A reexamination of Yuknessia from the Cambrian of British Columbia and Utah

被引:31
作者
LoDuca, Steven T. [1 ]
Caron, Jean-Bernard [2 ,3 ,4 ]
Schiffbauer, James D. [5 ]
Xiao, Shuhai [6 ]
Kramer, Anthony [7 ]
机构
[1] Eastern Michigan Univ, Dept Geog & Geol, Ypsilanti, MI 48197 USA
[2] Royal Ontario Museum, Dept Nat Hist Palaeobiol, Toronto, ON M5S 2C6, Canada
[3] Univ Toronto, Dept Ecol & Evolutionary Biol, Toronto, ON M5S 3B2, Canada
[4] Univ Toronto, Dept Earth Sci, Toronto, ON M5S 3B1, Canada
[5] Univ Missouri, Dept Geol Sci, Columbia, MO 65211 USA
[6] Virginia Tech, Dept Geosci, Blacksburg, VA 24061 USA
[7] Univ Cincinnati, Dept Geol, Cincinnati, OH 45221 USA
基金
美国国家科学基金会; 加拿大自然科学与工程研究理事会;
关键词
PHYLLOPOD BED COMMUNITY; BURGESS SHALE; RHABDOPLEURID HEMICHORDATE; CLAY-MINERALS; FOSSILS; PRESERVATION; TAPHONOMY; BIOTA; FOSSILIZATION; GRAPTOLITE;
D O I
10.1017/jpa.2014.7
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
To investigate the phylogenetic affinity of Yuknessia simplex Walcott, 1919, scanning electron microscopy was applied to the Burgess Shale (Cambrian Series 3, Stage 5) type material and to new material from the Trilobite Beds (Yoho National Park) and specimens from the Cambrian of Utah. On the basis of fine-scale details observed using this approach, including banding structure interpreted as fusellae, Yuknessia Walcott, 1919 is transferred from the algae, where it resided for nearly a century, to the extant taxon Pterobranchia (Phylum Hemichordata). Considered as such, Yuknessia specimens from the Trilobite Beds and Spence Formation (Utah) are amongst the oldest known colonial pterobranchs. Two morphs regarded herein as two different species are recognized from the Trilobite Beds based on tubarium morphology. Yuknessia simplex has slender erect tubes whereas Yuknessia stephenensis n. sp., which is also known in Utah, has more robust erect tubes. The two paratypes of Y. simplex designated by Walcott (1919) are formally removed from Yuknessia and are reinterpreted respectively as an indeterminate alga and Dalyia racemata Walcott, 1919, a putative red alga.
引用
收藏
页码:82 / 95
页数:14
相关论文
共 52 条
[1]   Taphonomic study of Ediacaran organic-walled fossils confirms the importance of clay minerals and pyrite in Burgess Shale-type preservation [J].
Anderson, Evan P. ;
Schiffbauer, James D. ;
Xiao, Shuhai .
GEOLOGY, 2011, 39 (07) :643-646
[2]  
[Anonymous], 1967, NEW DATA BIOSTRATIGR
[3]  
BABCOCK LE, 2001, CAMBRIAN SYSTEM S CH, V13, P66
[4]  
Babcock Loren E., 2011, Memoir of the Association of Australasian Palaeontologists, V42, P137
[5]  
Bateson W., 1885, Q J MICROSC SCI, V25, P81, DOI [10.1098/rspl.1884.0058, DOI 10.1098/RSPL.1884.0058, DOI 10.1242/JCS.S2-25.S1.81]
[6]   RHABDOTUBUS, A MIDDLE CAMBRIAN RHABDOPLEURID HEMICHORDATE [J].
BENGTSON, S ;
URBANEK, A .
LETHAIA, 1986, 19 (04) :293-308
[7]   Fossil diagenesis in the burgess shale [J].
Butterfield, Nicholas J. ;
Balthasar, Uwe ;
Wilson, Lucy A. .
PALAEONTOLOGY, 2007, 50 :537-543
[8]   Preservational modes in the Ediacaran Gaojiashan Lagerstatte: Pyritization, aluminosilicification, and carbonaceous compression [J].
Cai, Yaoping ;
Schiffbauer, James D. ;
Hua, Hong ;
Xiao, Shuhai .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2012, 326 :109-117
[9]   Paleoecology of the Greater Phyllopod Bed community, Burgess Shale [J].
Caron, Jean-Bernard ;
Jackson, Donald A. .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2008, 258 (03) :222-256
[10]   Taphonomy of the Greater Phyllopod Bed community, Burgess Shale [J].
Caron, Jean-Bernard ;
Jackson, Donald A. .
PALAIOS, 2006, 21 (05) :451-465