首页   按字顺浏览 期刊浏览 卷期浏览 Systematics and phylogenetic implications of the haplosclerid stromatoporoidNewellia mi...
Systematics and phylogenetic implications of the haplosclerid stromatoporoidNewellia miranov. gen.

 

作者: RACHEL WOOD,   JOACHIM REITNER,   RONALD R. WEST,  

 

期刊: Lethaia  (WILEY Available online 1989)
卷期: Volume 22, issue 1  

页码: 85-93

 

ISSN:0024-1164

 

年代: 1989

 

DOI:10.1111/j.1502-3931.1989.tb01171.x

 

出版商: Blackwell Publishing Ltd

 

数据来源: WILEY

 

摘要:

Wood, Rachel, Reitner, Joachim&West, Ronald R. 1989 01 15: Systematics and phylogenetic implications of the haploslerid stromatoporoidNewellia miranov. gen.Lethaia, Vol. 22, pp. 85–93. Oslo. ISSN 0024–1164.The presence of spicules in a Palaeozoic stromatoporoid is here confirmed.Parallelopora miraNewell, 1935 from the Upper Carboniferous of the U.S.A. is redescribed as a calcified haplosclerid sponge with a primary siliceous spicule framework of isodictyally arranged styles, sub‐tylostyles and strongyles and a secondary calcareous skeleton of stromatoporoid grade and probable aragonitic original mineralogy.P. mirais placed within a new genusNewellia, and family, the Newellidae. This form is postulated to have possessed large amounts of collagenous organic material which enveloped and bound the spicular framework in place. By the draping outline of the calcareous skeleton around the spicule framework and by analogy with the Recent demosponge genusVaceletia, the calcareous skeleton is suggested to have formed by the direct mineralization of this collagenous template.Newellia miranov. gen. is further proposed to constitute a member of a new clack of haplosclerid stromatoporoids, together withEuz‐Miella erenoensis(Lower Cretaceous); a clade with some similarity to Recent non‐calcified forms, e.g.Adocia. Most notably, the presence of different calcareous skeleton mineralogies and possibly microstructures in these two forms suggests the independent development of a calcareous skeleton at different times within this spicule clade. Demosponges appear to have produced calcareous skeletons independently in many different spicule clades. Calcified demosponges are now known from the Hadro‐merida (Lower carboniferous; Upper Cretaceous ‐ Recent), Axinellida (Upper Triassic ‐ Lower Cretaceous; Upper Cretaceous; Recent), Poecilosclerida (Recent) as well as the Haplosclerida (Upper Carboniferous ‐ Lower Cretaceous; Recent).□Upper Carboniferous, stromatoporoid, spicules, haplosclerid demosponges, calcareous skeleton biomineralization, demospong

 

点击下载:  PDF (2453KB)



返 回