Geometric shell growth and mode of life of a Devonian chonetoidean brachiopod

Morphological and statistical analysis of the chonetoid species Kentronetes variabilis from the Lower Devonian (Lochkovian) of the Argentine Precordillera demonstrate ontogenetic changes and allometric relationships between characters. A special study was made of spine distribution, morphology, and growth, compared to valve growth. The first, inner, developed spines (pairs 1–1'and 2–2') continued to grow after development of the following outer pairs. The spacing of spines, their diameter, and the density of growth rings vary from beak to posterolateral margins following a specific 2ⁿ geometric growth factor, compared to the regular, almost linear growth of the valves, attested by growth lines. The linear growth rate of outer spines (pairs 3–3'and 4–4') can be 6–8 times more rapid than that of the shell on the valve margin. Ontogenetic changes in spine morphology are interpreted as a response to changes in the mode of life.     

The mesolophe, a new lophophore type for chonetacean brachiopods

Rachebaeuf, P. R. & Copper, P. 1990 10 15: The mesolophe, a new lophophore type for chonetacean brachiopods. Lethaia , Val. 23, pp. 341–346. Oslo. ISSN 0024–1164.
Following a summary of previous lophophore reconstructions for the chonetaceans, we describe an unusual pyritized structure within the calcite infill of an exceptionally preserved shell of Archeochonetes primigenius (Twenhofel) from the Late Ordovician (Ashgill) of Anticosti Island, Quebec, Canada. The brachial valve interior of most Lower Devonian to Permian chonetaceans shows the development of three depressed deepened areas (gutters) in the valve floor. The disposition of these gutters coincides remarkably with the shape of the pyritized structure, which we postulate as a new type of lophophore, the mesolophe. ▭ Brachiopoda, Chonetacea, functional morphology, lophophore .     

Notes on the phylogeny of the nautiloidea

Critical notes on the monograph “Phylogeny of the Nautiloidea” by J. Dzik (1984), especially with respect to cephalopod material from the Lower Palaeozoic of Bohemia are presented. Oncocerid type of muscle scars in the Lower Devonian genusPtenoceras as well as succession of growth stages of the shell in Silurian genusSphooceras is figured.     

New insights into early land ecosystems: a glimpse of a lilliputian world

Small, relatively uncompressed, very fragmentary plant remains (mesofossils) are described from a Silurian (P ídolí) and a Lower Devonian (Lochkovian) locality in the Welsh Borderland. Excellent cellular preservation provides characters leading to the demonstration of diversity in plants of simple gross morphology and allows deliberations on functional anatomy (e.g. of stomata), and reproductive biology (including development and dehiscence of sporangia). A survey of in-situ spores is presented, and preliminary comparisons made with dispersed spore assemblages especially in relation to reconstruction of vegetation on local and regional scales. The earliest body fossils of unequivocal terrestrial arthropods isolated from the same locality as the P ídolí plants suggest that the decomposer/microherbivore/predator soil and litter communities found in the Lower and Middle Devonian extend back at least into the Silurian. Evidence for plant—animal interaction in the Lower Devonian comes from spore-dominated coprolites believed to have been produced by litter-feeding myriapods.     

Species-specific growth responses of favositid corals to soft-bottom substrates

Gibson, Michael A. & Broadhead, Thomas W. 1989 07 15: Species-specific growth responses of favositid corals to soft-bottom substrates. Lethaia , Vol. 22, pp. 287–299. Oslo. ISSN 0024–1164.
Species of favositid corals from the Upper Silurian and Lower Devonian of Tennessee, USA, exhibit structural modifications related to corallum geometry, interfacial skeletal material, and biotic associations that enabled them to survive in terrigenous mud rich environments. Favosites conicus Hall (Lower Devonian) had a flat, holotheca-covered base and a radial pattern of colony growth, but apparently had a short life span and may not have survived beyond the first reproductive cycle (monocarpous). It was adapted for living between major episodes of terrigenous mud influx. F. foerstei (Lower Devonian) had a convex, pseudoholotheca-covered base and a modified axial pattern of colony growth. Its large size, in comparison to that of F. conicus , suggests a longer lived colony (polycarpous), in which continued upward and outward growth enabled it to survive episodic sediment influx. F. forbesi (Upper Silurian) exhibited radial growth to form either (1) a globose corallum that was symbiotic with the stalks of living crinoids permitting the colony to live entirely above the substrate, or (2) a Gorallum with a steeply convex, holotheca-covered base that represents a bottom-dwelling colony in which the rate of growth probably only slightly exceeded the rate of sediment accumulation. * Functional morphology, astogeny, paleoecology, Tabulata .     

First report of brachiopod–brachiopod endoparasitism

Schemm-Gregory, M. & Sutton, M. 2010: First report of brachiopod–brachiopod endoparasitism. Lethaia , Vol. 43, pp. 111–115.
The first example of brachiopod–brachiopod endoparasitism is reported from the Lower Devonian of China. Three-dimensional reconstructions following serial sectioning show a specimen of a strophomenide ( Dicoelostrophia sp.) within an articulated shell of the spiriferide Rostrospirifer tonkinensis ; morphological modifications of the host and the positioning of the strophomenide with respect to the inhalant current demonstrate the in vivo nature of the association. The symbiosis is interpreted as parasitic; it appears to be facultative but demonstrates the viability of this mode of life, expanding the ecological range known to be exploitable by the Brachiopoda. □ 3-D reconstruction , Brachiopoda , Dicoelostrophia , endoparasitism , Lower Devonian , Rostrospirifer .     

Biological aspects of theoretical shell morphology

Savazzi, E. 1990 04 15: Biological aspects of theoretical shell morphology. Lethaia . Vol. 23 , pp. 195–212. Oslo. ISSN 0024–1164
Among the available methods in theoretical shell morphology. moving-frame method, produce the broadest range of shell shapes and appear to emulate most closely the biological processes involved in shell morphogenesis and growth. In addition, moving-frame methods can easily be enhnneed in both respects by adding operations that are similar in nature to the original procedures. Improvements beyond this point. however. require a qualitative change in approach. The focus of attention must he transferred from the shell lo the soft parts involved in shell construction. This may be done by (1) regarding the soft parts a5 pneus. and (2) controlling their shape and metabolism through morphogenetic programme based on biochemical reactions. * Theoretical morphology. functional morphology, modelling. computer graphics, Mollusca. Gastropoda. Bivalvia. Brachiopoda .     

Schischcatella (Fenestrata,Bryozoa) from the Devonian of the Rhenish Massif,Germany

Abstract: The Devonian fenestrate bryozoan, Schischcatella Waschurova, 1964 , possessed colonies in the form of low, erect bifoliate fronds that grew from an encrusting sheet‐like base with autozooecia arranged in biserial, bifurcating rows. This growth habit is unique in fenestrates, which normally had unilaminate arborescent colonies. Originally, Schischcatella was described from the Lower Devonian of Tajikistan. This article describes a new species, S. heinorum sp. nov., from the Middle Devonian of the Eifel (western Rhenish Massif, Germany) with additional material from the Lower Devonian of the Kellerwald (eastern Rhenish Massif, Germany). External and internal morphologies of this bryozoan have been studied using abundant material. The growth habit of Schischcatella suggests a completely different pattern of feeding currents than that in the normal fenestrate colony. The outflow of the filtered water occurred only on edges of colonies between rami. In the absence of chimneys (areas of vertical water expelling), such a functional morphology may have restricted extension of the colony in a distal direction. The evolution of Schischcatella is apparently an example of paedomorphosis, the genus evolved from an unknown semicosciniid species by the early ontogenetic interruption of colony development and further changes in the mode of growth.     

Considérations paléobiogéographiques sur les Streptelasmatina (Coelenterata,Rugosa) solitaires du Dévonien des monts Cantabriques (NW de l'Espagne)

The study of numerous fossil solitary forms ofStreptelasmatina (Coelenterata, Rugosa) and some ones belonging to different suborders from the Devonian of the Cantabrian Mountains (NW Spain), shows the importance of such organisms concerning the relations among the major faunal provinces during the Devonian time.The analysis of the Devonian Rugose coral fauna(from Emsian to Frasnian) lets to establish the paleobiogeographical relations of the Cantabrian genera. Particularly, during the Lower Devonian (Emsian) the relationships between the Eastern of North America and Spain would be closer than it was supposed until now.The evidence on the world distribution of thestudied forms suggest possible migration roads.     

Changes in the timing of mantle formation and larval life history traits in linguliform and craniiform brachiopods

The distribution of embryonic and larval mantles is documented in linguliform and craniiform brachiopods. Criteria are presented for identifying these mantle types. The mantle type is related to planktotrophic and lecithotrophic larval life history patterns. In the Linguliformea and Craniiformea, all Lower Palaeozoic families with adequate preservation had larval mantles, indicating the presence of a planktotrophic larva. Heterochronic changes in the time of mantle origin, from the larval to the embryonic stage of development, has occurred several times. In the Lingulidae this change appears to have taken place at about the time the family originated in the Devonian and has been retained in extant genera. The family Discinidae has also retained a planktotrophic larval stage from the Lower Palaeozic to the present. The extant genus Crania in the Craniidae has a short-lived lecithotrophic larva that lacks a mantle. Through the Lower Jurassic, this family had planktotrophic larvae with a larval shell. During the Upper Jurassic, genera with a lecithotrophic larva that lacked a larval shell began to appear; however, the last genera in this family with a planktotrophic larva and a larval shell did not become extinct until the Tertiary.     

Some morphological adaptations in freshwater bivalves

Savazzi, E. & Yao, P. 1992 04 15: Some morphological adaptations in freshwater bivalves. Lethaia , Vol. 25, pp. 195–209. Oslo. ISSN 0024–1164.
Several freshwater bivalves possess peculiar shell morphologies. An extension of the postero-dorsal shell margins above the hinge line evolved convergently in several unionids. This extension supplements the opening momentum of the ligament, but must be broken off periodically in order to allow further shell growth. Arconaia and Cuneopsis have evolved twisted commissure planes, comparable to those found in unrelated marine bivalves. In marine forms, byssus is believed to have played a fundamental role in the evolution of shell torsion. However, the twisted Unionidae do not possess a byssus in the adult stage, thus forcing us to re-evaluate our ideas on the adaptive value and evolution of shell torsion. Solenaia oleivora is apparently incapable of reburrowing and of retracting its foot within the shell. The foot may be functional as an anchor, and is perhaps involved in chemosynthesis by storing sulphur extracted as sulphide from the surrounding sediment. Other adaptations of freshwater bivalves include selective thickening of portions of the shell that enhance its stability, permanent anterior and posterior gapes, and oyster-like morphologies and shell structures. * Functional morphology, constructional morphology, burrowing, shell torsion, Mollusca, Bivalvia, Unionacea, Recent, Quaternary, People's Republic of China .     

A Middle Devonian symbiotic relationship involving a gastropod, a trepostomatous bryozoan, and an inferred secondary occupant

Morris, P. J., Linsley, R. M. & Cottrell. J. F. 1991 01 15: A Middle Devonian symbiotic relationship involving a gastropod, a trepostomatous bryozoan. and an inferred sceondary occupant. Lethaia , Vol. 24. pp. 55–67. Oslo. ISSN 0024–1164.
The high-spired gastropod Palaeozygopleuru (Loxonematacea) of the Hamilton Group (Middle Devonian) in New York State is often entrusted by the trepostomatous bryozoan Leptotrypella (Hetero-trypidae). The form of this enerustation leads us to infer a secondary occupant that dwelled in empty shells of Palaeozygopleura while the bryozoan grew upon them. Encrusted specimens usually have an open aperture, thin or no enerustation on the apertural side of the gastropod shell. and thick encrustation on the abapertural side. While the aperture is invariably open. the columellar and parictal lips of the aperture, and the apertural face of the first whorl are usually encrusted. While the gastropod is alive, this area rests upon the dorsal surface of the foot and the remainder of the shell rests upon the substratc. These encrustation patterns suggest that an occupant of the shell. other than the gastropexl. prevented overgrowth of the aperture and oriented the shell aperture-down. This allowed ahapertural growth of the bryozoan. The presence of thin encrustation on the apertural side of the shell is problematical. It requires either the presence of a secondary occupant capable of holding a thinly encrusted shell off the substrate, or the ability of the juvenile bryozoan colony to extend onto portions of the shell that were in contact with the substrate. The presence of a secondary occupant. such as a sipunculan worm. capable of lifting the shell, but usually resting it aperture-down on the substrate seems the most suitable explanation for the nature of the encrustation. Gastropoda. bryozoa. symbiosis. Devoniun. hermit crab, Sipuncula     

Devonian floral assemblages and plant megafossils from the Iberian Peninsula: A review

This paper presents a review and critical analysis of the literature on Devonian floras of the Iberian Peninsula. Although the known outcrops of Devonian strata in the Iberian Peninsula are marine, in some cases, a few fragmentary remains of vascular plants are associated with faunal remains. Records include largely specimens from the Lower Devonian of Barrancos (Alentejo, Portugal) and the Upper Devonian of Sierra de Hornachos in Badajoz province, southwest Spain; the remainder consists of drifted plant fragments from scattered sites in the Iberian Peninsula ranging in age from Lochkovian to Upper Devonian-Earliest Carboniferous. The vegetation inferred for the Lower Devonian of the Iberian Peninsula is mainly based on palynological data and corresponds to herbaceous types characterised by bryophytes, rhyniophytes (Horneophyton, Cooksonia, Rhynia), trimerophytes (Psilophyton, Pertica and Hostinella), primitive lycophytes (Drepanophycus) and incertae sedis such as Nothia and Chaleuria, all flora that developed near the coast in low-lying and, at least periodically, wet areas. In the Middle Devonian, two vegetation strata can be recognised: herbaceous (Psilophyton) and semi-arboreal (Cladoxylales). Although three levels of vegetation in the Upper Devonian, have been described from outcrops worldwide, the scarce available data from the Iberian Peninsula only indicate an arborescent lycopsid vegetation and species with uncertain botanical affinity such as Sphenopteridium keilhauii Nathorst.     

Growth and shell morphology of three mytilidae (Bivalvia) species from the Sea of Japan

The growth and shell morphology of bivalve mollusks Crenomytilus grayanus, Mytilus coruscus, and Modiolus modiolus from the Sea of Japan are examined. The changes in body proportions and shell form in the ontogenesis of C. grayanus, M. coruscus, and M. modiolus are different even in the cases when the mussels develop in similar environmental conditions. Rapid growth shapes a well-streamlined and flat form of shell; slow growth leads to the formation of a massive and convex form. The parameters of the Bertalanffy growth curve for each species are calculated. The differences are discussed from the standpoint of functional morphology and spatial distribution patterns of mytilids in the coastal areas of the sea.     

Discovery of soft parts of a fossil brachiopod in the “Hunsrückschiefer” (Lower Devonian, Germany)

The author recently discovered among 16 discinid brachiopods from the Lower Devonian Hunsrück Slate, by using the X-ray technique, two specimens with mineralized soft parts and pedicle. These are truly unique finds, as previously no bodily preserved pedicle of fossil discinids has been described. Also, they prove that in the Hunsriick Slate soft parts can be pyritized. New shell observations give rise to doubts on the generic assignment ofOrbiculoidea mediorhenana Fuchs 1915. By comparing the anatomy of the related, livingLingula with the extinct discinid in question, a reconstruction of the latter is presented.     

Shell structure and affinities of the enigmatic Lower Ordovician articulate brachiopod Lycophoria Lahusen, 1886

Wright, A. D. 1992 04 15: Shell structure and affinities of the enigmatic Lower Ordovician articulate brachiopod Lycophoria Lahusen. 1886. Lethaia . Vol. 25, pp. 125–129. Oslo. ISSN 0024–1164.
The enigmatic Baltoscandian Lower Ordovician brachiopod Lycophoriu has a combination of morphological characters that makes it difficult to place taxonomically. The more recent assignments of the genus have been with the Porambonitacea, the Triplesiacea and the Orthacea. A basic character in articulate brachiopods is the differentiation of the secondary shell into either stacked fibres or laminar sheets. The hitherto unknown shell structure in Lycophoria has been examined under the electron microscope and is shown to be fibrous, which is taken as ruling out any close affinity with the lamellar shelled Triplesiacea. Despite superficial similarities, features of the shell interior are not compatible with the pentameride Porambonitacea and although there are differences from the typical orthacean, these are no greater than those of the accepted orthid Producrorrhis. Lycophoria , in the monotypic family Lycophoriidae, is accordingly best regarded as a specialized offshoot of the basic orthacean stock. * Shell microstructure, Lycophoridae, Orrhacea, Porambonitacea, Triplesiacea, Lower Ordovician, Baltoscandia .     

Evidence of predation in Early Cretaceous unionoid bivalves from freshwater sediments in the Cameros Basin,Spain

Here, we present evidence of possible vertebrate predation on freshwater bivalves from the Lower Cretaceous strata of the Cameros Basin (Spain). The described collection contains the largest number of vertebrate‐inflicted shell injuries in freshwater bivalve shells yet reported in the Mesozoic continental record. Several types of shell damage on fossil shells of Protopleurobema numantina (Bivalvia: Unionoida) are described and their respective modes of formation interpreted in the context of morphological attributes of the shell injuries and the inferred tooth morphology of predators that could have inflicted such injuries. Detailed study of these bite marks shows similarities with the well‐documented injuries in the shells of marine molluscs, namely ammonoids, that have likewise been attributed to reptilian predators. The most parsimonious interpretation suggests crocodiles as the vertebrates interacting with the bivalves in the Cameros Basin. □Barremian–Aptian; bite marks; freshwater bivalves; predation; reptile; Unionoida.     

Wandel der Vorstellungen von der Frühevolution der Mollusken,besonders der Gastropoda und Cephalopoda

The ancestors of the molluscs are still unknown. Arguments in favour of flatworm-relationship are just as valid as those proposing segmented annelid-like worms as their closest relatives. The earliest molluscs lived before the onset of the Cambrian; but only at the end of this period the now existing classes of conchifers made their first appearance. Early and Middle Cambrian molluscan fossils are problematic. The hyoliths, for example, show relations to such fossils asSalterella andVolborthella, while closest living relatives can be found among tube-building annelids. Scars produced by tissue attached to the shell are of no use in the reconstruction of molluscan phylogeny, but a very useful tool in the analysis of the function regarding the body in interaction with its shell. The ontogenesis of the shell and muscles attached to it in recentFissurella (archaeogastropod) is presented as an example. Well known ontogenies in recent molluscs can aid to the reconstruction of fossils, demonstrated by some fossil gastropods. The interaction of soft and hard tissues, the function and structure of the shell of recent molluscs enables us to interpret the fossil forms, as for example the Lower Devonian coleoid cephalopods from the Hunsrück Schiefer. Reconstruction of the course of evolution is only possible, if information on living molluscs is integrated into historical data provided by the fossils.     

Plant and animal cuticle remains from the Lower Devonian of southern Poland and their palaeoenvironmental significance

Filipiak, P. & Zatoń, M. 2010: Plant and animal cuticle remains from the Lower Devonian of southern Poland and their palaeoenvironmental significance. Lethaia, Vol. 44, pp. 397–409. Assemblages of plant and arthropod remains are reported from the Lower Devonian clastic deposits of the Upper Silesian and Ma?opolska blocks in southern Poland. Most of the plant and animal remains are palynologically dated as Pragian–Emsian/Eifelian. The plant material comprises higher plant cuticles with stomata classified as Drephanophycus and Sawdonia, and more enigmatic remains (nematophytes) classified as Nematothallus, Cosmochlaina and tubular banded tubes. They are associated with abundant and diverse miospores. Animal remains consist of eurypterid respiratory organs, the morphology of which may presumably point to their advance physiological properties, and cuticular remains of eurypterid and probably scorpion origin, as well as some remains of unknown affinity. The presence of such mixed assemblages in the Lower Devonian of Poland indicate marginal‐marine and/or alluvial environments spreading in the southern margin of the Old Red Continent. The dominance of land‐derived plant remains and simultaneous scarcity of marine acritarchs indicate that the environment was very weakly influenced by marine conditions. If nematophytes were really related to extant liverworts, as suggested by some workers, they, together with the other associated spore‐producing plants, may strongly indicate moist environmental conditions, which may have offered suitable habitats for temporary eurypterid migrations onto land. □Cuticles, eurypterids, Lower Devonian, nematophytes, Poland, spores.