Observations on the morphology and behaviour of Chilina fluctuosa Gray (Chilinidae), with a discussion on the early evolution of pulmonate gastropods

An account is provided of (i) the general morphology, (ii) the vascular, nervous and feeding systems, and (iii) aspects of the behaviour of a representative species of the pulmonate genus Chilina . Examination of this genus has aided in understanding the pattern of early evolution of freshwater pulmonates from their marine prosobranch ancestors and of their divergence from opisthobranchs. The gross morphology of Chilina is adapted to ploughing through the surface layers of soft substrata. Although C. fluctuosa was found on rocks, it was nevertheless capable of burrowing into sand, using a stereotyped digging cycle. Streamlining to facilitate burrowing was achieved by nuchal shortening and by a ‘detorsion’ of the mantle complex as in opisthobranchs. The nuchal shortening incurred loss of a major vascular pathway which, in monotocardian prosobranchs, drains the head-foot. ‘Detorsion’, however, provided a substitute which incorporates the anterior roof of the mantle cavity where, in Chilina , the precursor of the rich pulmonary plexus characteristic of later pulmonates may be discerned. The suprapallalial vascular system is described in detail. In contrast, it is apparent that increased reliance on burrowing in opisthobranchs brought about loss of the anterior region of the mantle cavity, and thus any potential for development of a plexus in that region. Enclosure of the mantle cavity, which clearly pre-adapted the mantle complex to function also as a ‘lung’, was necessary to reduce clogging of the mantle cavity by particulate material. Only water is held in the cavity of Chilina flutuosa , whose habitat is rivers, but both air and water may be held in the mantle complex of other species found in Chile. The nervous system is extremely similar to that of the primitive opisthrobranch Acteon , but the posterior section of the visceral loop is shorter owing to greater nuchal reduction. The loop is uncrossed, though the supraoesophageal ganglion lies only a little right of the suboesophageal ganglion. The musculature of the buccal mass is extremely similar to that of Lymnaea and Planorbarius , and is designed for moving and tensing a broad radular ribbon. It is argued that the buccal morphology characteristic of these snails evolved to manipulate quantities of particulate material during the early infaunal phase, and only later was used to great effect in both microphagous and macrophagous feeding. Collectively, the observations made on C. flluctuosa (and also on estuarine species found in Chile) support the contention that the Basommatophora invaded freshwater habitats via estuarine niches. Continuity during this progression was apparently provided by soft substrata, and probably by diatoms as a food source. Previous arguments purporting a terrestrial or semi-terrestrial origin for the limnic basommatophorans are refuted.

2004 ◽  
Vol 78 (6) ◽  
pp. 1214-1216 ◽  
Author(s):  
Michael G. Bassett ◽  
Leonid E. Popov ◽  
Lars E. Holmer

A unique specimen of the micromorphic fossil lingulate (organophosphatic-shelled) brachiopod Linnarssonia constans Koneva, 1983 from the late Lower Cambrian Shabakty Group of the Malyi Karatau Range in Kazakhstan, Central Asia, preserves evidence of infestation within the mantle cavity by a vermiform animal, leading to the growth of an internal tubular protuberance (Fig. 1) resulting from symbiosis some 520 million years ago. Examples of symbiotic relationships between metazoans in the early Paleozoic are sparse (Conway Morris, 1981, 1990; Conway Morris and Crompton, 1982). Descriptions of a variety of galls and tumorlike swellings in some trilobites extend records back to the Middle Cambrian (Conway Morris, 1990), but their interpretation as traces of endoparasitic activity remains somewhat speculative. Thus galllike swellings on the stems of Silurian echinoderms (Franzen, 1974), vermiform tubes on some early Ordovician dendroid graptolites (Conway Morris, 1990), and various tubes and blisters on graptoloid graptolites (see Bates and Loydell, 2000 for review) are among the hitherto earliest known convincing records of host-parasite relationships within metazoans. Our example reported here predates the oldest of these previous records by approximately 35 to 40 million years, and demonstrates that symbiosis involving complex adaptations (e.g., larval settlement on or within living tissue and exploitation of feeding systems of the host) and codependent life cycles were already established soon after the ‘explosive’ evolutionary radiation of marine metazoans in the early Cambrian. The fossil evidence of infestation on lophophorates is especially sparse, at best. The oldest hitherto undoubted records are both from brachiopods of Devonian age, in the Lower Devonian Emsian Stage of eastern Australia and in the Middle Devonian Givetian Stage of the Holy Cross Mountains in Poland, respectively.


1988 ◽  
Vol 232 (1269) ◽  
pp. 431-442 ◽  

The protobranch bivalve mollusc Yoldia eightsi Courthouy is both a deposit feeder (on mud) and a suspension feeder (on diatoms in the ventilatory streams, which are trapped on the ctenidia). The species has a similar anatomy to other Yoldia species, but is a more shallow burrower which adopts a more horizontal shell orientation than the vertically burrowing Yoldia limatula and Yoldia ensifera . Although capable of feeding on the surface layers of mud by extending its palp proboscides outside the partly buried shell, Yoldia eightsi spends most of its time feeding while totally buried. To do this, sediment is taken into the mantle cavity by opening the shell valves, or by foot movements. The sediment is moved by ciliary action to the posterior part of the mantle cavity where it forms a compact, mucus-coated sediment slug. The slug is repeatedly sorted largely by the palp proboscides, fine material being transferred to the mouth via the palps. Sorting appears to be done on a simple size–density basis, with large, dense particles being rejected. After sorting, the inorganic fraction of the slug is expelled through the inhalant siphon (‘pseudofaecal plume’). Expulsions occur every 6–35 min. True faeces (‘faecal plume’) are expelled much more frequently in the expiratory bursts of water from the exhalant siphon. Pseudofaecal output is about 170 times the faecal output (on a dry mass basis), suggesting that Yoldia eightsi ingests 0.6% of processed material.


2020 ◽  
Vol 3 (6) ◽  
pp. 578-581
Author(s):  
HUAN-YU LIAO ◽  
XIN-NENG LIAN ◽  
JIAN GAO ◽  
CHEN-YANG CAI ◽  
ZHUO FENG ◽  
...  

Clam shrimp (Spinicaudata) are worldwide distributed branchiopod crustaceans specialised in ephemeral freshwater habitats. The Carboniferous is an important period for the early evolution and diversification of clam shrimp. Compared with the rare and geographically confined fossil record of the Devonian, clam shrimp in the Carboniferous have a much wider geographical distribution and higher biodiversity. Over 20 genera of clam shrimp have been recorded in the Carboniferous all over the world, but they are sparse in China. To date, five records of Carboniferous clam shrimp have been reported from China (Pruvost, 1927; Zhang et al., 1976; Wang, 1987; Zheng et al., 1988; Liu & Fan, 1995; Liao et al., 2019). Among them, four species Lioestheria? mathieui Pruvost, 1927, Protomonocarina huixianensis Wang, 1987, Retrofractus lingyuanensis Liu & Fan, 1995, and Pemphilimnadiopsis cheni Liao, Shen & Huang, 2019, are found in the Pennsylvanian Benxi Formation in North China (Pruvost, 1927; Zhang et al., 1976; Wang, 1987; Liu & Fan, 1995; Liao et al., 2019).


Author(s):  
T. H. J. Gilmour

The structure and ciliation of the lip-apparatus of two species of Lima—L. hians (Gmelin) and L. excavata (Fab.)—and one species of Pecten—P. maximus (L.)—is described.It is suggested that the lips of these three species of bivalves have been hypertrophied (and in one case partially fused) in order to retain particulate material being carried from the ctenidia to the mouth while at the same time allowing the escape of water currents, generated by the ciliary tracts of the ctenidia and palps, from the proximal oral grooves. Such water currents must emerge from between the lips of all bivalves but do not usually interfere with the passage of particulate material. In the Limidae and Pectinidae, these water currents have been intensified by the reduction of the anterior regions of the mantle cavity. Since this change in the proportions of the body can be correlated with the evolution of the monomyarian condition in the Anisomyaria, it is postulated that the lips of all monomyarian Anisomyaria will be similarly hypertrophied.


1990 ◽  
Vol 68 (6) ◽  
pp. 1137-1144 ◽  
Author(s):  
Jon L. Norenburg ◽  
Joan D. Ferraris

A glandular cushion, called the pedal aperture gland in this paper, lies adjacent and internal to each of the two mantle margins composing the pedal aperture of the soft-shelled clam Mya arenaria. Two types of glandular cells are found in the glands. The principal type (bacillary mucous cell) manufactures secretory vesicles that contain discrete protein-rich fibers in a matrix of glycoprotein. The second type (mucous goblet cell) produces sulfated and nonsulfated mucosubstances. The glands function in the formation of pseudofeces from particulate material, especially burrow sediments that enter the mantle cavity through the pedal aperture. Their possible phylogenetic relationship to similar glands in other bivalves is discussed briefly.


2015 ◽  
Vol 227 ◽  
pp. 487-490 ◽  
Author(s):  
Witold Walke ◽  
Zbigniew Paszenda ◽  
Marcin Basiaga ◽  
Paweł Karasiński ◽  
Marcin Kaczmarek

In their works the authors presented results of tests conducted for titanium Grade4 after its surface modification with the application of anodic oxidation and sol-gel (SiO2 layer) methods. In order to verify the usefulness of the obtained surface layers potentiodynamic and impedance tests have been carried out. They have been conducted with the use of measurement set equipped with the POSTAT 302n potentiostat with the FRA2 attachment for impedance tests. Measurements have been taken in an environment simulating human blood – artificial serum having temperature of T = 37 degrees Centigrade. To identify phenomenon occurring at phases border samples have been subjected to 28-day exposition in the artificial serum. It has been found that in the case of anodic oxidation the value of voltage of 100 V has an advantageous influence on electrochemical properties of modified surfaces. On the other hand, in the case of the sol-gel method thin layer of SiO2 baked at temperature T = 430 degrees Centigrade has been characterised by the most advantageous set of electrochemical properties. The knowledge of proper parameters of creating of surface layers has direct influence on the product quality and thus, appropriate course of patient therapy process.


2019 ◽  
Vol 36 (03) ◽  
pp. 171-176
Author(s):  
Jason W. Yu ◽  
Jordan D. Frey ◽  
Vishal D. Thanik ◽  
Eduardo D. Rodriguez ◽  
Jamie P. Levine

Abstract Background The lateral femoral circumflex artery (LFCA) system, which supplies the anterolateral thigh (ALT) flap territory, offers a plethora of tissue types for composite, functional reconstruction. However, the ability to include a reliable and flexible osseous component is limited. Based on cadaveric dissections, we describe an isolated LFCA branch to the femur separate from the vastus intermedius that can be included in ALT flap harvest in cases requiring bony reconstruction. Methods Cadaveric dissection was undertaken to define the LFCA vascular system with specific dissection of the proximal branches of the descending branch of the LFCA (db-LFCA) to define any muscular, periosteal, and/or osseous branches to the femur. Results Six thighs in four cadavers were dissected. Consistent in all specimens, there was an isolated branch extending distally, medially, and posteriorly from the proximal LFCA and entering the periosteum of the femur. In five specimens, the identified branch to the femur was located approximately 1-cm distal to the rectus femoris branch of the LFCA and approximately 1-cm proximal to a separate branch entering and supplying the vastus intermedius. In one specimen, there was a common trunk. The length of this branch from the origin at the LFCA to insertion into the femoral periosteum was approximately 6 to 8 cm. Conclusion There appears to be a consistent and reliable branch to the femur based on the proximal LFCA that may be included in ALT flap harvest, adding even more versatility, as another option in complex cases requiring composite reconstruction, including bone.


Author(s):  
A. R. Waterston ◽  
A. V. Holden ◽  
R. N. Campbell ◽  
P. S. Maitland

SynopsisThe Outer Hebrides comprise approximately 1·3% of the land area but 15·8% of the area of standing waters of Great Britain. Streams there are generally small and only three are as large as fifth order. The majority of the lochs occur below 200 m altitude and are less than 25 ha in area. A total of 1375 stream systems enter the sea, and drain the land mass through 9240 stream segments. There are just over 6000 lochs, of which less than half are connected to these networks. Most of the water systems are on geologically base-poor rock or soil, and less than 3%, situated on machair, are base-rich and eutrophic. The islands, due to their situation, receive precipitation in the form of very dilute sea water (with some non-marine sulphate probably derived from fossil fuel combustion) and this leads to unusual concentrations of chloride in the inland waters. Metamorphic rocks are resistant to weathering, so there is usually little variation in the composition of fresh waters except in the machair areas, where calcareous sands affect calcium concentrations and alkalinities.The flora and fauna reflect the aqueous conditions and there are some unique successions of species from high to low salinities even in the same water body. The lochs provide a wide range of habitats for aquatic vegetation, ranging from the rich machair lochs to the oligotrophic peaty lochs (which show marked similarities with their counterparts on the mainland). Three broad categories can be delineated on the basis of their water quality and vegetation: brackish lochs with varying degrees of marine influence, calcareous machair lochs which may also be affected by sea connections, and the peaty lochans of low alkalinity. A few brackish water animals are sufficiently euryhaline to exist in the machair lochs, which are otherwise dominated by freshwater species. The occurrence of chloride in inland waters enables some crustaceans, e.g. Neomysis integer, Gammarus duebeni and Diaptomus wierzejskii to extend into what are poor freshwater habitats. The main constituents of the freshwater fauna are molluscs and arthropods, and a few species of euryhaline fishes, i.e. salmon, sea and brown trout, three-spined and ten-spined sticklebacks and eels. There are some populations of non-migratory charr. No amphibians are present.


2021 ◽  
Author(s):  
Rossella Calvaruso ◽  
Janice Lawrence ◽  
Adrian Reyes-Prieto

Glaucophytes, red algae and viridiplants (green algae and land plants) are formally united in the supergroup Archaeplastida. Although diverse molecular and genomic evidence suggest the common origin of the three Archaeplastida lineages, the lack of a robust glaucophyte knowledgebase has limited comprehensive evaluations of competing hypotheses. Glaucophytes are rare and apparently confined to freshwater habitats. However, the distribution and diversity of these algae have not been thoroughly explored owing to challenges with detecting and isolating novel specimens. Here we examined the cytometric signatures of representative species of the genera Cyanophora, Cyanoptyche, Glaucocystis and Gloeochaete for a distinctive signal that would aid identification. Most glaucophytes analyzed presented a relatively high red fluorescence signal due to the presence of the blue phycobiliproteins C-phycocyanin and allophycocyanin. Cell-size differences and the concurrent presence of the red phycobiliprotein phycoerythrin in other algal lineages, such as red algae and cryptophytes, allowed us to distinguish glaucophytes from other photosynthetic cells containing blue phycobiliproteins. We used fluorescence-assisted cell sorting (FACS) to isolate viable Cyanophora and Glaucocystis individuals from existing cultures. Our results indicate that the peculiar autofluorescence signal of glaucophytes will facilitate further identification and isolation on novel specimens of this scarce but important algal group.


1984 ◽  
Vol 75 ◽  
pp. 407-422
Author(s):  
William K. Hartmann

ABSTRACTThe nature of collisions within ring systems is reviewed with emphasis on Saturn's rings. The particles may have coherent icy cores and less coherent granular or frosty surface layers, consistent with thermal eclipse observations. Present-day collisions of such ring particles do not cause catastrophic fragmentation of the particles, although some minor surface erosion and reaccretion is possible. Evolution by collisional fragmentation is thus not as important as in the asteroid belt.


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