Late Roman Forest in the Delta of the River Po (Italy): Remote Sensing and 3D Maps Computation for Palaeoenvironmental Reconstruction

Literary and historical sources provide information about Late Roman forests in the Delta of the River Po, in the district of Ferrara (Italy), between Vicus Aventiae (Voghenza), Sandalo, Gambulaga, Caput Gauri (Codigoro) and Castrum Cumiacli (Comacchio). Toponymy, archaeological excavations and geoarchaeological studies support the palaeoenvironmental reconstruction of this land. In this work, after a brief examination of the ancient texts, we are going to introduce some new data concerning archaeobotanical evidence, detected by remote sensing in combination with direct surveys (on land and underwater). On the technical side, we are going to present a geomatic application for underwater measurements of ancient trunks related to discoveries in the palaeo-watercourses of the River Po (geomatic measurements, thanks to remote sensing surveys, allows us to have detailed length and diameters of trunks and trees, which are not always visible and detectable while diving) together with some satellite elevation measurement of the river banks and 3D map supported by geocomputation. Thanks to botanical data, we are able to illustrate the local context of the paleoenvironmental/archaeological sites, offering a reconstruction of the landscape and of the use of the wood.


Introduction and Historical Sources
The open land of Pianura Padana, during the Late Antiquity and the Middle Ages, was characterized by rivers and watercourses with paludes and piscariae, between forests and woods. The complex hydrographic system was surrounded by a manifold botanical world. Data concerning forests in Late Antiquity in Italy are not abundant [1][2][3], but thanks to our recent studies we have been able to contribute to the knowledge of this historical phase and reconstruct a detailed panorama of the river banks of the Eridanus (ancient Po) between Voghiera and Portomaggiore, reaching the area of Codigoro and Comacchio (small towns in Ferrara district).
The innovative aspect of this research consists of introducing remote sensing technique with indirect measures of landscape and botanical findings with big dimensions, in order to make a contribution for the reconstruction of ancient forests, combined with satellite image analysis and remote sensing elevation data from Google Earth Pro 7.3.3.7699 (64-bit), in the new perspective of Waterscape Archaeology.
The focus of this study is a specific investigation with thematic analysis about the remains of the Late Antique and Medieval Forest with traditional and innovative methodologies. We are going to explain some details about palaeoenvironmental context of the River Eridanus, going more deeply into some topics and discovers of our project Underwater archaeology of inland waters performed The above-mentioned project is coordinated by the authors and it is focused on experimentation of the synergy of scientific disciplines and combined methodologies and techniques for underwater cultural heritage of the inland water. It is a collaboration between the scuba Federation ITA F07-CMAS Diving Center Italia, Confédération Mondiale des Activités Subaquatiques Soprintendenza Archeologia, Belle Arti e Paesaggio per la città metropolitana di Bologna e le province di Modena, Reggio Emilia e Ferrara, Archaeology sector, University of Padova, Cultural Heritage Department, Underwater Archaeology Laboratory (LAS).
The forest, from Roman Time to the Middle Ages, was developed circum ripa Padi et litora Maris Hadriatici (close to the banks of the River Po and the coast of the Adriatic Sea), as mentioned by Vitruvius (De Architectura, II,9,14) and Cassiodorus (Variae, V, 17, 5). S. Patitucci Uggeri, studying ancient document from Pomposa (Comacchio district) [9, 10], explains that there were some sylvae attested in official mediaeval documents, belonging to diploma and emphyteusis in Pomposa: a silva (wood, forest) in insula queae vocatur Adriana (in the island called Adriana) near Pomposa, a silva que vocatur de Montone (a forest called of the Montone) near Goro, a nemus Capitisgauri (a wood of Codigoro), a silva vocata Vaccolino (a forest called Vaccolino), near the selvosa insula Pomposiana (Pomposiana Island with dense forest). In this panorama, actually, we are able to add another silva, located between Voghenza and Portomaggiore, following the Eridanus, attested by archaeological evidences.
As underlined in our last publication about Lago Tramonto, the local toponymies give some suggestions about the old presence of a local forest; Runco, for example, from the verb runcare, to cut (referring to prune trees, place already known as Alberolungo-long tree), Rovereto, from roburetum, wood of oaks [11,12]. The above-mentioned project is coordinated by the authors and it is focused on experimentation of the synergy of scientific disciplines and combined methodologies and techniques for underwater cultural heritage of the inland waters. It is a collaboration between the scuba Federation ITA F07-CMAS Diving Center Italia, Confédération Mondiale des Activités Subaquatiques Soprintendenza Archeologia, Belle Arti e Paesaggio per la città metropolitana di Bologna e le province di Modena, Reggio Emilia e Ferrara, Archaeology sector, University of Padova, Cultural Heritage Department, Underwater Archaeology Laboratory (LAS).
The forest, from Roman Time to the Middle Ages, was developed circum ripa Padi et litora Maris Hadriatici (close to the banks of the River Po and the coast of the Adriatic Sea), as mentioned by Vitruvius (De Architectura, II,9,14) and Cassiodorus (Variae, V, 17, 5). S. Patitucci Uggeri, studying ancient document from Pomposa (Comacchio district) [9,10], explains that there were some sylvae attested in official mediaeval documents, belonging to diploma and emphyteusis in Pomposa: a silva (wood, forest) in insula queae vocatur Adriana (in the island called Adriana) near Pomposa, a silva que vocatur de Montone (a forest called of the Montone) near Goro, a nemus Capitisgauri (a wood of Codigoro), a silva vocata Vaccolino (a forest called Vaccolino), near the selvosa insula Pomposiana (Pomposiana Island with dense forest). In this panorama, actually, we are able to add another silva, located between Voghenza and Portomaggiore, following the Eridanus, attested by archaeological evidences.
As underlined in our last publication about Lago Tramonto, the local toponymies give some suggestions about the old presence of a local forest; Runco, for example, from the verb runcare, to cut (referring to prune trees, place already known as Alberolungo-long tree), Rovereto, from roburetum, wood of oaks [11,12].

Topographical and Geoarchaeological Context
The Southern Palaoeo-watercourse of the River Po, the Eridanus runs across the ancient sites of Vicus Aventiae (Vochiera-Voghenza), Gambulaga, Roburetum (Rovereto), turning to South to Castrum Cumiacli (Comacchio) from the Etruscan Period until the Late Antique Phase. In the sector between Gambulaga Heritage 2020, 3 784 and Rovereto the river was modified by the human presence. The riverbed shows anthropized banks modelling the river edges, arranged according to a rectilinear flow Southwest-Northeast [4,13] ( Figure 2). Heritage 2020, 3 3

Topographical and Geoarchaeological Context
The Southern Palaoeo-watercourse of the River Po, the Eridanus ran across the ancient sites of Vicus Aventiae (Vochiera-Voghenza), Gambulaga, Roburetum (Rovereto), turning to South to Castrum Cumiacli (Comacchio) from the Etruscan Period until the Late Antique Phase. In the sector between Gambulaga and Rovereto the river was modified by the human presence. The riverbed shows anthropized banks modelling the river edges, arranged according to a rectilinear flow Southwest-Northeast [4,13] (Figure 2).   [14]. The river was a jointing natural element used for transport, commerce, and every day economic life. Reading the local stratigraphy, we see the Eridanus bank developed on a multilevel structure, mainly natural, with artificial devices.
In Voghiera, for example, we see some layers of sand, coming from overflow of the river ( Figure  3) [5,8,15]. The presence of the vicus, Voghenza (with houses, necropolis, and brick furnaces) (http://www. archeobologna.beniculturali.it/Ferrara/area.htm#Necropoli_Romana_di_Voghenza), and the site of the necropolis of the Fadieni in Gambulaga (http://www.archeobologna.beniculturali.it/mostre/gambulaga. htm), connected by rivers and channels, already demonstrate the remarkable diffusion of the Roman and Late Roman Anthropic Phase [14]. The river was a jointing natural element used for transport, commerce, and every day economic life. Reading the local stratigraphy, we see the Eridanus bank developed on a multilevel structure, mainly natural, with artificial devices.
In Voghiera, for example, we see some layers of sand, coming from overflow of the river ( Figure 3) [5,8,15].
Moving to South, and going to Gambulaga, in Tramonoto Lake (Figure 4), after detecting the morphology and direction of the north bank margin, with underwater surveys with a direct draw on site, it is possible to see the stratigraphy in a largely preserved state, despite the dredging works of the old dismissed sand quarry. To define a microstratigraphy for a better comprehension we completed some geoarchaeological drillings (for a detailed description, please see bibliography [4,16]).
The sedimentology interpretation describes an upper modern level of silty clay covering a system of palaeosoils and alluvial layers. Three main anthropized levels are attested on site: at −3.15 m a grey compact clay anthropic stratum (Late Antique), at −5.40 m a thin violet clay layer with micro-carbonaceous cores and vegetal traces (palaeosoil-Roman Imperial Phase), at −6.10 m a thick violet silty clay level with micro-carbonaceous cores and vegetal traces (palaeosoil-perhaps belonging to Protohistory). Following the slope of the actual bank, underwater, we see debris and accumulation of wood, trunk and fictile pieces belonging to Roman and Late Roman Period. On the Late Antique-Middle Ages levels there are some big trunks and parts of amphora. Thanks to our geo-archaeological computation, we reconstruct a synthesis of local stratigraphy with metrical references ( Figure 5).  Moving to South, and going to Gambulaga, in Tramonoto Lake (Figure 4), after detecting the morphology and direction of the north bank margin, with underwater surveys with a direct draw on site, it is possible to see the stratigraphy in a largely preserved state, despite the dredging works of the old dismissed sand quarry. To define a microstratigraphy for a better comprehension we completed some geoarchaeological drillings (for a detailed description, please see bibliography [4,16]).   Moving to South, and going to Gambulaga, in Tramonoto Lake ( Figure 4), after detecting the morphology and direction of the north bank margin, with underwater surveys with a direct draw on site, it is possible to see the stratigraphy in a largely preserved state, despite the dredging works of the old dismissed sand quarry. To define a microstratigraphy for a better comprehension we completed some geoarchaeological drillings (for a detailed description, please see bibliography [4,16]).  Protohistory). Following the slope of the actual bank, underwater, we see debris and accumulation of wood, trunk and fictile pieces belonging to Roman and Late Roman Period. On the Late Antique-Middle Ages levels there are some big trunks and parts of amphora. Thanks to our geo-archaeological computation, we reconstruct a synthesis of local stratigraphy with metrical references ( Figure 5). Regarding the discussion of the site we invite you to read our 2018 reportage [4]. Our focus now is going on the wood findings. During the underwater surveys we documented not only the wood structure off the Late Roman bank, but also the presence of very big trunks all oriented in the direction of the river current, clear evidence of a large flood that swept over the river edges. Together with the botanical findings, we have found pottery fragments belonging to different classes of objects: amphorae, containers for daily use, fragments of bricks, tiles and bricks ( Figure 6 and Figure 7)).  Regarding the discussion of the site we invite you to read our 2018 reportage [4]. Our focus now is going on the wood findings. During the underwater surveys we documented not only the wood structure the Late Roman bank, but also the presence of very big trunks all oriented in the direction of the river current, clear evidence of a large flood that swept over the river edges. Together with the botanical findings, we have found pottery fragments belonging to different classes of objects: amphorae, containers for daily use, fragments of bricks, tiles and bricks ( Figures 6 and 7)).
Middle Ages levels there are some big trunks and parts of amphora. Thanks to our geo-archaeological computation, we reconstruct a synthesis of local stratigraphy with metrical references ( Figure 5). Regarding the discussion of the site we invite you to read our 2018 reportage [4].
Our focus now is going on the wood findings. During the underwater surveys we documented not only the wood structure off the Late Roman bank, but also the presence of very big trunks all oriented in the direction of the river current, clear evidence of a large flood that swept over the river edges. Together with the botanical findings, we have found pottery fragments belonging to different classes of objects: amphorae, containers for daily use, fragments of bricks, tiles and bricks ( Figure 6 and Figure 7)).

Materials and Methods
Our research was completed thanks to a great scientific synergy between many disciplines: mainly geology, archaeology and history, and palaeobotany from work in the libraries and at university, to the survey activities, with the help of remote sensing and geomatics (regarding remote sensing in landscape archaeology and studying relations between natural environment and archaeology, see the work of Campana Recording concerning the integration of new and old research methods [17]). Remote sensing technology has been applied through different instruments. On the land context, such as river banks, indirect studies begun by measuring elevation levels of the river coastal zones, areas of over flow, subject to natural rising up [18,19].
From a technical point of view, once established the topographical points, in Google Earth Pro, opening "ruler", after positioning and saving a line with a name (we choose a sector of Km 1, corresponding to the section we need), we moved to "Modify" and selected "Show elevation profile"; in the lower part of the video a monochromatic cross section of the site appears, including a narrow indicating the check point position. This function is very useful and enables a very easy understanding of the local geomorphology. We detected the height of the river edges: a crucial datum for the occupation and anthropic development of housing and commercial system. In addition, the activity of transport with the towpath took place on the banks. The helciarius was walking with quadrupeds on the bank, holding a rope with which boats are towed from the ground along a waterway.
In our case we realized four sections (length Km 100 ca.), individuating the highest topographical areas, attesting river depositional layers, fluvial islands and main banks. The North margin of the Eridanus is the key point for the comprehension of the ancient anthropogenic living/residential system during the Roman Period and Middle Ages. We detected a height above sea level between 3 and 2.5 m (Figure 8).

Materials and Methods
Our research was completed thanks to a great scientific synergy between many disciplines: mainly geology, archaeology and history, and palaeobotany from work in the libraries and at university, to the survey activities, with the help of remote sensing and geomatics (regarding remote sensing in landscape archaeology and studying relations between natural environment and archaeology, see the work of Campana Recording concerning the integration of new and old research methods [17]). Remote sensing technology has been applied through different instruments. On the land context, such as river banks, indirect studies begun by measuring elevation levels of the river coastal zones, areas of over flow, subject to natural rising up [18,19].
From a technical point of view, once established the topographical points, in Google Earth Pro, opening "ruler", after positioning and saving a line with a name (we choose a sector of Km 1, corresponding to the section we need), we moved to "Modify" and selected "Show elevation profile"; in the lower part of the video a monochromatic cross section of the site appears, including a narrow indicating the check point position. This function is very useful and enables a very easy understanding of the local geomorphology. We detected the height of the river edges: a crucial datum for the occupation and anthropic development of housing and commercial system. In addition, the activity of transport with the towpath took place on the banks. The helciarius was walking with quadrupeds on the bank, holding a rope with which boats are towed from the ground along a waterway.
In our case we realized four sections (length Km 1,00 ca.), individuating the highest topographical areas, attesting river depositional layers, fluvial islands and main banks. The North margin of the Eridanus is the key point for the comprehension of the ancient anthropogenic living/residential system during the Roman Period and Middle Ages. We detected a height above sea level between 3 and 2.5 m (Figure 8).
For a better comprehension of the ancient settlement system we constructed 4 3D plan-views, corresponding to the investigated areas thank to 3D Mapper (Figure 9). For a better comprehension of the ancient settlement system we constructed 4 3D plan-views, corresponding to the investigated areas thank to 3D Mapper (Figure 9).  For a better comprehension of the ancient settlement system we constructed 4 3D plan-views, corresponding to the investigated areas thank to 3D Mapper (Figure 9).  The geocomputation of the morphological sections supported by 3d plan-views show very well the altitude differences between the river edges, raised by the alluvial deposits, the old cut of the Eridanus river bed (actually lakes), and the system of small bumps on which the inhabited area has settled, as well places occupied by forest and sylvae.
Because of the strong presence of trunks and roots in the Lakes Campanella and Tramonto, knowing the underwater archaeological situation and the troubles of visibility, after some underwater direct investigations, we proceeded with echo side scan sonar surveys. We used an integrated instrument, echo sound scan sonar Humminbird 1198c SI Combo, reading data with the software HumViewer. The software while displaying the swath, allows us to measure the dimensions of findings and anomalies, thanks to the side image visualization thought utilities measure length/distance ( Figure 10).
The documentation of the trunks was particularly complex due to the poor visibility on the lake bottom linked to the presence of algae and very fine clay in suspension [20]. For this reason, remote sensing investigations were very useful for the positioning and measurement of artificial and natural findings: it was impossible to work with a buddy system because of safety between divers and incompatibility of visual communication.
The software is free o line (http://humviewer.cm-johansen.dk/) and offers an easy approach to elementary geomatic measurements. The trunks are detectable as anomalies on the bottom of the lake, because of their shape and dislocation, generating shadows and showing anomalous morphology compared to the sedimentology on site.
Thanks to the echo side scan sonar and relative reading software, we were able to detect the lengths and diameters of the giant trunks directly in the studio, using a computer.
In Lake Tramonto, seven large tree trunks, numerous branches and twigs have been identified. Some of them bear traces of binding and processing.
The data fusion of the elements coming from direct and indirect investigations was completed by computer Asus Tuf with Intel COREi7, 8th Gen (2019), with Windows 10 for a multitask elaboration, integrating remote sensing technologies for the interpretation of landscape and waterscape ecosystems [21]).
Heritage 2020, 3 8 The geocomputation of the morphological sections supported by 3d plan-views show very well the altitude differences between the river edges, raised by the alluvial deposits, the old cut of the Eridanus river bed (actually lakes), and the system of small bumps on which the inhabited area has settled, as well places occupied by forest and sylvae.
Because of the strong presence of trunks and roots in the Lakes Campanella and Tramonto, knowing the underwater archaeological situation and the troubles of visibility, after some underwater direct investigations, we proceeded with echo side scan sonar surveys. We used an integrated instrument, echo sound scan sonar Humminbird 1198c SI Combo, reading data with the software HumViewer. The software while displaying the swath, allows us to measure the dimensions of findings and anomalies, thanks to the side image visualization thought utilities measure length/distance (Figure 10). The documentation of the trunks was particularly complex due to the poor visibility on the lake bottom linked to the presence of algae and very fine clay in suspension [20]. For this reason, remote sensing investigations were very useful for the positioning and measurement of artificial and natural

Discussion
Big arboreal finds were discovered in Lago Campanella and in Lago Tramonto. Particular attention should be paid to long oak trunks, which are important for length and diameter, attributable as habitat to the local or nearby forest, and from an archaeological point of view to the raw material to build pirogues.
Seven Heritage 2020, 3 9 findings: it was impossible to work with a buddy system because of safety between divers and incompatibility of visual communication.
The software is free o line (http://humviewer.cm-johansen.dk/) and offers an easy approach to elementary geomatic measurements. The trunks are detectable as anomalies on the bottom of the lake, because of their shape and dislocation, generating shadows and showing anomalous morphology compared to the sedimentology on site.
Thanks to the echo side scan sonar and relative reading software, we were able to detect the lengths and diameters of the giant trunks directly in the studio, using a computer.
In Lake Tramonto, seven large tree trunks, numerous branches and twigs have been identified. Some of them bear traces of binding and processing.
The data fusion of the elements coming from direct and indirect investigations was completed by computer Asus Tuf with Intel COREi7, 8th Gen (2019), with Windows 10 for a multitask elaboration, integrating remote sensing technologies for the interpretation of landscape and waterscape ecosystems [21]).

Discussion
Big arboreal finds were discovered in Lago Campanella and in Lago Tramonto. Particular attention should be paid to long oak trunks, which are important for length and diameter, attributable as habitat to the local or nearby forest, and from an archaeological point of view to the raw material to build pirogues.
Seven  The big trees were used both to build means of transport (pirogue) for local traffic and for sale: perhaps there was a production centre of small wood boot, between Lake Campanella and Lake Tramonto (underwater, we found two bow or stern fragments, some starboards of monoxyle boats, and some partially excavated trunks) [12].
The  The big trees were used both to build means of transport (pirogue) for local traffic and for sale: perhaps there was a production centre of small wood boot, between Lake Campanella and Lake Tramonto (underwater, we found two bow or stern fragments, some starboards of monoxyle boats, and some partially excavated trunks) [12].
The trunks number 1 and number 5 are compatible with lengths and diameters (about 1.0 m) of the pirogues discovered in the Ferrara area (more than 23 exemplars are already known: Valle Isola, Valle Rillo, Valle Ponti, Valle Pega (all in Comacchio area), Pomposa (Codigoro), Codigoro, Valle Volta (Massafiscaglia), Valle delle Gallare (Ostellato), Iolanda di Savoia. These boats, characterized by a common shape, similar measure, and the same kind of wood, can be traced back to the Late Antiquity and the Middle Ages [22,23] (Figure 12).
Heritage 2020, 3 10 by a common shape, similar measure, and the same kind of wood, can be traced back to the Late Antiquity and the Middle Ages [22,23] (Figure 12). The most evident comparison with similar botanical finds, still in the status of tree, quite similar in size and stratigraphic locations, are the woods from the nearby Campanella Lake (an artificial basin, born from quarry excavation in palaeowatercourse of the River Po) a few Km West of Lake Tramonto, located at the elbow of the meander of the ancient Po.
Very important studies for the Campanella lake were carried out by the University of Bologna during 1995, by L. Forlani and G. Nanni investigating the Sandalo wood fossil forest. After a cataloguing of 1519 wooden finds, including 147 trunks, 2 artefacts, 3 roots, 7 cork samples, 8 branches. There were parts of trees, shrubs, lianas, most of all deciduous broadleaf and conifer. In between the three main units identified by the palaeobotanists, the third sampling conserve elements dating back to the Roman period or the early Middle Ages [25]. The C14 analysis are dating traces back to a chronological span between the fourth and sixth century AD. The same chronology is attested by pottery findings, Late Roman V amphorae, found during direct underwater surveys.
In addition, the recent archaeological excavation in Comacchio (2014) [26], always on the palaeowatercoruse of the Eridanus, provided some information regarding the panorama of wood use for nautical means. The preliminary archaeobotanical analysis performed by M. Marchesini [27], superintendence palaeobotanist, on the planks of the sewn boat and on pieces of the monoxyl pirogue found close to the local bank, detected Oak wood (Quercus cf. robur -Fagaceae Family) and Elm (Ulmus -Ulmaceae family), respectively, the first to build the monoxyle pirogue, the second to build the boat. Considering the diffusion area of the plants from which the wood was obtained, it could be assumed that the river boat of Comacchio 2014 field http://www.archeobologna.beniculturali.it/fe_comacchio/imbarcazioni_2014.htm, was built in the Po area, northern than Santa Maria in Padovetere (exact location of the excavations). Elm trees were found also in Voghiera [28].
The monoxyle pirogue, given the construction type and the type of wood used, is likely to have been made in an area not too far from the place of discovery (Comacchio). Was it built in Gambulaga? Perhaps! The site might have been a pirogue factory, before the diluvium mentioned by Paulus Diaconus (Historia Langobardorum III.23). A Mediaeval iconographic support regarding pirogues The most evident comparison with similar botanical finds, still in the status of tree, quite similar in size and stratigraphic locations, are the woods from the nearby Campanella Lake (an artificial basin, born from quarry excavation in palaeowatercourse of the River Po) a few Km West of Lake Tramonto, located at the elbow of the meander of the ancient Po.
Very important studies for the Campanella lake were carried out by the University of Bologna during 1995, by L. Forlani and G. Nanni investigating the Sandalo wood fossil forest. After a cataloguing of 1519 wooden finds, including 147 trunks, 2 artefacts, 3 roots, 7 cork samples, 8 branches. There were parts of trees, shrubs, lianas, most of all deciduous broadleaf and conifer. In between the three main units identified by the palaeobotanists, the third sampling conserve elements dating back to the Roman period or the early Middle Ages [25]. The C14 analysis are dating back to a chronological span between the fourth and sixth century AD. The same chronology is attested by pottery findings, Late Roman V amphorae, found during direct underwater surveys.
In addition, the recent archaeological excavation in Comacchio (2014) [26], always on the palaeowatercoruse of the Eridanus, provided some information regarding the panorama of wood use for nautical means. The preliminary archaeobotanical analysis performed by M. Marchesini [27], superintendence palaeobotanist, on the planks of the sewn boat and on pieces of the monoxyl pirogue found close to the local bank, detected Oak wood (Quercus cf. robur -Fagaceae Family) and Elm (Ulmus-Ulmaceae family), respectively, the first to build the monoxyle pirogue, the second to build the boat. Considering the diffusion area of the plants from which the wood was obtained, it could be assumed that the river boat of Comacchio 2014 field -http://www.archeobologna.beniculturali.it/fe_ comacchio/imbarcazioni_2014.htm, was built in the Po area, northern than Santa Maria in Padovetere (exact location of the excavations). Elm trees were found also in Voghiera [28].
The monoxyle pirogue, given the construction type and the type of wood used, is likely to have been made in an area not too far from the place of discovery (Comacchio). Was it built in Gambulaga? Perhaps! The site might have been a pirogue factory, before the diluvium mentioned by Paulus Diaconus (Historia Langobardorum III.23). A Mediaeval iconographic support regarding pirogues construction is offered by the Bayeux Tapestry ( Figure 13).
To complete the palaeobotany panorama, we need to add data coming from analysis performed by F. Facchini, University of Ferrara working on the sedimentological characterization of the samples catalogued during 2017 campaign [30]. In many samples we see the presence of seeds belonging to flora palustris (marsh flora), typical of inland waters, attesting an inter-distributive environment complex surviving on the northern side of the Eridanus bank itself in Gambulaga. The documented plants are floating hydrophytes, Nymphaea alba (White Water Lily), Sparganium erectum (Branched Bur-reed), helophytes Apium inondatum (Lesser Marshwort), and Typha latifolia (Bulrush).

Conclusions
The integrations of data coming from direct (surveys on sites, on land and underwater) and indirect investigation (remote sensing, satellite data elaboration, 3D map computation), together with botanical analysis and ancient sources studies, demonstrate the remarkable role of scientific synergy applied on archaeological research. This chance of collaboration demonstrates how anthropogenic occupation of this central part of the Delta can be traced back to Roman Imperial and to Late Antique Period: forests were not exclusively areas of woodland. They were being exploited for providing food, as fuel for furnaces for production of bricks, tiles (Pansiana production [4,12,13]) and glass making (from the area of Tramonto Like there is a pottery lamp decorated with the image of a local glass maker working at his furnace [31]), for manufacturing wooden goods, especially boats, and a means of water transport and carpentry.
The actual status of the river, surviving only as palaeo-watercourse, partially occupied by ex quarries of sand, conserves useful data for the reconstruction of the Late Antique phase. Certainly, the Eridanus, as one of the major rivers, was serving as communication corridor across the Southern Delta reaching the Adriatic Sea; it was a commercial route, more than a territorial dividing device.
The evidence attested between Lago Campanella and Lago Tramonto with a river level packed full of timber, testify the presence of the forest alongside the Eridanus. Many trunks come drifting down with the river. There are also sequences of uprights which mark the big destructive flow of the sixth century, reported by ancient sources. The data fusion allowed us to reconstruct a full botanical local context.
The Late Antique -Mediaeval silva was growing along the rivers, with Populus, Ulmus, Salix, Quercus, Alnus glutinosa, Juglans regia, Juniperus communis, Prunus (Poplar, Elm, Willow, Oak, Alder, Walnut, Juniper), Cherry Laurel). In between fluvial islands and meanders, small lakes and ponds housed marsh flora with floating plants and flowers like Nymphaea alba, Apium inondatum, Typha latifolia, Sparganium erectum (White Water Lily, Lesser Marshwort, Bulrush, Branched Bur-reed), giving birth to a locus amoenus (a beautiful place with trees, grass, fruits, flowers and water, Figure  14). To complete the palaeobotany panorama, we need to add data coming from analysis performed by F. Facchini, University of Ferrara working on the sedimentological characterization of the samples catalogued during 2017 campaign [30]. In many samples we see the presence of seeds belonging to flora palustris (marsh flora), typical of inland waters, attesting an inter-distributive environment complex surviving on the northern side of the Eridanus bank itself in Gambulaga. The documented plants are floating hydrophytes, Nymphaea alba (White Water Lily), Sparganium erectum (Branched Bur-reed), helophytes Apium inondatum (Lesser Marshwort), and Typha latifolia (Bulrush).

Conclusions
The integrations of data coming from direct (surveys on sites, on land and underwater) and indirect investigation (remote sensing, satellite data elaboration, 3D map computation), together with botanical analysis and ancient sources studies, demonstrate the remarkable role of scientific synergy applied on archaeological research. This chance of collaboration demonstrates how anthropogenic occupation of this central part of the Delta can be traced back to Roman Imperial and to Late Antique Period: forests were not exclusively areas of woodland. They were being exploited for providing food, as fuel for furnaces for production of bricks, tiles (Pansiana production [4,12,13]) and glass making (from the area of Tramonto Like there is a pottery lamp decorated with the image of a local glass maker working at his furnace [31]), for manufacturing wooden goods, especially boats, and a means of water transport and carpentry.
The actual status of the river, surviving only as palaeo-watercourse, partially occupied by ex quarries of sand, conserves useful data for the reconstruction of the Late Antique phase. Certainly, the Eridanus, as one of the major rivers, was serving as communication corridor across the Southern Delta reaching the Adriatic Sea; it was a commercial route, more than a territorial dividing device.
The evidence attested between Lago Campanella and Lago Tramonto with a river level packed full of timber, testify the presence of the forest alongside the Eridanus. Many trunks come drifting down with the river. There are also sequences of uprights which mark the big destructive flow of the sixth century, reported by ancient sources. The data fusion allowed us to reconstruct a full botanical local context.