Reproductive Biology of Amblema neislerii, Elliptoideus sloatianus, Lampsilis subangulata, Medionidus penicillatus, and Pleurobema pyriforme (Bivalvia: Unionidae): final report

A study on the reproductive biology of Amblema neislerii, Elliptoideus sloatianus, Lampsilis subangulata, Medionidus penicillatus, and Pleurobema pyriforme was conducted from May 1995 to May 1997. The objectives of this study were as follows: 1) determine period of gravidity for each of the five mussel species, 2) determine host fish via laboratory experiments, 3) test whether unionid glochidia will transform on a nonidingenous fish, and 4) describe the glochidial morphology for each of the five mussel species using a scanning electron microscope. Amblema neislerii are tachytictic breeders and were found with mature glochidia in May. Elliptoideus sloatianus are tachytictic breeders and were found with mature glochidia from late February to early April. Lampsilis subangulata are bradytictic breeders and were found with mature glochidia from December to August. Superconglutinates were released by L. subangulata from late May to early July. Medionidus penicillatus are bradytictic breeders and were found with mature glochidia in November and February to April. Pleurobema pyriforme are tachytictic breeders and were found with mature glochidia from March to July. The following fish species served as hosts for A. neislerii: Notropis texanus, Lepomis macrochirus, L. microlophus, Micropterus salmoides, and Percina nigrofasciata. The following fish species served as hosts for E. sloatianus: Gambusia holbrooki, Poecilia reticulata, and P. nigrofasciata. The following fish species served as hosts for L. subangulata: G. holbrooki, P. reticulata, L. macrochirus, Micropterus punctulatus, and M. salmoides. The following fish species served as hosts for M. penicillatus: G. holbrooki, P. reticulata, Etheostoma edwini, and P. nigrofasciata. The following fish species served as hosts for P. pyriforme: Pteronotropis hypselopterus, G. holbrooki, and P. reticulata. Poecilia reticulata, a nonindigenous fish, served as a host for E. sloatianus, L. subangulata, M. penicillatus, and P. pyriforme. (76 page document)

Dinâmica populacional e caracterização conquiliomorfológica de Diplodon ellipticus Spix in Wagner, 1827 (Bivalvia: Unionoida: Hyriidae) da lagoa dos Caiçaras (Piraí, Rio de Janeiro, Brasil)

No presente estudo monitoramos uma população de Diplodon ellipticus Spix in Wagner, 1827 da lagoa dos Caiçaras, Piraí, Rio de Janeiro, e avaliamos alguns aspectos conquiliomorfológicos da larva e do adulto, a relação peso-comprimento, os padrões populacionais tais como crescimento, mortalidade e expectativa de vida, e o ciclo larval. Amostragens mensais foram realizadas de novembro/2012 a novembro/2013 em três pontos da lagoa. Em cada ponto, definimos uma area de 15 m2, que foi subdividida em 15 quadrados de 1m2 cada. Os bivalves foram procurados por três coletores, usando mãos e pés, totalizando 45 minutos de coleta/área. Posteriormente, foram medidos com um paquímetro em relação ao comprimento total, marcados e devolvidos a lagoa. Quinze bivalves foram coletados e analisados em laboratório durante dois anos. Os fatores abióticos (condutividade, temperatura da água, temperatura do ambiente, umidade, pH e oxigênio dissolvido) foram mensurados e amostragens do sedimento e da água foram realizados em cada ponto. Os indivíduos foram agrupados em classes de comprimento com intervalo de 2,0 mm para análise da estrutura de comprimento da população. Os parâmetros de curva de crescimento foram estimados pela rotina ELEFAN (distribuição de frequência) e pelo método de Gulland-Holt (marcação e recaptura), ambos no programa FISAT. A mortalidade foi calculada pelo método da curva de captura convertida em comprimento e a expectativa de vida foi calculada pela equação invertida de von Bertalanffy. Ao todo, 3474 bivalves foram marcados e 1849 recapturados, alguns deles mais de uma vez. O menor bivalve recapturado mediu 23,58 mm e foi recapturado 127 dias depois com 25,50 mm e o maior bivalve recapturado mediu 62,14 mm e foi recapturado 31 dias depois com 62,20 mm. Pelo método indireto analizamos 6922 bivalves com comprimentos variando de 11,37 a 62,49 mm. A maior frequência de comprimento foi encontrada em tamanhos intermediários de 44-46 mm, como foi observado em outras populações de Diplodon. A análise do crescimento, mortalidade e expectativa de vida foram similares em ambos os métodos, por isso, utilizamos em conjunto para ajustar a curva de crescimento da população. A relação peso-comprimento foi alta (r = 0,7-0,8). A avaliação do ciclo reprodutivo indica uma continuidade no desenvolvimento larval ao longo dos meses, à exceção de janeiro/2014. Contabilizamos um total de 54.617 gloquídios, havendo mais indivíduos grávidos com gloquídios (n=5) nos meses de julho e setembro de 2014. Padrão similar foi encontrado em outras espécies de bivalves de água doce, inclusive em Diplodon ellipticus no estado do Paraná. Os gloquídios maduros foram encontrados em amplitudes de temperaturas de 20,1-25,27C e acreditamos que a temperatura pode influenciar na liberação dos mesmos. Os bivalves com o maior e o menor número de gloquídios foram encontrados em novembro/2013 (n= 4759) e setembro/2014 (n= 212), respectivamente. A correlação entre o comprimento do marsúpio e o tamanho da ninhada foi testada pela primeira vez nesse gênero e foi significativa (r= 0,303 , p<0,05). As informações deste estudo são relevantes ao conhecimento da espécie e às futuras ações de gestão que tenham como objetivo preservar as espécies de Diplodon

The costs and benefits in an unusual symbiosis: experimental evidence that bitterling fish (Rhodeus sericeus) are parasites of unionid mussels in Europe

Interspecific symbiotic relationships involve a complex network of interactions, and understanding their outcome requires quantification of the costs and benefits to both partners. We experimentally investigated the costs and benefits in the relationship between European bitterling fish (Rhodeus sericeus) and freshwater mussels that are used by R. sericeus for oviposition. This relationship has hitherto been thought mutualistic, on the premise that R. sericeus use mussels as foster parents of their embryos while mussels use R. sericeus as hosts for their larvae. We demonstrate that R. sericeus is a parasite of European mussels, because it (i) avoids the cost of infection by mussel larvae and (ii) imposes a direct cost on mussels. Our experiments also indicate a potential coevolutionary arms race between bitterling fishes and their mussel hosts; the outcome of this relationship may differ between Asia, the centre of distribution of bitterling fishes, and Europe where they have recently invaded.

Conservation status and reproduction of the critically endangered freshwater pearl mussel (Margaritifera margaritifera).

1. Freshwater unionoids are one of the most threatened animal groups worldwide and the freshwater pearl mussel Margaritifera margaritifera is currently listed as critically endangered in Europe. The ‘EC Habitats & Species Directive’ requires that EU member states monitor the distribution and abundance of this species and report regularly on its conservation status.
2. The pearl mussel meta-population in Northern Ireland was surveyed to assess temporal population trends in Special Areas of Conservation (SACs) and mussel reproduction throughout its range.
3. Mussels occurred in six rivers and numbers within three SAC designated sites remained stable between 2004-07 and 2011. The discovery of >8,000 previously unknown individuals in the Owenreagh River contributed to an overall increase (+56.8%) in the total known population. All populations actively reproduced during 2010 with approximately half of all individuals gravid. Moreover, suitable salmonid hosts occurred at all sites with 10.7% of salmon and 22.8% of trout carrying encysted glochidia. Populations were composed entirely of aged individuals with little evidence of recent recruitment.
4. We infer that the break in the life cycle must occur during the juvenile stage when glochidia metamorphose and settle into the interstitial spaces within the substrate. Water quality parameters, most notably levels of suspended solids, exceeded the recommended maximum thresholds in all rivers.
5. We posit that the deposition of silt may be the main cause of juvenile mortality contributing to a lack of recruitment. Consequently, all populations were judged to be in ‘unfavourable’ conservation status. Catchment-level management plans are urgently needed to reduce siltation with the aim of improving recruitment. Our results have implications for the success of ex-situ conservation programmes; specifically, the size at which captive bred juveniles are released into the wild. Further research is required to assess the vulnerabilities of early life stages of M. margaritifera to siltation.

Pollen and macroremains from three sediment cores from Göttingen, Germany

In a borehole in the southern outskirts of the town of Göttingen, limnic sediments of several Pleistocene warm periods occur intercalated with coarse solifluction debris and gravel of the river Leine. Pollen analysis of the limnic sediments in a borehole at Ottostrasse gave evidence of three warm periods of interglacial character, followed by three interstadial phases. The warm phases are separated one from another by stadial phases with, at least in one case, indications of periglacial solifluction. This sequence belongs to the Brunhes magnetic epoch. The pollen data allow to exclude an Eemian or Holsteinian age of the warm period sediments. Thus a Cromerian age is assumed, though the exact position of the newly described warm periods within the ''Cromerian'' remains uncertain. A section in a borehole at Akazienweg is of Holsteinian age.

Pollen and macroremains from profiles from site Osterholz and Elm

The biostratigraphic classification of the Pleistocene in north-western and central Europe is still insufficiently known, in spite of numerous geological and vegetation-history investigations. The question is not even clear, for example, how often a warm-period vegetation with thermophilous trees such as Quercus, Ulmus, Tilia, Carpinus etc could develop here. In past years, on the basis of several geological and vegetation-history findings, suspicion has often been expressed that some of the classical stages of the Pleistocene could include more warm periods than heretofore assumed, and as a result of recent investigations the period between the Waal and Holstein interglacials seems to include at least two warm periods, of which the Cromer is one. This paper contributes to this problem. The interglacial sediments coming from the Elm-Mountains near Brunswick and from the Osterholz near Elze - both within the limits of the German Mittelgebirge - were investigated by pollen analysis. In both cases a Pinus-Betula zone and a QM zone were found. The vegetation development of the Pinus-Betula zone is characterized in both sequences by the early appearance of Picea. Because of strong local influence at the Osterholz a detailed correlation is difficult. However, vegetation development at the time of the QM zone at both sites was similar; it is especially characterized by the facts that Ulmus clearly migrated to the site earlier than Quercus and was very abundant throughout this time. Furthermore, both diagrams show very low amounts of Corylus. The interglacial of the Osterholz shows in addition to the above; a Carpinus-QM-Picea-zone in which Eucommia reaches a relative high value and in the upper of which Azolla filiculoides was also found. The similarity of vegetation development justifies acceptance of the same age for the occurrences. A comparison of the vegetation development at the Elm and the Osterholz with those of the Eem, Holstein, Waal, and Tegelen warm periods as well as with all the Cromer sites so far investigated shows that only a correlation with the Cromer Complex is possible. This correlation is supported by the geologic relations in the Osterholz (the deposit is overlain by Elster till). Therefore the till-like material with Scandinavian rock fragments underlying the deposit at Elm is of particular interest. The 'Rhume' interglacial beds at Bilshausen, only 60 km south of Osterholz, is also assigned to the Cromer complex, but the two deposits cannot be of the same age because the vegetation development differs. Therefore the Cromer complex must include at least two warm periods. Further conclusions about the relative stratigraphic position of these two occurrences and correlations of other Cromer sites are at this time not possible, however.