explain these inconsistent data, a mineralogical classification that is more suitable for hybrid sands (Zuffa 1980) has been used. The felsic and mafic minerals and the lithic fragments were grouped in the NCE class (non-carbonate extrarenite class); the carbonate lithoclasts were grouped in the CE class (carbonate extrarenite class); and, the bioclasts were grouped in the CI class (carbonate intrarenite class). Fig. 18 shows the results of this classification. The sands have a low content in bioclasts and are mainly classified as siliciclastic hybrid sands or hybrid sands, among which, only one sample is classified as a calcilithic hybrid sand. Nevertheless, there are some slight differences of the content in bioclasts in tube, intertube, and beach sands. Beachface and shoreface contain a higher content of bioclasts compared with tube and intertube sectors of the bioconstruction. This data is not surprising, since not all bioclasts that are available in the shallow-marine environments can be trapped by the worm, as a result of the differences in bulk density, composition, shape, roughness, etc. Sands that form the tubes contain a larger number of bioclasts than in the intertubes. This data shows that the Sabellaria alveolata tubes contain grains having no specific composition, except for carbonate bioclasts that are trapped because their elongated morphology and low bulk density could result in a higher chance of being suspended during storm events.
The genus Sabellaria is a very common bioconstructor in temperate areas; its bioconstructions reach large dimensions along the coasts of the oceans and in the Mediterranean Sea. The peculiarity of these polychaetes is represented by the manner in which sand grains are agglomerated to build bioconstructions made up of millions of centimetric tubes. Data and results of this study show that Sabellaria alveolata bioconstructions contain: (1) sands that are directly inserted by the worms in the tube framework and (2) sands that fill the spaces between adjacent tubes (intertube areas). Tube and intertube sands have more or less the same D50 (about 200 mm), but tube sands are well sorted, being selected by the worms and by their building organ, while intertube sands are poorly sorted, being casually deposited in the empty spaces. Nevertheless, both sectors have sands that are fine-grained if compared with sands of the surrounding beach sub-environments. By a mineralogical point of view, the Ostia worm bioconstruction holds sandy grains that have the same compositional features of beach sands; tubes show a slight increase in the bioclast content. This result seems to be confirmed by the morphometric analysis that proves a definite predominance of elongated grains in the worm tubes.
A clear relationship between the size/density of worm tubes and the seasonal variations has been established and compared with data coming from classical ecological procedures (scuba diving monitoring, Sabellaria larvae sampling, etc.) carried out in the same study area. At a microscopic scale, the bioconstruction growth phases (winter and autumn) are recorded by: (1) a high tube density; (2) a drastic decrease of tubes diameters; (3) a large variability of the tube diameters. The destructive phases (spring and summer) can be recognised by: (1) the low tube density; (2) an increase of tube diameters; (3) a low variability of tube diameters. These results show that the autumnal larval peak of Sabellaria alveolata, the vernal mussel recruitment, and the summer anthropogenic disturbances leave unmistakable traces in the sedimentary record of the worm tubes.
In conclusion, this study shows that the Sabellaria alveolata bioconstructions are fundamental for the coastal protection, representing a continuous and stable storage of fine-grained sands during their seasonal evolutionary stages. The monitored cyclic volume variations of the bioconstruction (described as areal/thickness changes) and the calculation of its total porosity (relatively low if compared with carbonate reefs) show that the Sabellaria alveolata bioconstructions act as nourishment agents, storing and furnishing enormous quantities of sediment that can be redistributed in the coastal sub-environments by the action of storm waves, tides and currents.
Availability of data and materials
The datasets analysed during the current study are available from the corresponding author on reasonable request.
- D50 :
Fiftieth percentile of the grain-size distribution
- VT :
- VV :
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The authors thank Prof. Zeng-Zhao Feng, Prof. Ian D. Somerville, Ms. Yuan Wang and two anonymous reviewers for comments that greatly improved the manuscript.
The authors declare that the data reported here were obtained with research financed by the universities involved.
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Lisco, S.N., Acquafredda, P., Gallicchio, S. et al. The sedimentary dynamics of Sabellaria alveolata bioconstructions (Ostia, Tyrrhenian Sea, central Italy). J. Palaeogeogr. 9, 2 (2020). https://doi.org/10.1186/s42501-019-0050-6
- Sabellaria alveolata
- Shallow-marine environment
- Image analysis
- Tyrrhenian Sea
- Latium coast