Micarea Confusa: A New Species from Zinc- and Cadmium-Contaminated Soils in Belgium and the Netherlands

1995 ◽  
Vol 27 (02) ◽  
pp. 81 ◽  
Author(s):  
B. J. Coppins ◽  
P. P. G. van den Boom
1995 ◽  
Vol 27 (2) ◽  
pp. 81-90 ◽  
Author(s):  
B. J. Coppins ◽  
P. P. G. van den Boom

AbstractMicarea confuse, a species easily confused with M. denigrate, is described from heavy-metal contaminated ground in Belgium and The Netherlands. Additional information is provided on the main locality at Budel-Dorplein.


Mycotaxon ◽  
2013 ◽  
Vol 123 (1) ◽  
pp. 467-472 ◽  
Author(s):  
D. Haelewaters ◽  
A. De Kesel

Author(s):  
Jonathan J.W. Wallaard ◽  
René H.B. Fraaije ◽  
Henk J. Diependaal ◽  
John W.M. Jagt

AbstractOn the basis of dissociated and scattered skull bones and several types of scutes and scales of a single, large-sized individual, a new species of dercetid is recorded from the lower to middle portion of the Maastricht Formation (upper Gronsveld, Schiepersberg or Emael members) as formerly exposed at ’t Rooth quarry near Bemelen, east of Maastricht, the Netherlands. This new taxon,Pelargorhynchus grandisn. sp., the fifth dercetid recorded to date from the type area of the Maastrichtian Stage, is characterised by the presence of both large, smooth scutes and small ornamented scales, by the degree of curvature of skull bones, the presence of unfused premaxillae and the lack of teeth.


2003 ◽  
Vol 77 (4) ◽  
pp. 738-744 ◽  
Author(s):  
Paul C. H. Albers ◽  
Olivier Rieppel

A new species of the genusNothosaurusfrom the Lower Muschelkalk of Winterswijk, The Netherlands, shows relatively plesiomorphic features such as a relatively forward position of the pineal foramen. The jugal enters into the ventral margin of the orbit, which would also be regarded as plesiomorphic, were it not that this feature optimizes unequivocally as a reversal and, hence, as a diagnostic (derived) character of the new taxon. The new taxon does not, however, increase the fit of the cladogram for the phylogenetic relationships withinNothosaurusto the stratigraphic record of the genus. The basal position ofNothosaurus juvenilisremains problematic.


2018 ◽  
Vol 23 (4) ◽  
pp. 724 ◽  
Author(s):  
Vladimir Pešić ◽  
Harry Smit

The water mite genus Wettina has a Holarctic distribution and includes only one known species from the Palaearctic, i.e. W. podagrica (Koch, 1837). This species has been considered as a rhitrobiontic and crenophilous species. In the present study we used morphological data and DNA barcoding to describe a new species of the genus, W. lacustris sp. nov. from the glacial Biogradsko Lake in northern Montenegro. The level of COI differentiation between lake population of Wettina lacustris sp. nov. and stream and spring populations of W. podagrica from Western Europe (The Netherlands) was 8.4%. It is likely that Wettina lacustris sp. nov. is more widely distributed in the Palaearctic.


2001 ◽  
Vol 20 (1) ◽  
pp. 1-11 ◽  
Author(s):  
Hamid Slimani

Abstract. A palynological study of Campanian-Danian chalks from the quarries at Beutenaken and Hallembaye (Maastricht region) and from a borehole at Turnhout (northern Belgium) has revealed the presence of seven new species and subspecies of dinoflagellate cysts: Exochosphaeridium? Masureae sp. nov., Leberidocysta chlamydata subsp. schiolerii subsp. nov., Odontochitina streelii sp. nov., Pervosphaeridium septatum sp. nov., Spiniferites ramosus subsp. pterocoelus subsp. nov., Stephodinium? spinosum sp. nov. and Xenascus wetzelii sp. nov. Nexosispinum? complicatum described by Slimani (1996) as a new species is now a junior synonym of Pulchrasphaera minuscula Schiøler et al. (1997).


1996 ◽  
Vol 70 (3) ◽  
pp. 463-465 ◽  
Author(s):  
René H. B. Fraaye

A new species of Graptocarcinus is the stratigraphically youngest known member of the genus; it is here described together with a new species of the genus Caloxanthus from the late Maastrichtian of The Netherlands. The known stratigraphic distribution and paleobiogeography of both genera are discussed. The range of Graptocarcinus is extended from the Aptian to the late Maastrichtian.


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