ORIGINAL RESEARCH article

Front. Mar. Sci., 29 March 2022

Sec. Marine Biology

Volume 9 - 2022 | https://doi.org/10.3389/fmars.2022.856979

The Portuguese Man-of-War Has Always Entered the Mediterranean Sea—Strandings, Sightings, and Museum Collections

  • 1. Department of Biological, Geological and Environmental Sciences, University of Catania, Catania, Italy

  • 2. Ente Fauna Marina Mediterranea, Avola, Italy

  • 3. Department of Biological, Chemical and Pharmaceutical Sciences and Technologies, University of Palermo, Palermo, Italy

  • 4. Instituto de Ciencias Marinas de AndalucĂ­a, Consejo Superior de Investigaciones Cientificas, Cádiz, Spain

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Abstract

A search of records from different kinds of sources namely, scientific and grey literature, social media, and zoological museum collections, has been carried out to review the incidence of Physalia physalis (Linnaeus, 1758), the Portuguese man-of-war, in the Mediterranean Sea. The temporal frame of the records, considered valid if documented with images or collected specimens, ranged from the second half of the eighteenth century to the year 2021. Thanks to colonies preserved in some Italian historical museum collections, originating from the western basin, it was possible to date the putative first documented record of P. physalis of the Mediterranean Sea in 1850. The dataset shows some massive strandings that occurred in localities of the Strait of Gibraltar and Alboran Sea, the area of the entrance, from the Atlantic toward the Mediterranean waters, and the starting point from where the species spread toward the western and central basin. Physalia physalis does not reach the eastern area of the Mediterranean Sea. As the records of this species from the Italian maritime regions were abundant in the summertime and considering the danger related to contact with humans, they were subdivided into three categories of risk according to the months of occurrence. These categories were created to assign a level of danger for swimmers. The increasing sightings of such a poisonous cnidarian in coastal waters can represent a risk to human health, and a threat to all those activities linked to the marine tourism sector. The overview given goes beyond scientific purposes and aims to reach society and public administrators. The involvement of citizens and touristic structures for the early detection of P. physalis can play a key role in preventing encounters with the species, allowing marine tourist facilities to operate within a range of reasonable security.

Introduction

The presence or even the blooms of gelatinous zooplankton (cnidarians, ctenophores, and pelagic tunicates) can have several negative impacts on ecosystems, on the economy (e.g., tourism, fisheries, aquaculture) and human health (Boero et al., 2008; De Donno et al., 2014; Bosch-Belmar et al., 2017; Marambio et al., 2021). About this latter aspect, it is well-known that zooplanktonic cnidarians, commonly named jellyfish, can generate serious wounds and poisoning to humans, and in some cases death (Burnett and Gable, 1989; Burke, 2002). However, since this gelatinous zooplankton is not usually targeted by fisheries and not easily surveyed or collected by research activities, data on dispersal and impact on human life are sometimes lacking (Condon et al., 2012; De Donno et al., 2014; Rossi et al., 2019; Gravili and Rossi, 2021). Hence, we cannot state with absolute certainty for several species that a general increase of their abundance is occurring or will occur in a specific region. In this regard, Citizen Science and local public networks can be of great help in collecting data on a large spatial-temporal scale in order to better understand the dynamics of jellyfish populations, as demonstrated by several projects (Boero et al., 2010; Baumann and Schernewski, 2012; Fleming et al., 2013; Bellido et al., 2020; Gutiérrez-Estrada et al., 2021; Marambio et al., 2021), though some species remains overlooked, such as Physalia physalis (Linnaeus, 1758).

One of the most dangerous pelagic species in the Mediterranean Sea is the Portuguese man-of-war, P. physalis, a pleustonic colonial organism rarely observed in the open Mediterranean basin, whose direct observations mainly concern stranded specimens (Berdar and Cavallaro, 1980; Deidun, 2010; Boero, 2013; Prieto et al., 2015; Castriota et al., 2017; Mghili et al., 2020; Deidun et al., 2020; Macías et al., 2021). This species, belonging to the Cnidarian group—order Siphonophores, is part of the floating community of ocean organisms that live at the interface between water and air (Boero, 2013; Munro et al., 2019). Though the whole body seems a single individual, it is a colony in which small individuals (zooids) perform different functions such as floating, feeding, defence and reproduction (Lane, 1960). The structure of the colony is complex; on the whole, it can be described as composed of two portions: a portion visible floating on the ocean surface—pneumatophore—and a not visible tentacular portion expanding below the water surface—the complex of zooids (Munro et al., 2019).

Physalia physalis is easily recognized by its bluish pneumatophore, an air bladder developed from one of the zooids that can reach 30 cm in length (Bardi and Marques, 2007; Munro et al., 2019), surmounted by a crest that acts like a sail that helps to navigate and float on the surface of the sea (Lane, 1960; Iosilevskii and Weihs, 2009). The tentacles of this species, maybe up to 30 m long and containing more than 750,000 stinging cells each (Munro et al., 2019), contain the “physaliatoxin” (Bardi and Marques, 2007) that is the cause of its painful sting, which causes a series of symptoms, ranging from local skin necrosis to neurological and cardiorespiratory problems that can cause death (Labadie et al., 2012). Furthermore, unlike other cnidarian species, the Portuguese man-of-war nematocysts seem to penetrate surgical gloves (Pierce, 2006). Physalia physalis behaves like a predator, plays an important ecological role and influences the abundance of populations of small animals, in particular juveniles of fishes and larvae that it captures with tentacles (Purcell, 1984). On the other hand, the species can be preyed upon by fishes, turtles, lepadomorph barnacles, and glaucid nudibranchs (Wangersky and Lane, 1960; Bieri, 1966; Thompson and Bennett, 1970; Arai, 2005), and other taxa not disclosed yet (Arai, 2005).

Physalia physalis is a cosmopolitan species, distributed from tropical to temperate waters roughly comprised from 51°N to 38°S (Shannon and Chapman, 1983; Kirkpatrick and Pugh, 1984; Haddad et al., 2002; Elston, 2007; Pontin et al., 2011; Oliveira et al., 2016). The species is surface-dwelling thanks to the chamber filled with air and carbon monoxide which represents a sail, thus the colony moves with the prevailing wind (Mapstone, 2014).

It is interesting to underline that the cohorts of P. physalis originate from unknown marine georeferenced points (Graham et al., 2001; Ferrer and Pastor, 2017; Ferrer and González, 2021). These colonies move toward coastal areas, where they find optimal trophic conditions, and float along the shoreline, as a consequence of the direction and energy of prevailing winds and surface currents (Ferrer and Pastor, 2017). Thus, the continuously updating of records is much relevant to foresee the dispersal routes.

Up to date, the first documented record of P. physalis for the Mediterranean Sea dates back to 1980 (Berdar and Cavallaro, 1980). The species has been subsequently reported sporadically, in the western and central basins, mostly around Sicily and Malta (Deidun, 2010; Deidun et al., 2020; Boero, 2013). The latest records in Sicily date back to 2019 and 2021, in the Aegadian Sicilian Islands (Deidun et al., 2020) and Donnalucata (Sicily), respectively.

Gathering the baseline information on this species records over time and space constitutes an important task for the elaboration of management programs aimed to alert the local human population and touristic structures (MacĂ­as et al., 2021). Physalia physalis represents an important species to be aware of, and for which dissemination of data about its presence should be improved.

Here we introduce a dataset of sightings, strandings, and museum records of the species in the Mediterranean Sea, and the first documented Mediterranean records, originating from the southern Tyrrhenian basin. Relevant biodiversity information can be obtained from materials and data collected in the past and preserved in the Natural History Museums, which can provide overlooked and, in many cases, still unpublished data (Tedesco et al., 2020; Lo Brutto et al., 2021). Additionally, the sightings and strandings herein reported highlight the potential role of the citizens’ participatory science. The data from social media and local Citizen Science projects can have a key role if well-managed; the information is often uploaded on the web but not archived in the scientific literature or summarized in any report, thus risking being lost. The case of P. physalis fills such a gap.

The paper gives an overview on (i) the first records of P. physalis in the Mediterranean Sea through analysis of zoological collections; (ii) the recent records detected in the literature and data from civil society; (iii) the recent records in Italian waters and an assessment of risk for humans.

All data here reported can represent an important reference point for the development of models and predictive tools based on the presence, abundance, and jellyfish trends over a large timeframe.

Materials and Methods

A survey on the presence of P. physalis in the Mediterranean Sea was carried out. Information was obtained from scientific and grey literature, from the web and social media (mainly Facebook, Instagram and Twitter) and analysed.

As the zoological records of museum collections are not reported in the literature, a further search of historical museum specimens in Italy and Malta was integrated to find out old data never published. In particular, information was acquired from the Natural History Museum of the University of Florence, Italy, the “Darwin Dohrn” Museum of the Anton Dohrn Zoological Station of Naples, Italy, the Museum of Zoology “P. Doderlein” of the University of Palermo, Italy, the Museum of the Department of Biology of the University of Malta, Malta, and the Museum of Zoology, University of Cagliari, Italy. A very recent record of the species is preserved at the Civic Museum of Natural History of Comiso, Italy.

For each source, only information documented with images or collected specimens were validated for the aims of the present study. The records were assigned to the main Mediterranean sectors based on the sampling locality; from west to east: Strait of Gibraltar, Alboran Sea, Algerian-Balearic Sea, Western Mediterranean, Liguro-Provençal basin, Central Tyrrhenian Sea, Southern Tyrrhenian Sea, Channel of Sicily, Strait of Messina.

In accordance with the results by Macías et al. (2021), apart from the Spanish coast, the colonies in the summer period are more frequent in the southern Italian zone. Consequently, the records from the Italian maritime regions were subdivided into three “categories of risk” according to the season of occurrence. The records of P. physalis detected in February-March were included in the low-risk category; the records occurred in April-May in the medium-risk one; the records happened in June-August in the high-risk category. These categories were created to designate a level of danger for swimmers in such a particular area, specifically it was assumed that the sightings of P. physalis in the summer period (June-August) could be considered the most dangerous (high-risk), according to the higher number of swimmers than the remaining months of the year; while medium and low-risk were associated to a lower frequency of human activities accordingly. The records from this zone belonging to the three categories of risk were counted and grouped following the biogeographical sectors proposed by Bianchi (2004). A final map showed such clustering.

Results

We can assert that at least 8,744 colonies of P. physalis entered the Mediterranean Sea, in a timescale comprised between 1850 and 2021 (August). Thirteen colonies were counted in the museum collections explored, 8,346 colonies were counted from scientific literature, information about 16 colonies was found on the web, and 369 records are herein published for the first time. Most of the colonies were reported stranded. The highest incidence was recorded in the Alboran Sea, in a limited area extending from the Strait of Gibraltar to the Algerian-Balearic Sea; while the central Mediterranean area was the one where P. physalis mainly spread (Table 1). None information was found from the Eastern Mediterranean, Adriatic Sea and Aegean and Levantine basin.

All data are shown in Table 1; the records are listed according to chronological order, and each locality is associated with a marine sector indicated by a point in the map of Figure 1 (see the ID numbers). The marine sectors where P. physalis was been recorded are the following: Strait of Gibraltar (corresponding to the ID number 1 on the map of Figure 1), Alboran Sea (ID 2), Algerian-Balearic Sea—Western Mediterranean (ID 3 and 4), the Liguro-Provençal basin (ID 4 and 5), coastline of Corsica—Liguro-Provençal basin (ID 6 and 8), the coastline of Sardinia—Western Mediterranean (ID 7), Tunisian waters—Channel of Sicily (ID 9 and 10), Pelagie Archipelago—Channel of Sicily (ID 11), Northern Tyrrhenian Sea (ID 12), Aegadian Archipelago – Southern Tyrrhenian Sea (ID 13), Southern Tyrrhenian Sea (ID 14), Central Tyrrhenian Sea (ID 15), Maltese Archipelago—Channel of Sicily (16), Strait of Messina (17) (Table 1 and Figure 1).

The First Mediterranean Records of Physalia physalis

Due to the scarcity of scientific literature documenting the presence of Physalis physalis in the past, some of the oldest zoological museum collections in Italy, which preserve specimens collected in the western area, were explored. The aim was to track down the first records of P. physalis in the Mediterranean Sea.

TABLE 1

YearMonthLocalityMediterranean
marine sector
ID on mapDocumentedNumber of coloniesCoordinates/link to coordinates
References
LatLon
1850UnknownNice (France)Liguro-Provençal basin5Yes143.6975517.265345Present paper MZUF
1863UnknownLivorno (Italy)Liguro-Provençal basin5Yes143.54057810.279674Present paper MZUF
1914UnknownGulf of Naples (Italy)Central Tyrrhenian Sea15Yes240.81462514.271982Present paper DDM
Antecedent 1972UnknownGulf of Naples (Italy)Central Tyrrhenian Sea15Yes540.81462514.271982Present paper DDM
Antecedent 1980UnknownGulf of Palermo (Italy)Southern Tyrrhenian Sea14Yes138.13799513.391992Present paper MZPA
1980FebruaryCoast of Messina (Italy)Strait of Messina17Yes138.24734615.625401Berdar and Cavallaro, 1980 MDBM
2001MayGolden Bay (Malta)Maltese Archipelago Channel of Sicily16Yes135.93455114.343233Deidun, 2010
2008AugustMálaga, Granada (Spain)Alboran Sea2Yes12https://static-content.springer.com/esm/art%3A10.1038%2Fsrep11545/Media Objects/41598_2015_BFsrep11545 _MOESM1_ESM.pdfPrieto et al., 2015
2009April-JulyMurcia (Spain)Algerian-Balearic Sea3Yes67https://static-content.springer.com/esm/art%3A10.1038%2Fsrep11545/Media Objects/41598_2015_ BFsrep11545_MOESM1_ESM.pdfPrieto et al., 2015
2009JuneCeuta (Spain)Strait of Gibraltar1Yes3https://static-content.springer.com/esm/art%3A10.1038%2Fsrep11545/MediaObjects/41598_ 2015_BFsrep11545_MOESM1_ESM.pdfPrieto et al., 2015
2009FebruaryGolden Bay (Malta)Maltese Archipelago Channel of Sicily16Yes135.93617814.343233Deidun, 2010 And P. J. Schembri pers. comm.
2009AprilMgarr ix-Xini; Cirkewwa (Malta)Maltese Archipelago Channel of Sicily16Yes236.02017314.271735Deidun, 2010
35.98840214.326594And P. J. Schembri pers. comm.
2009JulyGhar Lapsi (Malta)Maltese Archipelago Channel of Sicily16Yes135.82747414.424703Deidun, 2010 And P. J. Schembri pers. comm.
2009MarchCapo Peloro (Italy)Strait of Messina17Yes238.26499715.651731Castriota et al., 2017
2009AprilLampedusa Island (Italy)Pelagie Archipelago Channel of Sicily16Yes135.51328412.557236Castriota et al., 2017
2009AugustCrystal Lagoon,Maltese Archipelago16Yes136.01034614.327940Deidun, 2010
Comino (Malta)Channel of Sicily
2010February-JulyCadiz and Ceuta (Spain)Strait of Gibraltar1Yes161https://static-content.springer.com/esm/art% 3A10.1038%2Fsrep11545/MediaObjects/41598 _2015_BFsrep11545_MOESM1_ESM.pdfPrieto et al., 2015
2010MarchMálaga, Granada (Spain)Alboran Sea2Yes316https://static-content.springer.com/esm/art% 3A10.1038%2Fsrep11545/MediaObjects/41598 _2015_BFsrep11545_MOESM1_ESM.pdfPrieto et al., 2015
2010March-JulyAlmeria, Murcia, Alicante (Spain)Algerian-Balearic Sea3Yes363https://static-content.springer.com/esm/art% 3A10.1038%2Fsrep11545/MediaObjects/41598 _2015_BFsrep11545_MOESM1_ESM.pdfPrieto et al., 2015
2010March-JuneCirkewwa; St. ThomasBay; Xlendi (Malta)Maltese Archipelago Channel of Sicily16Yes335.98840214.326594Deidun, 2010
35.85208814.566352
36.02882614.213850
2010MarchN-E coast of Sicily (Italy)Strait of Messina17No1UnknownUnknownBoero, 2013
2010March-AugustTorre dei corsari; Funtanamare; Island San Pietro; Villaputzu (Italy)coastline of Sardinia Western Mediterranean7No4UnknownUnknownBoero, 2013
2010March-AugustGozo Island (Malta)Maltese Archipelago16No2UnknownUnknownBoero, 2013
Channel of Sicily
2010June-AugustCorsica Island (France)Coastline of Corsica06-AugNo2UnknownUnknownBoero, 2013
Liguro-Provençal basin
2010JulySant’Antioco Island (Italy)Coastline of Sardinia Western Mediterranean7Yes138.9676098.439221Present paper MZCA
2010JulyPorto Ercole (Italy)Northern Tyrrhenian Sea12No1UnknownUnknownBoero, 2013
2010JulySicily (Italy)Southern Tyrrhenian Sea14No1UnknownUnknownBoero, 2013
2011JanuaryCadiz (Spain)Strait of Gibraltar1Yes1https://static-content.springer.com/esm/art% 3A10.1038%2Fsrep11545/MediaObjects/415 98_2015_BFsrep11545_MOESM1_ESM.pdfPrieto et al., 2015
2011JanuaryMálaga, Granada (Spain)Alboran Sea2Yes3https://static-content.springer.com/esm/art% 3A10.1038%2Fsrep11545/MediaObjects/415 98_2015_BFsrep11545_MOESM1_ESM.pdfPrieto et al., 2015
2011JanuaryAlicante (Spain)Algerian-Balearic Sea4Yes3https://static-content.springer.com/esm/art% 3A10.1038%2Fsrep11545/MediaObjects/415 98_2015_BFsrep11545_MOESM1_ESM.pdfPrieto et al., 2015
2011MarchSa Maison (Malta)Maltese Archipelago16Yes135.89499914.499521Deidun et al., 2020
Channel of Sicily
2012MarchBarcelona (Spain)Algerian-Balearic Sea4Yes8https://static-content.springer.com/esm/art% 3A10.1038%2Fsrep11545/MediaObjects/41 598_2015_BFsrep11545_MOESM1_ESM.pdfPrieto et al., 2015
2012MarchGhajn Tuffieha (Malta)Maltese Archipelago Channel of Sicily16Yes135.928234 35.92821714.343357 14.343260Deidun et al., 2020
2013February-AprilCadiz (Spain)Strait of Gibraltar1Yes121https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2013April/JulyMálaga, Granada (Spain)Alboran Sea2Yes425https://digital.csic.es/handle/10261/244755Macías et al., 2021
2013April/JuneAlmeria, Valencia (Spain)Algerian-Balearic area4Yes40https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2013JulyGnejna Bay (Malta)Maltese Archipelago16Yes135.92103914.342470Social network
Channel of Sicily
2014MarchCapo Peloro (Italy)Strait of Messina17Yes138.26499715.651731Castriota et al., 2017
2014AprilXlendi (Malta)Maltese Archipelago16Yes136.02943414.215403Deidun et al., 2020
Channel of Sicily
2014AprilLevanzo Island (Italy)Aegadian Archipelago13Yes138.01735712.331665Deidun et al., 2020
Southern Tyrrhenian Sea
2018FebruaryGranada (Spain)Alboran Sea2Yes13https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2018MarchCadiz and Ceuta (Spain)Strait of Gibraltar1Yes1125https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2018MarchGibraltar (UK)Strait of Gibraltar1Yes8https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2018MarchStrait of Gibraltar (Morocco)Strait of Gibraltar1Yes8See Table 1 in Mghili et al. (2020)Mghili et al., 2020
2018MarchMálaga, Granada (Spain)Alboran Sea2Yes397https://digital.csic.es/handle/10261/244755Macías et al., 2021
2018MarchAlmeria, Murcia (Spain)Algerian-Balearic Sea3Yes76https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2018AprilCadiz and Ceuta (Spain)Strait of Gibraltar1Yes1425https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2018AprilM’diq, Fnideq, Martil, Azla (Morocco)Strait of Gibraltar1Yes169See Table 1 in Mghili et al. (2020)Mghili et al., 2020
2018AprilGibraltar (UK)Strait of Gibraltar1Yes184https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2018AprilMálaga, Granada (Spain)Alboran Sea2Yes1474https://digital.csic.es/handle/10261/244755Macías et al., 2021
2018AprilAlmeria, Murcia, Alicante, Balearic Islands (Spain)Algerian-Balearic Sea3Yes1668https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2018MayMartil, M’diq, Fnideq (Morocco)Strait of Gibraltar1Yes46See Table 1 in Mghili et al. (2020)Mghili et al., 2020
2018MayCadiz (Spain)Strait of Gibraltar1Yes3https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2018MayMálaga, Granada (Spain)Alboran Sea2Yes53https://digital.csic.es/handle/10261/244755Macías et al., 2021
2018AprilAlmeria, Murcia, Balearic Islands (Spain)Algerian-Balearic Sea3Yes133https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2018MayGhasri valley, Gozo; Valletta Grand Harbour (Malta)Maltese Archipelago Channel of Sicily16Yes236.078960 35.90264314.228525 14.519831Deidun et al., 2020
2018MayFavignana Island (Italy)Aegadian Archipelago13Yes137.93849712.271064Deidun et al., 2020
Southern Tyrrhenian Sea
2018JuneMálaga, Granada (Spain)Alboran Sea2Yes4https://digital.csic.es/handle/10261/244755Macías et al., 2021
2018JuneAlmeria, Valencia (Spain)Algerian-Balearic Sea3Yes2https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2018JulyAlicante, Valencia, CastellĂłn (Spain)Algerian-Balearic Sea3Yes5https://digital.csic.es/handle/10261/244755MacĂ­as et al., 2021
2019January and AprilGhajn Tuffieha; North Comino Channel (Malta)Maltese Archipelago16Yes235,93008214,342845Deidun et al., 2020
Channel of Sicily36,02003714,335388
2019MarchCadiz (Spain)Strait of Gibraltar1Yes3https://digital.csic.es/handle/10261/244755Present paper
2019MarchAlicante, Valencia, CastellĂłn (Spain)Algerian-Balearic Sea3Yes9https://digital.csic.es/handle/10261/244755Present paper
2019April-MayCadiz (Spain)Strait of Gibraltar1Yes2https://digital.csic.es/handle/10261/244755Present paper
2019AprilGranada (Spain)Alboran Sea2Yes1https://digital.csic.es/handle/10261/244755Present paper
2019April-MayBalearic Islands (Spain)Algerian-Balearic Sea4Yes10https://digital.csic.es/handle/10261/244755Present paper
2019JuneCadiz, Ceuta (Spain)Strait of Gibraltar1Yes121https://digital.csic.es/handle/10261/244755Present paper
2019June-AugustAlmeria, Murcia, Alicante, Valencia, Balearic Islands (Spain)Algerian-Balearic Sea3Yes14https://digital.csic.es/handle/10261/244755Present paper
2019SeptemberBalearic Islands (Spain)Algerian-Balearic Sea4Yes1https://digital.csic.es/handle/10261/244755Present paper
2020MayBalearic Islands (Spain)Algerian-Balearic Sea4Yes1https://digital.csic.es/handle/10261/244755Present paper
2020MayS-W coastline of Sardinia Island (Italy)coastline of Sardinia Western Mediterranean7Yes139.7022758.454307Deidun et al., 2020
2020AugustCeuta (Spain)Strait of Gibraltar1Yes4https://digital.csic.es/handle/10261/244755Present paper
2020AugustGranada (Spain)Alboran Sea2Yes1https://digital.csic.es/handle/10261/244755Present paper
2021February- MarchCadiz (Spain)Strait of Gibraltar1Yes61https://digital.csic.es/handle/10261/244755Present paper
2021FebruaryBalestrate, N-W Sicily Island (Italy)Southern Tyrrhenian Sea14Yes138.04813012.997849Present paper
2021February-AprilMaamoura (Tunisia)Tunisian waters Channel of Sicily10Yes236.46340910.815337Social network/web
2021MarchBalearic Islands (Spain)Algerian-Balearic Sea4Yes2https://digital.csic.es/handle/10261/244755Present paper
2021MarchLampedusa Island (Italy)Pelagie archipelago Channel of Sicily11Yes235.50970412.563556Social network/web
2021MarchDonnalucata (Italy)Channel of Sicily16Yes136.75903514.629979Present paper
MSNC
2021March-AprilNabeul-Chebba (Tunisia)Tunisian waters Channel of Sicily10Yes236.43532610.712459Social network/web
2021AprilMálaga (Spain)Alboran Sea2Yes12https://digital.csic.es/handle/10261/244755Present paper
2021AprilRades; Amilcar Beach; Carthage; Bizerte (Tunisia)Tunisian waters Channel of Sicily9Yes636.77405310.298923Social network/web
36.87865210.347118
37.2823009.886873
2021AprilSan Pietro Island (Italy)Coastline of Sardinia7Yes139.2467988.248352Social network/web
Western Mediterranean
2021AprilCapo Peloro (Italy)Strait of Messina17Yes138.27136215.656095Social network
2021AprilMaltaMaltese Archipelago16Yes135.97549714.451138Social network
Channel of Sicily
2021April-MayAlmeria, Balearic Islands (Spain)Algerian-Balearic Sea4Yes63https://digital.csic.es/handle/10261/244755Present paper
2021JuneBalearic Islands (Spain)Algerian-Balearic Sea4Yes60https://digital.csic.es/handle/10261/244755Present paper

Records of Physalia physalis in the Mediterranean Sea, pointed out in the map of Figure 1.

The records are listed following a chronological order; year and month, when noticed, are specified. The locality and the marine sector are indicated, the last according to the biogeographical division of the Mediterranean Sea and Italian waters.

MZUF, Natural History Museum of the University of Florence, Italy; DDM, Darwin Dohrn Museumof the Anton Dohrn Zoological Station of Naples, Italy; MZPA, Museum of Zoology “P. Doderlein” of the University of Palermo, Italy; MDBM, Museum of the Department of Biology of the University of Malta; MZCA Museum of Zoology, University of Cagliari; MSNC, Comiso Natural History Museum.

FIGURE 1

FIGURE 1

Map of thePhysalia physalis records in the Mediterranean Sea (1850 – 2021). The black points with the ID number indicate the area where P. physalis was found. The localities reported in Table 1 are associated with the ID number of such areas according to a neighbouring criterion. The arrows indicate the model of the main surface currents present in the Mediterranean Sea, according to Millot (1999) and Poulain et al. (2012).

The oldest documented colonies in the Mediterranean Sea were collected in the north-western area. The oldest uncovered records are preserved at the Natural History Museum of the University of Florence, a colony collected near Nice, France, dated back to 1850 (Figure 2; acquired by Gal Frères in June 1884—MZUF-uncatalogued) and a colony sampled in front of Livorno in 1863 (A. Targioni Tozzetti collection–voucher code MZUF-Cnidaria 1208). In 1914 a colony was collected in the Gulf of Naples, now preserved at the “Darwin Dohrn” Museum of the Anton Dohrn Zoological Station in Naples (voucher code HYD001; Figure 3). Further, by consulting the archive of the Museum of Zoology “Pietro Doderlein” of the University of Palermo, it was also possible to date a colony of P. physalis, collected along the north-western coast of Sicily Island (southern Italy), in a period antecedent to 1980, around 1960 (Silvano Riggio pers. comm.) (voucher code MZPA-IM-545). Presumably, further five colonies, preserved at the “Darwin Dohrn” Museum of the Anton Dohrn Zoological Station in Naples (voucher codes HYD002A, HYD002B, HYD174) and lacking date of capture, can be dated in a period antecedent to 1972 (Andrea Travaglini pers. comm.).

FIGURE 2

FIGURE 2

The colony of P. physalis collected in Mediterranean French waters (Nice) in 1850, voucher code MZUF-uncatalogued, preserved at the Natural History Museum of the University of Florence (photo ©Saulo Bambi, Museo di Storia NaturaleUniversitàdeglistudi di Firenze).

FIGURE 3

FIGURE 3

The two colonies of P. physalis collected in the Gulf of Naples (Italy) in 1914, preserved at the “Darwin Dohrn” Museum of Naples (photo by Akira Kihara, Science Center, Hosei University, Tokyo; ©2007 Zoological Collection Database Stazione Zoologica “Anton Dohrn”).

All the colonies were found stored in glass jars and were in a good state of conservation.

Recent Records

The recent records here assumed are the ones reported from 1980 to 2021. The year 1980 was the year of the presumptive first Mediterranean record, as highlighted by Berdar and Cavallaro (1980), however not confirmed by the museum collections above listed. The specimens preserved in the zoological collections did not further corroborate a record that was presumptively thought of as the first on the north-western coast of Sicily. Such colony stranded on the 17th February 2021 (Balestrate beach, Gulf of Castellammare) was photographically documented (Figure 4) and is here stated as new information. It was found still alive and showed the typical bluish colour of the species; it measured approximately 20 cm in total length. Considering that the sail of P. physalis can reach 30 cm in total length, the colony can be considered of medium-large size (Wilson, 1947; Prieto et al., 2015). In the same year (2021), from February to April, P. physalis strandings occurred along the coast of Tunisia and Lampedusa Island (Channel of Sicily sector), in the Strait of Messina and the waters of Sardinia Island (Western Mediterranean sector) (Table 1 and Figure 1). The sightings were photographed and published on the web and social networks. On the 19th of August 2021, a colony was found stranded in Donnalucata (Channel of Sicily sector—Sicily). The colony is currently preserved at the Civic Museum of Natural History of Comiso. The pneumatophore has a length of 111 mm (Gianni Insacco pers. comm.).

FIGURE 4

FIGURE 4

The colony of P. physalis recorded in the north-western coast of Sicily, southern Tyrrhenian basin in 2021 (photo by Rosario Badalamenti).

The records of P. physalis successive to the 1980 start in 2001. There is a gap of 20 years, from 1980 to 2000.

In 2001, the presence of this species was documented in Malta Island, although local fishermen affirmed that they had encountered the species previously (Calleja, 2009). In Maltese waters, this species has been frequently registered: in May 2001, from February to August 2009, from March to June 2010, and in the period 2011-2020 [Patrick J. Schembri pers. comm.; Deidun (2010) and Deidun et al. (2020)]. The sample registered in May 2001, stranded in Golden Bay, Malta, is preserved in the Museum of the Department of Biology of the University of Malta (Patrick J. Schembri pers. comm.). In this latter period (2011–2020), two records were also reported from the Aegadian archipelago—Southern Tyrrhenian sector, and one from the Island of Sardinia—Western Mediterranean sector (Deidun et al., 2020; Table 1 and Figure 1).

In February-July 2010, 840 colonies were registered along the Spanish coast (Prieto et al., 2015). The Western Mediterranean basin experienced several swarms, recording hundreds of colonies in different sites on the Spanish coast (Alboran Sea sector). A colony captured along Sardinia coast is preserved at the Museum of Zoology of the University of Cagliari (Table 1); it represents a record that supports the information extrapolated from Boero (2013) of which documentation was not retrieved.

In the following years, 2011, 2012, and 2013, the number of sightings decreased significantly, in fact, lesser colonies were recorded in the same Spanish monitored sites (Prieto et al., 2015).

In 2018, between March and April, an increasing number of colonies of P. physalis were registered for the first time on the Mediterranean coast of Morocco—Alboran Sea—Algerian-Balearic Sea sectors (Mghili et al., 2020; Macías et al., 2021) (see Table 1).

The flow of P. physalis from the Atlantic Ocean toward the western Mediterranean basin seemed to be attributed to an unusual combination of meteorological and oceanographic factors during the winter period (Poulain et al., 2012; Prieto et al., 2015). In the spring of 2010 (Prieto et al., 2015), 2013 (MacĂ­as et al., 2021), 2018 (Mghili et al., 2020; MacĂ­as et al., 2021; Prieto, 2021), 2019 and 2021 intense strandings were recorded in the Alboran Sea area, probably due to the action of the Western Alboran Gyre (WAG) and Eastern Alboran Gyre (EAG) (Poulain et al., 2012). Such surface currents of the Alboran Sea can behave also as physical barriers to the flow toward the western Mediterranean, as suggested by Prieto et al. (2015), limiting the easternmost circulation of a large number of P. physalis colonies. Only a few colonies that escape the front manage to circulate by the benefit of the surface currents present in the Mediterranean Sea (Poulain et al., 2012). By creating a map of the P. physalis records documented in the last century, and superimposing it with the trajectories of the surface currents that drive the colonies (Poulain et al., 2012), it has been shown a general pattern of occurrence of the Portuguese man-of-war within the Mediterranean Sea (Figure 1).

Records of Physalia physalis in the Italian Maritime Regions

A portion of the records of P. physalis was grouped in four Italian biogeographical sectors: Sardinian waters, Channel of Sicily, Tyrrhenian Sea, Strait of Messina, mainly around the Sicily Island, central Mediterranean. Such sectors are the ones supposed by MacĂ­as et al. (2021) as the zone where the species mainly occurs in the summer period; thus the clustering was arranged to identify those marine areas most affected by P. physalis sightings and strandings. The validated records of P. physalis were subdivided into three categories of risk (Figure 5) according to the season of occurrence and the level of danger for swimmers.

FIGURE 5

FIGURE 5

A schematic clustering of the records of P. physalis in the Italian maritime zone (see Table 1 for details); the records were aggregated in four different geographic sectors (from west to east, Sardinian waters; Channel of Sicily; Tyrrhenian Sea;Strait of Messina), and categorizedto a level of risk as tool for tourism sector. The green records indicate the number of colonies sighted in the period February–March (low-risk); yellow is the number of colonies sighted in the period April–May (medium-risk); red is the number of colonies sighted in the period June–August (high-risk). The map can be be used by local and regional managers to assess the risk of having free floating P. physalis colonies intheir area of interest.

A total of eight colonies were recorded in Sardinian waters, two belonging to the low-risk category, three to medium-risk and three to high-risk class (Figure 4). The Channel of Sicily showed the largest number of colonies sighted and stranded, thirty-two colonies of which ten were at low-risk, eighteen at medium-risk and four at high-risk. In the Tyrrhenian marine sector five colonies occurred, of which the only one at low-risk, two at medium-risk and two at high-risk. In this marine sector, the colonies of the Gulf of Naples and the Gulf of Palermo recorded in the museum collections were excluded because they were catalogued without a precise date. A total of six colonies were registered in the Strait of Messina, of which five were at low-risk and one at medium-risk.

Discussion

Physalia physalis is one of the most dangerous species of cnidarians that threaten public health. This is because the sting of this species is very painful and the venom present in nematocysts can cause health complications for people attacked. In some documented cases, these incidents have had fatal outcomes (Burke, 2002; Labadie et al., 2012). P. physalis can be harmful also in an indirect way, as prey of neustonic nudibranchs; in fact, some planktonic molluscs ingest the cnidarian and undischarged nematocysts as a defensive strategy (Thompson and Bennett, 1969). The nematocysts maintain toxicity in the predators (Thompson and Bennett, 1969; Ottuso, 2009). The same harmfulness has been detected in the stranded P. physalis individuals on a beach, even after several days of dehydration (Tibballs, 2006).

In the “Guidelines for safe recreational water environments” of the World Health Organization (WHO), P. physalis is included among the most dangerous aquatic organisms for human health, suggesting avoiding bathing in waters where Portuguese man-of-war is concentrated (World Health Organization [WHO], 2003). In order to develop policies for controlling and managing the well-being in recreational activities, a wide spatial and temporal scale of data is needed for an adequate assessment of the risk of contact with the Portuguese man-of-war within the Mediterranean Sea. Further, the launch of a series of activities based on scientific dissemination campaigns can allow the local authorities in charge to plan effective actions regarding the protection of public health and tourism (De Donno et al., 2014; Montgomery et al., 2016).

This is particularly relevant within the Mediterranean Sea where dispersal of some cnidarian species need major attention (Rossi et al., 2019) and where a great portion of the population still ignore the real hazard of most of the species, even though the high number of sightings and strandings recently detected through the media and social networks have helped to deepen the knowledge of the animal group.

Thus data were herein collected from different sources: social networks—scientific literature—museum zoological collections, as current and historical information on the distribution of the Portuguese man-of-war in the Mediterranean had not been organized yet and presented in a single article.

Under this operational framework, it was possible to track the putative first records of P. physalis in the Mediterranean Sea. The oldest documented capture of P. physalis occurred in Nice in 1850. Furthermore, it was possible to date further colonies of P. physalis, preserved in museums and captured in a wide area of the Western Mediterranean region in a period antecedent to 1980, even older than the record attributed as the first by Berdar and Cavallaro (1980) in the Strait of Messina.

The role of museums was fundamental for reconstructing the past distribution of P. physalis. A new scenario on its presence in the Mediterranean Sea has been depicted, up to now suspected by the scientific community (Boero, 2013). Indeed, based on these new data and those reported in the literature and here examined, it is very likely that P. physalis has always entered the Mediterranean Sea.

The occurrence of P. physalis in the Mediterranean had been considered rare till the last decades, due to the lack of documented records in the literature (Castriota et al., 2017). Only in recent years, an increase of P. physalis sightings in the central Mediterranean Sea was reported. The reasons are attributable to the advancement of technological innovations (smartphones), which make sightings validated with photographs or videos (not possible in the past) as the case of the Maltese fishermen who were not able to provide evidence of sightings (Calleja, 2009).

From 2001 to 2020, several P. physalis strandings have been documented in the Mediterranean Sea [Patrick J. Schembri pers. comm.; Deidun (2010), Focus (2010), Boero (2013), Mare Nostrum Italia (2013), Prieto et al. (2015); Castriota et al. (2017), Deidun et al. (2020); Mghili et al. (2020), Marambio et al. (2021), and MacĂ­as et al. (2021)] and lead us to assess the pathway of the colonies in the Mediterranean Sea. The route and the extent of flow depend on the particular climatic-oceanographic conditions which regulate the entry from the Atlantic Ocean toward the Mediterranean, as argued by Poulain et al. (2012).

The data showed massive strandings (thousands of colonies) recorded in the Alboran Sea (Prieto et al., 2015; Mghili et al., 2020; Macías et al., 2021), probably due to the action of the strong gyres in shallow water (Poulain et al., 2012), which behave like a physical barrier, as suggested by Prieto et al. (2015). The Atlantic water in the Alboran Sea describes two anticyclonic (clockwise rotating) gyres that dominate the surface flow pattern: a quasi-permanent anticyclonic gyre in the west (Western Alboran Gyre, WAG) and a more variable circuit in the east (Eastern Alboran Gyre, EAG) (Figure 1; Millot, 1999). In such a situation, the vein flowing from Spain to Algeria, named “the Almeria-Oran jet” (Millot, 1999), stops a large number of colonies, preventing their eastward dispersal, except some colonies that find a favourable oceanographic route and move toward the western and central Mediterranean.

As the circulation features of the Alboran sector is largely controlled by meteorological conditions (MacĂ­as et al., 2021), some concerns regard climate change which could alter the role of natural barrier in the future, allowing a greater entry of P. physalis from the Atlantic Ocean. Under such a hypothetical scenario of an increasing number of colonies of P. physalis, we should limit human activities eventually exposed to risks in the central Mediterranean.

The pattern described in the map of Figure 1 gives an idea of how the Portuguese man-of-war circulates in the Mediterranean. The records follow the surface currents and cover a limited geographical range maybe due to biological constraints, as it is probable that P. physalis dies during its “travel” in the Mediterranean Sea and new colonies enter through the Strait of Gibraltar the successive year. Based on this, at least for now, we cannot consider this species as an invasive or non-indigenous one.

The tracking of this species in the Mediterranean Sea should not be neglected, as the species threaten human health. For this reason, we selected some areas of risk by grouping the records of P. physalis in the most concerned four Italian maritime sectors: Sardinian waters; Channel of Sicily; Tyrrhenian Sea; Strait of Messina. The marine sectors most involved by P. physalis passage were identified and associated with levels of danger for swimmers according to the seasons of occurrence of the colonies (Figure 5). The highest number of colonies were recorded in the Channel of Sicily, probably also thanks to the active monitoring that has taken place in recent years. The area showed records belonging to the three categories of risk, low- medium- and high-risk category; it means that the species occurs from February to August. The Strait of Messina seems to be the area less involved by the passage of the Portuguese man-of-war. Concerning some records here reported, such as the specimen of the Gulf of Castellammare (Balestrate, southern Tyrrhenian Sea), the particular morphology of gulfs or bays with their currents regime could contribute to maintaining the colonies of P. physalis within the bay once has entered, with no or little chance to leaving the area. Hence the need for a better understanding and prediction through models of the currents and wind regime in these particular areas is auspicate.

The recent expansion of Citizen Science projects and the use of social media for the detection of “strange-looking species” or charismatic species may have certainly contributed to increasing the number of observations in nature, including Physalia physalis. In this regard, we observed, especially in the last decade, how Citizen Science is experiencing an upsurge of interest and was demonstrated to be particularly effective for data collection and maritime monitoring (Devictor et al., 2010; Dickinson et al., 2010). In the Mediterranean Sea, several Citizen Science projects are currently active and contribute to the early detection and monitoring of uncommon or non-indigenous species (Giovos et al., 2019; Tiralongo et al., 2019, 2020). These projects have often benefited from the involvement of the public through social media (Azzurro and Tiralongo, 2020; Al Mabruk et al., 2021). Citizen Science could be an efficient tool for information campaigns to introduce the Portuguese man-of-war to the public and better track the early detection of the species, as already done for other harmful organisms (Andaloro et al., 2016).

The results suggest that a national multidisciplinary summer surveillance program in the central Mediterranean Sea coast is required to provide alerts to the public, and hopefully to improve the quality of health care. Local authorities should set up a monitoring and alert system, with the participation of territorial organizations, and the contribution of the scientific community, as proposed in other seas (Labadie et al., 2012). In this regard, engaging tourists as citizen scientists can be a useful and low-cost method for the monitoring of this and other dangerous species in general and on a large spatial-temporal scale (Schaffer and Tham, 2019). Continuous monitoring could beneficial for marine tourist facilities.

In general, the data reported can be considered an important reference point for the development and calibration of predictive models on jellyfish abundance and distribution over a large timeframe. The importance of obtaining time-series data to monitor biodiversity changes in the Mediterranean Sea is crucial and acquire a relevant role in respect to the more frequent extreme events and temperature anomalies.

Publisher’s Note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.

Statements

Data availability statement

The raw data supporting the conclusions of this article will be made available by the authors, without undue reservation.

Author contributions

SL and FT conceived the project and contributed to final review and editing of the manuscript. LP provided some data. SL, LP, and RB analysed the data. SL, FT, and RB drafted the manuscript. SL, LP, FT, and VA reviewed the manuscript. All authors contributed to the article and approved the submitted version.

Funding

Open Access Funding provided by Università degli Studi di Palermo. This work was carried out within the framework of the Ph.D. project of RB funded by Università degli Studi di Palermo. This research was also supported by the Project Agreement “Sistema de Observación y Predicción de Medusas en el Mar Balear” among Govern des Illes Balears, SOCIB and CSIC (Disposición 15052, BOE núm. 310, 2020).

Acknowledgments

We thank Cecilia Volpi (Natural History Museum of the University of Florence, Florence, Italy), Gianni Insacco [Museo Civico di Storia Naturale, Comiso (RG), Italy], Claudia Gili and Andrea Travaglini (Darwin Dohrn Museum of the Anton Dohrn Zoological Station, Naples, Italy), Enrico Bellia (Museum of Zoology P. Doderlein of the University of Palermo, Palermo, Italy), Susanna Salvadori (Museum of Zoology, University of Cagliari), Maria Linda Tumbiolo and Paola Pepe for helping in catalouging the marine invertebrates collection of the Museum of Zoology P. Doderlein of the University of Palermo, and Silvano Riggio and Patrick J. Schembri for being very helpful in getting information about museum specimens. We thank the three reviewers for their helpful suggestions.

Conflict of interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

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Summary

Keywords

Physalia physalis, zoological collections, dangerous species, citizen science, tourism sector, Mediterranean biodiversity

Citation

Tiralongo F, Badalamenti R, Arizza V, Prieto L and Lo Brutto S (2022) The Portuguese Man-of-War Has Always Entered the Mediterranean Sea—Strandings, Sightings, and Museum Collections. Front. Mar. Sci. 9:856979. doi: 10.3389/fmars.2022.856979

Received

18 January 2022

Accepted

28 February 2022

Published

29 March 2022

Volume

9 - 2022

Edited by

Pierluigi Carbonara, COISPA Tecnologia & Ricerca, Italy

Reviewed by

Dimitris Poursanidis, Terrasolutions Marine Environment Research, Greece; Juan Jesús Bellido López, Aula del Mar Málaga, Spain; Joe El Rahi, Ghent University, Belgium

Updates

Copyright

*Correspondence: Sabrina Lo Brutto,

This article was submitted to Marine Biology, a section of the journal Frontiers in Marine Science

Disclaimer

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.

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