Oichnus simplex Bromley infesting Hemipneustes striatoradiatus (Leske) (Echinoidea) from the Maastrichtian type area (Upper Cretaceous,The Netherlands)

Abstract

The large holasteroid echinoid Hemipneustes striatoradiatus (Leske) was exploited by diverse invertebrate encrusters and borers during the Maastrichtian, both pre- and post-mortem. In life, the specimen described herein was perforated by multiple Oichnus simplex Bromley borings close to the apical system. Each engendered a growth reaction from the echinoid, a mound-like swelling on the external surface of the test with the boring at the centre. These would have been moved away from the apical system as the echinoid grew and inserted new plates apically. Whether this infestation was the product of numerous individual organisms or, less likely, just one organism (gastropod?) that relocated when discouraged by each mound-like swelling is uncertain. Similar growth reactions are known from other echinoderms, but associated with non-penetrative Oichnus paraboloides Bromley.     

A Dense Infestation of Round Pits in the Irregular Echinoid Hemipneustes striatoradiatus (Leske) from the Maastrichtian of the Netherlands

A test of the holasteroid echinoid Hemipneustes striatoradiatus (Leske) from the upper Meerssen Member (subunit IVf-6; Maastricht Formation) in the type area of the Maastrichtian Stage (Late Cretaceous) was infested by 170 non-penetrative pits assigned to Oichnus excavatus (Donovan and Jagt). The echinoid is assumed to have been alive at that time. The distribution of pits is approximately bilaterally symmetrical and mainly supraambital; pits on the oral surface may have been carried subambitally by echinoid plate growth. Many pits are comparatively shallow; they probably were partly filled by the echinoid after death of the pit-forming organisms. The area around the periproct is devoid of pits as is the anterior ambulacrum (amb III). The latter was probably kept free of larval pit-formers by the tube feet; other ambulacra, with tube feet adapted for respiration, lacked such defense.     

Entobia exogyrarum (Frič, 1883) from the Upper Cretaceous of the Bohemian Cretaceous Basin

The validity of the little-known ichnospecies Entobia exogyrarum (Fri?) is verified. Shells of an oyster, Rhynchostreon suborbiculatum (Lam.), represent the substrate for the sponge borings. The borings occur in many Upper Cenomanian to Middle Turonian localities of the Bohemian Cretaceous Basin. This study revealed that the sponges attacked shells of living oysters. Entobia exogyrarum (Fri?) also represents one of the shallowest occurrences of Entobia borings in the Upper Cretaceous rocks.     

Bored and Burrowed: An Unusual Echinoid Steinkern from the Type Maastrichtian (Upper Cretaceous,Belgium)

A test of the irregular echinoid Hemipneustes striatoradiatus (Leske) was dissolved in dilute hydrochloric acid to expose the flint steinkern. This revealed slender, string-like borings that were mainly limited to ambulacra (Talpina isp. cf. T. canna (Price)); less common pouch-like borings limited to part of one ambulacrum only (Rogerella isp. cf. R. pattei (Saint Seine)); and slender, sinuous to contorted burrows, Planolites montanus Richter. Ingress to the test (borers) and sediment infill (burrowers) was presumably through the ambulacral pore pairs of the dead test. Borings and burrows were probably not coeval. Such infestations of fossil echinoids may be locally common, but their identification is controlled by the difficulty of seeing features of both the test and the infill.     

Site Selectivity of the Pit Oichnus excavatus Donovan and Jagt Infesting Hemipneustes striatoradiatus (Leske) (Echinoidea) in the Type Maastrichtian (Upper Cretaceous,The Netherlands)

Two tests of the holasteroid echinoid Hemipneustes striatoradiatus (Leske) from the type area of the Maastrichtian Stage (Upper Cretaceous) bear a varied infestation of episkeletozoans (oysters, bryozoan colony, and serpulids), borings (probable Caulostrepsis isp., Oichnus simplex Bromley), surface abrasion (Gnathichnus? isp.), and pits (O. excavatus Donovan and Jagt). Only O. excavatus represents a premortem infestation. In one specimen, the four individual pits of this ichnospecies are each associated with a different ambulacrum and pore pairs that, in life, bore respiratory tube feet; the anterior ambulacrum, of different gross morphology, is not infested. In the second test, three out of four of the same ambulacra are infested, although there are also O. excavatus in the interambulacra. The association between O. excavatus and the ambulacra of the echinoid, and thus its tube feet, is open to several plausible explanations, but most likely provided some form of feeding or protective advantage to the pit-forming organism.     

Salenioid Echinoids from the Maastrichtian (Upper Cretaceous) of Belgium and The Netherlands

The Salenioid echinoids in the Royal Belgian Institute for Natural Sciences, from the Belgian and Dutch Maastrichtian (Upper Cretaceous) are systematically revised. Three species belonging toSalenidia, and three belonging toSalenia are redefined. One new species(Salenidia sanctipetri) is named and described.Salenidia maestrichtensis is represented by many specimens of all ages, allowing morphological variation, to be traced during growth.     

Shallow Traces (Pits) in the Test of the Irregular Echinoid Echinocorys scutata Leske from the Chalk (Upper Cretaceous) of the United Kingdom

Specimens of epifaunal irregular echinoids in the Upper Cretaceous of northern Europe have been reported with patterns of circular, nonpenetrative parabolic pits, Oichnus paraboloides (Bromley), in the apical region. Specimens of Echinocorys scutata Leske from the Chalk at two sites in southeast England were commonly penetrated by this trace, generated by an indeterminate pit-forming organism. Pits commonly surround the apical system and, less commonly, occur within it; they occur preferentially anteriorly. Pits occur within plates, not along margins or sutures. Crosscutting of pits indicates that multiple spatfalls probably occurred. The host echinoid added new test plates adjacent to the apical system; thus, plates bearing O. paraboloides were moved abapically. The reduction in number of pits away from the apex, including those with echinoid tubercles reestablished on the base, indicates that, following death of an infester, the echinoid “reclaimed” and infilled them with calcite. The pit-former was most probably an unmineralized invertebrate that used E. scutata as a domicile which provided good access to food-rich currents for suspension feeding. Although the systematic position of the pit-former is unknown, similar infestations are known from other Upper Cretaceous echinoids and Mississippian crinoids.     

Dasycladales from the Upper Maastrichtian of Salento Peninsula (Puglia, southern Italy)

Summary A rich dasycladalean assemblage, mainly consisting of new taxa, has been discovered in upper Maastrichtian coarse bioclastic limestones of shelf margin facies cropping out along the southeastern coast of Salento peninsula (Puglia, Southern Italy). It consists of 8 species grouped into 6 genera:Cymopolia decastroi Parente 1994;C. barattoloi Parente, 1994;Zittelina fluegeli n.sp;Jodotella koradae (Dieni, Massari & Radoicic, 1983) nov. comb.;Barattoloporella salentina n. gen. n. sp.;Morelletpora dienii n. sp.;Neomeris spp. (two different species). Zittelina fluegeli n. sp. is characterized by an ovoid thallus with calcification made by a calcareous wall enveloping only the proximal part of the branches (except in basal whorls) and by closely packed, and partly coalescent, calcified ampullae arranged all around the median and distal portion of branches. The transferral ofNeomeris (Larvaria) koradae Dieni, Massari & Radoicic, 1983 into the genusJodotella, with the new combinationJodotella koradae, is proposed on the basis of new observations on the number and arrangement of fertile ampullae. The new genusBarattoloporella, type-speciesBarattoloporella salentina n. gen. n. sp., is erected for dasycladalean algae characterized by a segmented thallus. Each segment consists of: a) basal and apical sterile whorls made by primary branches only, b) central fertile whorls made by primary branches bearing in terminal position one fertile ampulla and one or two secondary branches. morelletpora dienii n. sp. is characterized by a segmented thallus with barrel shaped to pear shaped repetitive elements, consisting of simple whorls of first order branches only. Shape of the branches varies from regularly phloiophorous to more or less differentiated in a stalk and a swollen portion, with or without a subterminal constriction. This is by far the most diverse dasycladalean assemblage ever found in the Maastrichtian. Its diversity supports the conclusion that, within the Late Cretaceous, the Maastrichtian represents a maximum in dasycladalean diversity. Its taxonomic composition strenghtens the hypothesis that dasycladaleans were hardly affected by K/T mass extinction.     

Mass mortality of an asteriid starfish (Forcipulatida,Asteroidea, Echinodermata) from the late Maastrichtian (Late Cretaceous) of Morocco

Abstract: A mass occurrence, numbering tens of thousands of individuals in a single lens, belonging to a single species of asteroid, is described from the late Maastrichtian (Late Cetaceous) of Morocco. The lens of partially silicified asteroidal limestone is made up largely of fully articulated specimens of similar size and probably represents the mass mortality of a single recruitment. By comparison with mass strandings of the present‐day species Asterias rubens (Linnaeus), it can be inferred that a feeding swarm of individuals was swept into a submarine channel by either a storm or an exceptionally strong tidal current, and permanently buried. The genus and species are herein described as Cretasterias reticulatus gen. et sp. nov. The exceptional preservation of the material enables the identification of wreath organs (clusters of crossed pedicellariae set in a dermal pad around spines) for the first time in the fossil record. Comparison between extant Asteriidae, putative fossil asteriids and C. reticulatus provides ambiguous evidence of its affinities; it appears to display a combination of plesiomorphic and derived characters. It is shown that all Mesozoic forcipulatid asteroids described so far share a very simple arm construction (single row of adradial ossicles) unknown in adult extant Forcipulatida.     

Bivalve Wood Borings of the Ichnogenus Teredolites Leymerie from the Bohemian Cretaceous Basin (Upper Cretaceous,Czech Republic)

Finds of fossil wood with bivalve wood borings (Teredolites clavatus and T. longissimus) occur in various facies and presumed sedimentary settings of the platform, shallow-marine Bohemian Crectaceous Basin. The basin comprises areas with sandy-dominated sediments, with marl and clay-dominated sediments, areas with predominat sandy-marly rocks, and finally areas dominated by calcareous nearshore sediments. Teredolites clavatus is common in fossil wood of sandstones, originating in beach or deltaic settings; marl and clay-dominated rock frequently bear wood fragments densely bored by Teredolites longissimus. When accompanied by evidence of marine environments as body fossils, glauconite or typical trace fossils, most of the wood fragments are bored. The presence/absence of borings in wood fragments can be considered the most reliable and easily useable criterion of distinction of marine settings in sandy sediments of the margin of the Bohemian Cretaceous Basin.     

Titanosaur eggshells from the Tremp Formation (Upper Cretaceous,Southern Pyrenees,Spain)

Hundreds of megaloolithid eggshells have been found at the Costa de la Coma site (Tremp Fm, South-Central Pyrenees, Spain), the microstructural features (spherulitic eggshell units, thickness, ornamentation and pore system) of which agree with the Megaloolithus oogenus diagnosis. Comparisons with other megaloolithids from the Tremp Basin, southern France and South America, however, showed that these eggshells share many features with the South American oospecies Megaloolithus patagonicus. A cladistic analysis of the qualitative eggshell features of the main dinosaur taxa was performed. The results grouped the Costa de la Coma eggshells with Megaloolithus patagonicus, forming a clade separated from other megaloolithids, and revealed a polytomy of megaloolithids (associated with sauropods) and spheroolithids (associated with hadrosaurs). The finding of Megaloolithus cf. patagonicus in the Tremp Fm agrees with skeletal evidence provided by four indeterminate titanosaur forms from the Formation's late Cretaceous deposits. Other Megaloolithus oospecies of the Tremp Fm may belong to hadrosaurs, the skeletal remains of which are also abundant in the Tremp Basin.     

The Boring Cunctichnus probans Fürsich,Palmer and Goodyear, 1994, from the Type Maastrichtian (Upper Cretaceous,Northeast Belgium)

The ichnogenus Cunctichnus Fürsich, Palmer and Goodyear, 1994 is monotypic, its type ichnospecies, C. probans Fürsich, Palmer and Goodyear, 1994, having hitherto been described solely from the Upper Jurassic (Tithonian) of southern England and the Paris Basin. Cunctichnus probans is recorded herein from the type Maastrichtian (Upper Cretaceous) of the province of Liège, northeast Belgium, that is, about 75 million years younger than previous published records. This specimen differs from the holotype in having a Y-shaped branch.     

Arbacioid echinoids from the maastrichtian (Upper Cretaceous) of Belgium and the Netherlands

Arbacioid Echinoids from the Maastrichtian of the Benelux countries, present in some Belgian and Dutch collections, are systematically revised. Three species, belonging to two genera are identified and described.     

The Upper Cretaceous belemnite <Emphasis Type="Italic">Praeactinocamax plenus</Emphasis> (Blainville, 1827) from Lower Saxony (Upper Cenomanian,northwest Germany) and its distribution pattern in Europe

Occurrences of the Upper Cenomanian (Upper Cretaceous) belemnite Praeactinocamax plenus from the plenus Bed of northwest Germany (Söhlde-Loges working quarry near Salzgitter, Lower Saxony) are documented and described for the first time on the basis of two in situ finds. The find horizon and its surrounding beds are re-evaluated in a sequence stratigraphical context. In contrast to the interpretations of other authors, the plenus Bed is seen as a pelagization event in a parasequence of transgressively stacked beds, delimited by two significant erosion surfaces below and above. The exclusive occurrence of P. plenus in the top part of the plenus Bed and its absence from the post-plenus Bed succession, in the equivalent of which (higher part of the Plenus Marls Member) it is very common in southern England (Anglo-Paris Basin), is explained by ecological factors in stratigraphically complete sections (intra-shelf depressions) and by gaps in the stratigraphic records in swell settings. The distribution pattern of P. plenus suggests a preference for nearshore settings and a demersal mode of life.     

Rogerella isp. Infesting the Pore Pairs of Hemipneustes striatoradiatus (Leske) (Echinoidea: Upper Cretaceous,Belgium)

An otherwise well-preserved test of the holasteroid echinoid Hemipneustes striatoradiatus (Leske) from the Emael Member, Maastricht Formation (Maastrichtian, Upper Cretaceous) of Belgium, is infested by encrusting bivalves and foraminiferans and the boring Rogerella isp. In this specimen, Rogerella preferentially infested and modified the ambulacral pore pairs of the echinoid close to the apex. This was not a commensal association. The echinoid test shows no growth deformations in response to this invasion; pore pairs are locally strongly infested; and encrusting invertebrates testify to the long post-mortem residence time of the test on the sea floor. Rather, the pore pairs of the dead echinoid were crannies attractive to settling larvae of acrothoracian barnacles, the producers of Rogerella.     

History of diatom research in The Netherlands and Flanders

The history of diatom research in The Netherlands and Flanders is summarized in this report. A. van Leeuwenhoek observed diatoms as early as 1702. The first inventories were made in The Netherlands by R. B. van den Bosch (1846) and in Flanders by J.-J. Kickx (1867). Diatoms were already used in geological research in the second half of the nineteenth century. The Synopsis by H. van Heurck (1880–1885) enabled many twentieth century workers to do applied research for geological and ecological purposes.     

First titanosaur (Saurischia,Sauropoda) axial remains from the Uberaba Formation,Upper Cretaceous,Bauru Group,Brazil

The Adamantina and Marília formations are considered to be the richest vertebrate-bearing units in the Bauru Group, Upper Cretaceous, Brazil. In contrast, the fossil content from the Uberaba Formation, which only outcrops in Minas Gerais State, is scarce and poorly understood. In this essay the first taxonomically informative titanosaur remains unearthed from this unit are reported. They comprise anterior caudal vertebrae from two different individuals corresponding to a probably basal titanosaur (CPP-360) and a derived titanosaur (CPP-217). Although these remains can be clearly distinguished from other titanosaurs on the basis of their unique association of characteristics like the presence of mildly procoelous centra, lateral pits in the anterior caudal vertebrae, and prezygapophyses with a dorsal protuberance in anterior caudals in CPP-360 and the presence of strongly developed prespinal, spinopostzygapophyseal and centropostzygapophyseal laminae in CPP-217, more complete materials are needed to propose them new names.     

On the finding of ornithomimid dinosaurs (Saurischia, Ornithomimosauria) in the Upper Cretaceous beds of Tajikistan

Fragmentary remains of ornithomimids (Ornithomimidae indet.) from the Lower Santonian (Upper Cretaceous) Kansai locality in northwestern Fergana (Tajikistan) are described, and the composition of its dinosaurian assemblage is updated.