ON THE PROTONEPHRIDIA AND 'LARVAL KIDNEYS' OF NASSARIUS (HINIA) RETICULATUS (LINNAEUS) (CAENOGASTROPODA)

Protonephridia in marine streptoneuran gastropods are describedfor the first time. The organization of these paired organsof the intracapsular veliger larva of Nassarius reticulatusis described. The ciliary flame is formed by a single terminalcell. The duct is formed by one tubular cell and the aperturalcell, which forms the lips of the excretory pore. In addition,the surface of the apertural cell is covered to a great extentby the post-velar bud cell (usually termed ‘larval kidney’).Protonephridia like these are considered to be widely distributedamong streptoneuran gastropods. The homology of these organswith those of opis-thobranchs and pulmonates is suggested. Thepost-velar buds (= ‘larval kidneys’) are suggestedas a synapomorphous character of Caenogastropoda. The functionof the postvelar buds is discussed taking into considerationthe existence of a protonephridium and a possible functionalconnection between these two structures. (Received 14 June 1990; accepted 1 September 1990)     

HOMOLOGY OF THE PALLIAL AND PULMONARY CAVITY OF GASTROPODS

The development and morphology of the pallial and pulmonarycavities of various gastropods has been investigated using epoxy-resinserial sections. In the veliger larvae of Cellana sandwicensis(Patellogastro-poda), Gibbula adansonii (Vetigastropoda), Modulustectum (Caenogastropoda) and Ovatella myosotis (Pulmonata) theformation of the pallial cavity is nearly identical. After shellformation a shallow dorsal pallial groove develops beneath themantle edge. During the late veliger stage, the ectoderm formsa deep invagination along the bottom of the pallial groove onthe right side of the larva, giving rise to the pallial cavity.In the ellobiid O. myosotis the pallial cavity becomes the lung(=pulmonary cavity), without any major post-metamorphic modification.Thus, the lung of this species is clearly homologous with thepallial cavity of prosobranchs. The lung of pulmonates withveliger development, as well as of fresh water basommatophoransand stylommatophorans, can be shown to be homologous by comparisonof adult morphology. In contrast to previous views, the pulmonatelung should be regarded as truly homologous with the pallialcavity of prosobranchs and opisthobranchs. In the onchidiidpulmonate Onchidium cf. branchiferum, the larval pallial cavityshifts posteriorly after metamorphosis, where it gives riseto a lung and a cloaca. Contrary to previous interpretations,it can be shown that the onchidiid lung is homologous with atleast part of the pallial cavity. Smeagol climoi has only asmall pallial cavity and no separate lung. The previously described‘lung’ is shown to be a gland. The re-evaluationof the development and morphology of the pulmonate lung hasimportant systematic implications: (1) The pulmonary cavitydoes not represent a synapomorphic character of pulmonates.(2) The gymnomorphs cannot be separated from the remaining pulmonatesbased on lung development. (3) The lack of a lung in the smeagolidsmight give reason to reconsider this group's systematic placementwithin the pulmonates.     

Macroevolution in progress: competition between semislugs and slugs resulting in ecological displacement and ecological release

The vitrinids, which represent a probably competitively inferior transitional stage between shelled snails and slugs, and their sister group, the limacoid slugs, are used to investigate a macroevolutionary effect of a microevolutionary process, competition between individuals resulting in ecological displacement of one clade by another, based on patterns in the present-day world. The activity period and the altitudinal distribution of the vitrinids has shifted - to the cold season or to higher altitudes, respectively - in those regions where their range overlaps with that of the limacoid slugs. The diversity of the vitrinids is lower in regions with limacoid slugs. These patterns can be ascribed to the ecological displacement or the exclusion of the vitrinids from some habitats by limacoid slugs. Two vitrinid clades which independently colonized regions without limacoid slugs show patterns attributable to ecological release. The ecological displacement or exclusion of the vitrinids by the slugs is probably due to competition for shelter.     

Distribution and genetic divergence of two parapatric sibling ant species in Central Europe

The two sibling ant species Temnothorax nylanderi and Temnothorax crassispinus are widely distributed throughout deciduous forests in Europe. Their resemblance in morphology and similar ecological requirements suggest that they evolved from the same ancestral species in different glacial refugia and re-immigrated into Central Europe after the last ice age. Here, we show that the two species are parapatrically distributed in south-eastern Germany and hybridize along a narrow contact zone close to the continental divide. Phylogeographical data based on the mitochondrial genes cytochrome oxidase subunit I and cytochrome b suggest that the dominant haplotypes for T. nylanderi and T. crassispinus might have diverged already 1.5–2 Mya. Intraspecific variability is extremely low in both species, which might be explained by severe bottlenecks during rapid postglacial expansion into Central Europe.  © 2006 The Linnean Society of London, Biological Journal of the Linnean Society , 2006, 88 , 223–234.     

Impact of intentionally injected carbon dioxide hydrate on deep-sea benthic foraminiferal survival

Sequestration of carbon dioxide (CO₂) in the ocean is being considered as a feasible mechanism to mitigate the alarming rate in its atmospheric rise. Little is known, however, about how the resulting hypercapnia and ocean acidification may affect marine fauna. In an effort to understand better the protistan reaction to such an environmental perturbation, the survivorship of benthic foraminifera, which is a prevalent group of protists, was studied in response to deep-sea CO₂ release. The survival response of calcareous, agglutinated, and thecate foraminifera was determined in two experiments at ∼3.1 and 3.3 km water depth in Monterey Bay (California, USA). Approximately 5 weeks after initial seafloor CO₂ release, in situ incubations of the live–dead indicator CellTracker Green were executed within seafloor-emplaced pushcores. Experimental treatments included direct exposure to CO₂ hydrate, two levels of lesser exposure adjacent to CO₂ hydrate, and controls, which were far removed from the CO₂ hydrate release. Results indicate that survivorship rates of agglutinated and thecate foraminifera were not significantly impacted by direct exposure but the survivorship of calcareous foraminifera was significantly lower in direct exposure treatments compared with controls. Observations suggest that, if large scale CO₂ sequestration is enacted on the deep-sea floor, survival of two major groups of this prevalent protistan taxon will likely not be severely impacted, while calcareous foraminifera will face considerable challenges to maintain their benthic populations in areas directly exposed to CO₂ hydrate.