Showing posts with label Encrusting Organisms. Show all posts
Showing posts with label Encrusting Organisms. Show all posts

Friday, 7 August 2020

Lodgers on the tubes of Tube Anemones.

Benthic organisms are well adapted to the habitat conditions present in the locations where they live and estimates of abundance of these organisms are usually related to the habitat in which they are found. Moreover, some species require anchoring sites to settle and complete part of or their whole life cycles. Thus, the lack of consolidated structures on unconsolidated bottoms leads many benthic settlers to seek different suitable substrates, amongst which are artificial substrates such as ship hulls or offshore platforms, and natural substrates, such as marine invertebrate shells, Corals, and Ceriantharian (Tube Anemone) tubes. Ceriantharians (Cnidaria: Anthozoa) are tube-dwelling Animals that synthesize their tubes primarily with the use of ptychocysts, a type of cnida only found in this group, combined with small sediment fragments from the sea bottoms where the tube is built. The soft texture of ceriantharian tubes would initially appear not to be an attractive feature for the anchoring of invertebrate species that usually use rigid structures as anchoring locations. However, a few studies have reported on species able to settle on this microhabitat. In spite of it, the sampling of Ceriantharia is rather troublesome and rare, and tubes are usually overlooked and rarely collected along with polyps, contributing to lack of information about this subject.

In a paper published in the journal Biodiversity Data on 8 January 2020, Hellen Ceriello and Celine Lopes of the Instituto de Biociências at the Universidade Estadual Paulista, James Davis Reimer of the University of the Ryukyus, Torkild Bakken of the University Museum at the Norwegian University of Science and Technology, Marcelo Fukuda of the Museu de Zoologia da Universidade de São Paulo, Carlo Magenta Cunha of the Universidade Federal de São Paulo, and Sérgio Stampar, also of the Instituto de Biociências at the Universidade Estadual Paulista report on invertebrate communities inhabiting tubes of different Ceriantharian species from different locations, and discusses their main characteristics.

Ceriello et al. sampled 22 tubes of 10 species of Ceriantharia by SCUBA surveys in Argentina, Brazil, Japan, Norway, Portugal, and the United States. All material, except for Isarachnanthus nocturnus, and Ceriantheomorphe sp., was preserved along with their polyps and, before analyses, all polyps were removed from their tubes which were kept individually in labelled jars containing 70% ethanol.

The Tube Anemone, Isarachnanthus nocturnusSergio Stampar/National Science Foundation.

Each tube was analyzed separately under a stereomicroscope in a bowl with dark craft foam in the bottom and full of freshwater. All tubes were longitudinally cut with surgical carbon steel scalpels, opened, and fixed in the craft foam using acupuncture needles. Both inner and outer walls were analysed. The fauna found in or on the tubes was removed, photographed, and measured using a Zeiss AxioCam MRc5 and Zeiss AxioVision SE64 Rel 4.8 imaging software. Afterwards, the associated fauna was morphologically identified with specific taxonomic keys for each group.

A total of 58 species (8 crustaceans, 24 molluscs, 26 polychaetes) was observed in/on ceriantharian tubes. It is noteworthy that, although Crustaceans and Polychaetes in this study were alive at the time of sampling, they were not alive during tube analyzes. The results were separated by taxonomic group.

Thirghty eight Mollusc shell specimens, including Gastropoda and Bivalvia, were observed and were always found adhered to the outside of the tubes, and none had a periostracum coating, indicating that they were not alive at the time of collection.

Mollusca found on Ceriantharian tubes. (A) Schwartziella bryerea (B) Parvanachis obesa (C) Bittiolum varium (D) Cerithidea balteata (E) Chrysallida sp. (F) Liotella sp. (G) Emarginula sp. (H) Bostrycapulus odites (I) Collonista rubricincta (J) Eulima sp. (K) Microgaza rotella (L) Turbonilla sp. (M) Caecum regulare (N) Puncturella noachina (O) Basterotia elliptica (P) Ervilia nitens (Q) Macomopsis melo (R) Cumingia lamellosa (S) Musculus lateralis (T) Cardites micellus (U) Tivela sp. (V) Sphenia fragilis. Scale bars (A)-(N) 500 μm (O)–(U) 500 μm (V) 100 μm. Ceriello et al. (2020).

Ceriello et al.observed shells of Schwartziella bryerea and Turbonilla sp. adhered to the fragile tube of Arachnanthus sp., as well as amongst sediments that surrounded the tube. Shells of Cerithidea balteata, Eulima sp., Liotella sp., Emarginula sp., Chrysallida sp. and Collonista rubricincta, were found attached to the entire length of the thin and delicate tube of Isarachnanthus bandanensis. Bittiolum varium was found attached to the tubes of Isarachnanthus nocturnus. Puncturella noachins was, in part, adhered to the thin and fragile tube of Cerianthus lloydii.

On the tubes of Ceriantheomorphe brasiliensis, Ceriello et al. noted shells of Bittiolum varium, Finella dubia, Parvanachis obesa, Bostrycapulus odites, Caecum regulare, and Microgaza rotella. The tubes of Ceriantheomorphe brasiliensis usually have a high amount of overlap of filaments and, although this pattern was also observed in specimens in this study, no Mollusc shells were found between layers, and shells were only found on the outermost surfaces of the tubes.

Shells of Ervilia nitens, Chama sp., Cardites micellus, and Tivela sp. were observed adhered on the tube of Arachnanthus sp., while Ervilia nitens, Basterotia elliptica, and Musculus lateralis, were observed adhered on the tubes of Isarachnanthus nocturnus.

Shells of Sphenia fragilis, Ervilia nitens and Musculus lateralis were observed upon the tubes of Ceriantheomorphe brasiliensis, and shells of Macomopsis melo, were observed covering considerable areas of the tube of Ceriantheomorphe sp.

The only area on the tube of Ceriantheopsis americana where Ceriello et al. observed the presence of Mollusc shells, was on its slender end that was vertically inserted into the soft bottom. All specimens observed were Cumingia lamellosa, and these were found in high amounts and firmly attached to the tube.

Ceriello et al. observed 29 Peracaridans, belonging to 8 families, including 5 Amphipod species, 2 Isopod species and 1 Tanaidacean species on the tubes of three Ceriantharian species.

Crustacea and Polychaeta found in/on Ceriantharian tubes. (A) Monocorophium acherusicum (B) Idotea balthica (C) Cymadusa filosa (D) Paranthura urochroma (E) Photis sarae, female and male, respectively (F) Ampelisca burkei (G) Chondrochelia savignyi (H) Elasmopus pectenicrus (I) Nereis sp. (J) Phyllodocidae, indet. (K) Cirriformia sp. (L) Sternaspis sp. Scale bars: (A)-(H) 1000 μm (I) 2000 μm (J) 600 μm (K) 1000 μm (L) 3000 μm. Ceriello et al. (2020).

Most peracaridans were found in areas far from the Ceriantharian tentacles, thus not easily accessible to the Ceriantharian. No specimen was found inside the tubes or amongst tube layers. On the tubes of Ceriantheomorphe brasiliensis, Ceriello et al. observed the Amphipods Ampelisca burkei, Cymadusa filosa, Elasmopus pectenicrus, and Photis sarae, and the Isopod Paranthura urochroma firmly attached to the tube external wall; both Amphipods and Isopods were surrounded by ptychocyst filaments. Additionally, Ceriello et al. found Tanaidaceans of species Chondrochelia savignyi; however, those were free from ptychocyst filaments and were not firmly attached. Monocorophium acherusicum (Amphipoda) and Idotea balthica (Isopoda) were also found surrounded by ptychocyst filaments and attached to the external wall of the tube of Ceriantheopsis lineata. One specimen of Photis sarae was noted amongst Algae thalli covering the tube of Isarachnanthus nocturnus. It is noteworthy that the amphipod was not directly attached to the tube, but instead it was freely on its surface.

A total of 122 Polychaetes, including 17 families and 26 species, were found in or on tubes of six species of Ceriantharia. Some of the specimens were not possible to identify further than family or genus, as they were fragmented or in poor condition.

Ceriello et al. observed one specimen of Lysilla loveni (Terebellidae), two Cirratulids, two Paraonids and two Syllids in between layers of the tube of Botrucnidifer norvegicus. On the external wall of the tube of Ceriantheomorphe brasiliensis, Ceriello et al.found Cirratulids (Cirriformia spp.), Eunicids (Lysidice spp.), nereidids (Neanthes sp.), Syllids (Exogone spp., Myrianida sp. and Syllis prolifera), and Spionids (Aonides sp. and Dipolydora spp.), and one specimen each of Sabellidae (Branchiomma sp.), Flabelligeridae (Brada sp.), Magelonidae (Magelona sp.), Polynoidae (Malmgreniella sp.), Capitellidae (Mediomastus spp.), and Phyllodocidae. Only some specimens had ptychocyst filaments surrounding them and keeping them firmly attached to the tube. Ceriello et al. observed Dipolydora spp. amongst Algae thalli covering this tube, as well as in between folds of layers of the tube of Ceriantheomorphe brasiliensis from Guanabara Bay.

The heavy tubes of Ceriantheopsis lineata showed many perforations that were occupied by either deeply or superficially burrowed Polychaetes between some layers. Beneath layers, we observed some Spionids (Dipolydora spp.) and single specimens of Capitellid (Mediomastus spp.), Cirratulid (Cirriformia spp.), and Oenonid (Notocirrus spp.). The removal of layers also revealed empty boring holes under them. Moreover, Ceriello et al. found Syllis garciai (Syllidae) and one Phyllodocid on the tube surface, surrounded by ptychocyst filaments and mucus, respectively.

Some Parasabella sp., Lysidice spp., Cirriformia spp., and Spirobranchus sp. were found amongst algae thalli partially covering one of the tubes of Isarachnanthus nocturnus. However, they were not attached to the tube and neither had ptychocyst filaments surrounding them. Additionally, Ceriello et al. observed Notocirrus spp. on the surface of this tube.

Ceriello et al. observed one maldanid on the surface of the tube of Ceriantheomorphe sp., as well as large Nereis sp. partially burrowed, and small groups of Sternaspis sp. (3 specimens each group) both superficially anchored and deeply burrowed into tube layers.

Finally, Ceriello et al. found 36 Notocirrus spp. and two syllids on tubes of Pachycerianthus schlenzae, either burrowed between layers or attached to the surface of the tubes. In both cases, there were some specimens coated by their own mucus, but none was firmly attached to the tubes.

There have been some previous studies on the presence of marine invertebrates anchored on Ceriantharian tubes, with results suggesting that they are a suitable option as a consolidated structure for the settlement in unconsolidated bottoms. Ceriello et al.'s results not only corroborate the use of ceriantharian tubes as alternative substrates for other organisms, but also indicate a different anchoring method for species of the three phyla evaluated, Mollusca, Arthropoda (Crustacea) and Annelida (Polychaeta). Furthermore, they suggest possible benefits acquired by species on Ceriantharian tubes, discuss the use of mollusc shells in ceriantharian tube construction, and report new location records for six taxa.

Ceriello et al. did not observe whether Peracaridans and Polychaetes voluntarily settle on Ceriantharian tubes or are incorporated into the tubes by the Ceriantharians. In spite of this, their results show that most of these specimens were found in areas of the tubes where the tentacles of the Ceriantharian could not easily reach them. Thus, it is most likely that these species have actively recruited this alternative substrate than have been incorporated into it by the actions of the Ceriantharian. As Ceriello et al. could not evaluate this possibility, this hypothesis cannot be excluded.

Ptychocyst filaments are the most common material in Ceriantharian tubes. Notably, most Amphipods and Isopods firmly anchored to Ceriantharian tubes were surrounded by filaments (e.g. Ampelisca burkei, Cymadusa filosa, Idotea balthica, Monocorophium acherusicum, Paranthura urochroma, and Photis sarae), while some other specimens, such as Chondrochelia savignyi, were not. Likewise, some Polychaetes were observed surrounded by filaments (e.g. Syllis garciai) and thus firmly anchored, while others were coated by their own mucus (e.g. Phyllodocids and Notocirrus spp.) and only superficially anchored. It has been suggested that ptychocyst filaments have adhesive properties and our observations support this suggestion, as it is likely that the adhesive property of ptychocyst filaments is used by Peracaridans and Polychaetes as an anchoring method to settle on Ceriantharian tubes. Otherwise, specimens not surrounded by ptychocyst filaments must have alternative anchoring methods to keep them on tubes.

Crustaceans, Tubeworms and Ceriantharians often acquire shelter against predators in self-built-tubes which may be rigid, as in some Cirratulids, Sabellids and Serpulids. Ceriello et al. observed the Polychaetes Lysidice spp. anchored on Ceriantharian tubes. As members of this genus commonly excavate galleries or temporarily occupy empty galleries/tubes of other organisms, it is possible that Lysidice spp. use Ceriantharian tubes as alternative habitats.

Tube-dwelling Amphipods, Isopods, and Tanaidaceans usually burrow directly into the soft bottom, forming mucous tubes for habitation. For instance, the Amphipod Photis sarae was observed anchored on tubes of Isarachnanthus nocturnus and Ceriantheomorphe brasiliensis. However, this species is usually found in soft tubes built with mucus, small sediments and, sometimes, living organisms (e.g. Algae), similar to Ceriantharia. Ceriello et al. also observed other tube-dwelling Peracaridans coated by ptychocyst filaments and attached to the surface of Ceriantharian tubes, suggesting that, by using Ceriantharian tubes, Peracaridans can be sheltered, without the necessity of building their own tubes.

Mollusc shells were observed on all Ceriantharian tubes examined. However, the absence of periostracum coating these shells suggests that Ceriantharians do not shelter living Molluscs, but instead they adhere empty shells to their tubes, using them as a relevant component for the tube construction. The addition of Mollusc shells and other sediment remains as tube constituents may reinforce the tube, increasing its resistance and, thus, having an architectural role. Moreover, the external surfaces of all shells were usually very worn, indicating that they were part of the seafloor sediment rather than part of living assemblages. Although Ceriello et al.'s data do not allow them to assess how the shells were obtained during tube construction, future studies would be useful to provide such information (e.g. is there any special behavior associated with inclusion of Mollusc shells?) and to examine if it is possible that Ceriantharian tubes shelter living Molluscs.

It has been suggested that empty Mollusc shells enable the understanding of biodiversity patterns of Mollusca fauna at a specific site and can thus be used to provide data on ecological and evolutionary timescales. Accordingly, a similar role could be attributed to the accumulation of shells in Ceriantharian tubes, reflecting the species richness of living Molluscs in the surrounding habitat.

This is the first record of Microgaza rotella (Mollusca) and Brada sp. (Polychaeta) in Laje de Santos, and Photis sarae (Peracarida) in São Sebastião and Laje de Santos, São Paulo State, in southeastern Brazil. To date, Microgaza rotella had been reported as occurring from the southeastern United States to northern Brazil, and, since that there have been no other records in literature regarding this species in southeastern Brazil Microgaza rotella may occur naturally at this location (Laje de Santos) and may be rare or allochthonous (i.e. originated in a region other than where it was found) and transported by other species. Brada had been previously reported in Brazil only from Ubatuba City, while Photis sarae had only been previously reported in Rio de Janeiro State.

This is also the first record of Dipolydora in Rio de Janeiro State, and Notocirrus spp. and Syllis garciai in Espírito Santo State. Dipolydora had only been previously reported from Brazil in São Paulo, Paraná and Espírito Santo States. Notocirrus had been reported occurring in São Paulo, Rio de Janeiro, Paraná and Bahia States, while Syllis garciai had only been previously reported in São Paulo State.

It is noteworthy that Lysilla loveni (Polychaeta) was found on the tube of a Nordic Ceriantharia species, Botrucnidifer norvegicus. This Polychaete species has only rarely been found and usually as single occurrences scattered along the Norwegian coast.

Biogenic structures, such as Ceriantharian tubes, play a major role in altering community structure, thus affecting species richness and individual abundances. Tubes may affect the stability of the sea bottom and provide refugia from predation, as well as surfaces for the recruitment of benthic organisms. In fact, species abundance and richness have been observed to be greater around or on tubes than in areas without tubes. Ceriello et al. did not compare the fauna from Ceriantharian tubes to that from the surrounding sea bottoms however, their results demonstrate that Ceriantharian tubes appear to be suitable alternative substrates for numerous species, especially tubicolous and infaunal invertebrates that usually spend much energy burrowing into sediments or anchoring on fixed or mobile habitats while seeking shelter. Moreover, other than shelter, residents on and in Ceriantharian tubes may also acquire protection. Therefore, the tubes of Ceriantharia may play an important role as small-scale biodiversity hotspots.

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Sunday, 17 December 2017

Terpios hoshinota: Tracking the progress of the Black Death Sponge on Okinoerabu-jima Island.

Sponges, Porifera, form an important part of many benthic marine communities, both for their contribution to the structure of reefs and their forming of symbiotic relationships with a variety of other organisms, including Prokaryotes, Shrimp, Worms, Hydroids, Zoantharians, and Fish. However not all Sponges are beneficial to the communities that host them. The Heteroscleromorph Demosponge Terpios hoshinota forms symbiotic relationships with a variety of Cyanobacteria, spreading rapidly by photosynthetic growth. This enables it to grow at a rate of several milometers per day, forming a thin black or grey crust that rapidly overgrows and kills Hard Corals such as Lobophylia, Montipora, Acropora, Merulina, and Goniastrea

The first known outbreak of Terpios hoshinota was recorded on Guam in 1973, since when it has spread to the Northern Mariana Islands, Western Caroline Islands, the Philippines, American Samoa, southern Taiwan, the Great Barrier Reef, Sulawesi, Java, the Maldives, Mauritius and the Ryukyu Islands. The first outbreak of the Sponge in the Ryukyu Islands hit the island of Tokunoshima in 1985-86, where it rapidly spread across the reefs of the Yonama Coast, eventually covering 87.9% of the reefs, and gaining the name 'Black Death Sponge'. 

 A colonoy of Terpios hoshinota overgrowing a Coral on Guam. Florida Museum.

The Sponge was detected on the reefs of Okinoerabu-jima Island, about 50 km to the southwest of Tokunoshima in 2010, raising concerns about the fate of the reefs there, however a survey carried out at this time found that Terpios hoshinota had completely disappeared from Tokunoshima, where reefs were now dominated by Hard Corals of the genus Acropora, suggesting that the appearance of the Sponge does not necessarily represent the end of a Coral Reef community.

In a paper published in the journal Zoological Studies on 19 April 2017, Masashi Yomogida, Masaru Mizuyama, and Toshiki Kubomura of the Molecular Invertebrate Systematics and Ecology Laboratory at the University of the Ryukyus, and James Davis Reimer, also of the Molecular Invertebrate Systematics and Ecology Laboratory, and of the Tropical Biosphere Research Center at the University of the Ryukyus, describe the results of a long-term study of the Terpios hoshinota outbreak on Okinoerabu-jima Island, based upon a series of surveys carried out between March 2010 and September 2014.

Yomogida et al. carried out a series of transect studies on the Yakomo Coast of Okinoerabu-jima Island, with each survey examing the surface covering of an area of reef measuring 10 m by 1 m. Each survey divided the covering of the reef into nine categories: (1) Terpios hoshinota, (2) Macroalgae (Seaweed) except the Sponge Weed Ceratodictyon spongiosum, (3) the Sponge Weed Ceratodictyon spongiosum, (4) Cyanobacterial mats, (5) living reef-building Corals, (6) dead Coral, (7) other benthic organisms, including Soft Corals, Giant Clams, Sea Cucumbers, and Sea Urchins, (8) sand and gravel, and (9) anything that could not be identified.

(A) Location of Okinaerabu-jima Island, Kagoshima, Japan in the northwestern Pacific and, (B) map of Yakomo coast on Okinoerabu-jima Island. Red dotted box shows the Terpios hoshinota survey area, white dotted lines show the approximate area of Terpios hoshinota along the coast, and red solid lines approximate locations of permanent transects. Google Earth/Yomogida et al. (2017).

Terpios hoshinota covered over 24% of the reef at the outset of the study (March 2010), and remained this high until October of that year, but fell to 17.6% coverage in December 2010. In June 2011 the species underwent a catastrophic die-back, falling to a covering of only 0.02% of the reef. Sponge levels remained low for the next year, having reached only 0.3% coverage by May 2012, but did eventually begin to recover, reaching 11.4% coverage by September 2014.

Coverage of the reef by Macroalgae remained below 10% in all surveys except one, in May 2012, when it reached 13.6%. Cyanobacteria were completely absent from the reef in all surveys except one, in October 2011, when it covered 39.9% of the reef. Sand and gravel remained the dominant coverings of the reef throughout the survey, with coverage varying between 50.2% and 89.4%; none of the other categories ever climbed above a 5% coverage on the reef.

Clearly some event significantly reduced the coverage of Terpios hoshinota in 2011, and came close to removing the Sponge from the reef altogether. Yomogida et al. suggest that the most likely culprit was Typhoon Songda, which passed close to the island on 28 May 2011, and which is recorded as having generated windspeeds of up to 139 kilometres per hour, and wave heights of up to 10.22 m. This event could have removed the Sponge encrustation either by directly tearing it from the reef or covering it in sand or other soft sediments.

This suggests that typhoons could play a major role in inhibiting the ability of Terpios hoshinota to dominate ecosystems, and are likely to have been the cause of the disappearance of the Sponge from Tokunoshima Island. However Yomogida et al. also note that tropical storms may also play a role in the dispersal of Terpios hoshinota, as the larvae of Cyanobacteria-hosting Sponges tend to have rather limited dispersal capacities, suggesting that something else has aided the apparent rapid dispersal of this species. They also note that Terpios hoshinota is now found in both tropical and subtropical seas, and that tropical storms are a feature of only subtropical seas, with areas such as Indonesia and the Maldives, where the Sponge has become established, not effected by these storms.

Yomogida et al. also note that an outbreak of Terpios hoshinota on Pagan Island in the Mariana group was strongly linked to a volcanic eruption on that island, with a large patch of the Sponge appearing with the onset of volcanic activity in 2010, and disappearing when volcanic activity stopped in 2012. They suggest that this might be connected to the deposition of volcanic ash into the waters around Pagan Island, which would have increased the levels of nutrients, particularly iron, to the Sponge and its symbiotic Cyanobacteria. This raised the possibility that Human activities may be facilitating the spread of Terpios hoshinota, if these activities result in extra nutrients being released into the water.

See also...

http://sciencythoughts.blogspot.co.uk/2017/10/plenaster-craigi-new-species-of.htmlhttp://sciencythoughts.blogspot.co.uk/2015/03/preservation-of-cellular-structures-in.html
http://sciencythoughts.blogspot.co.uk/2014/12/two-new-species-of-homoscleromorph.htmlhttp://sciencythoughts.blogspot.co.uk/2014/12/a-new-species-of-sponge-from-late.html
http://sciencythoughts.blogspot.co.uk/2014/12/thirteen-new-species-of-deepwater.htmlhttp://sciencythoughts.blogspot.co.uk/2014/11/calcifying-endosymbiotic-bacteria-in.html
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Saturday, 3 September 2016

Palaeoconchus wilsoni: A new species of Microconchid from the Silurian of Estonia and Gotland.

Microconchids are a groups of poorly understood encrusting organisms known from the Ordivician to the Jurassic. They formed tubular encrustations on hard substrates in a similar way to modern Serpulid Worms, and were for a long tme were thought to be early members of that group, but the tubes have since been recognised as being structurally different to those made by Serpulids, leaving the identity of the tube-mekers enigmatic.

In a paper published in the Estonian Journal of Earth Sciences on 20 June 2016, Michał Zatoń of the Faculty of Earth Sciences at the University of Silesia, Olev Vinn of the Department of Geology at the University of Tartu and Ursula Toom of the Institute of Geology at the Tallinn University of Technology describe a new species of Microconchid from the Silurian of Estonia and Gotland.

The new species is placed in the genus Palaeoconchus, and given the specific name wilsoni, in honour of Mark Wilson of the College of Wooster in Ohio, for his work on the biotas of hard substrates, including Microconchids. It is described from six specimens; five from the Kuressaare Formation of Saaremaa Island, Estonia, where they were found growing on Rugose Corals, and one from Gotland in Sweden, where it was encrusting a Brachiopod Shell. A number of other specimens were collected on Saaremaa Island, but no others found in Sweden.

Palaeoconchus wilsoni, from Saaremaa Island, Estonia (A–E) and Gotland, Sweden (F). Scale bars 500 μm. Zatoń et al. (2016).

The specimens are flattened and dextrally coiled (coiling to the right when seen from above, clockwise) and ornamented with thicj transverse ribs. The largest specimens reach 2.7 mm.

Encrusted Rugose Corals from Saaremaa Island, Estonia. (A) Auloporids (white arrow), Cornulitid Conchicolites (black arrow) and two associated Microconchids. (B) Anticalyptraea (white arrows) and Trepostome Bryozoan colony (black arrow). (C) Ascodictyids (black arrows) and associated Microconchids. (D) Cornulitid Conchicolites (black arrows). (E) Rugose spatfalls within the calyx (black arrow) and a Hederelloid colony (white arrow). Zatoń et al. (2016).

See also...

http://sciencythoughts.blogspot.co.uk/2016/05/dyrnwynia-conollyi-new-species-of.htmlDyrnwynia conollyi: A new species of Marrellomorph Arthropod from the Middle Ordovician of Pembrokeshire, Wales.         The Marrellomorphs are a poorly understood group of early Arthropods known from Palaeozoic deposits at a number of sites around the world. They are not thought to have had any mineralized parts, making them rare in the fossil record, and to date only three species...
http://sciencythoughts.blogspot.co.uk/2016/01/possible-annelid-worm-tubes-from-early.htmlPossible Annelid Worm tubes from the Early Devonian of Brazil.                                   Worm tubes first appear in the fossil record in the Ediacaran and become increasingly common through the Palaeozoic. Most Worm tubes today are made by Polychaete Annelids, a group which have existed...
http://sciencythoughts.blogspot.co.uk/2015/12/iocrinus-africanus-new-species-of.html Iocrinus africanus: A new species of Crinoid from the Middle Ordovician of Morocco.   The Ordovician was a period of rapid diversification and geographic expansion in many Echinoderm groups, including Crinoids. However their fossil record is not good in every area, making understanding this period in their evolutionary history difficult. The northern Gondwanan continental shelf was an important area...
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Friday, 21 December 2012

An invasive Serpulid Worm in the La Encrucijada Biosphere Reserve, Mexico.

The Serpulid Worm Ficopomatus uschakovi was first described from Sri Lanka in 1960. Like all Serpulid Worms is an encrusting, sessile Polychaete that secretes a tube of calcite (calcium carbonate) in which it dwells. Unlike most other Serpulids Ficopomatus uschakovi inhabits brackish waters in estuaries and lagoons rather than fully saline waters. It can form large, reef-like masses and rapidly dominates ecosystems where it is present, outcompeting other invertebrates such as Barnacles, Oysters and Mussels.

In the 1970s the species was found to be living along the West Coast of Africa, where colonies were reported to have first appeared in the 1950s. Since this time the species has been found in the Philippines, Indonesia, Australia, Brazil and Venezuela. Because of its ability to modify ecosystems it is considered to be an invasive pest, associated with contamination by introduced with Shrimp farms; many invasive marine organisms are associated with ballast water and hull fouling of shipping, but since Ficopomatus uschakovi is not thought able to colonize fully marine waters this seems improbable for this species.

In a paper published in the journal ZooKeys on 5 November 2012, Rolando Bastida-Zavala and Socorro García-Madrigal of the Laboratorio de Sistemática de Invertebrados Marinos at the Universidad del Mar describe the discovery of colonies of Ficopomatus uschakovi in coastal lagoons in  La Encrucijada Biosphere Reserve in Chiapas State, on the south coast of Mexico.

Ficopomatus uschakovi from La Encrucijada Biosphere Reserve. (A) tubes
on mangrove roots. (B) Tubes on the shell of the gastropod Thaisella kiosquiformis. (C) Mangroves in the collecting site. (D) Tubes forming small aggregations. (E) Large, single tube. (F) Complete specimen in dorsal view. (G) Complete specimen with mass of sperm attached to the abdomen. (H) Operculum in dorsal view. (I) Operculum in aboral view. Bastida-Zavala & García-Madrigal (2012).

There are no Shrimp farms in La Encrucijada Biosphere Reserve, and the nearest port is at Puerto Chiapas, 70 km to the south. It is therefore unclear how the Worms reached the lagoons, suggesting that they have a means of dispersal that scientists are unaware of. At the moment the infestation appears limited in scope, with no reef-like structures observed. How the Worms will affect the reserve in the future remains unclear; Bastida-Zavala and García-Madrigal recommend that the situation should be monitored carefully.

(A) World-wide distribution of Ficopomatus uschakovi; circles represent previously described colonies, the triangle the new colonies described in this study. (B) Study area and the localities where specimens of Ficopomatus uschakovi were recollected. 1: Zacapulco; 2: Barra San Juan; 3: Las Garzas boat pier. Bastida-Zavala & García-Madrigal (2012).


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