Archaeichnium haughtoni: a robust burrow lining from the Ediacaran-Cambrian transition of Namibia

被引:1
|
作者
Turk, Katherine A. [1 ,2 ]
Pulsipher, Mikaela A. [3 ,4 ]
Bergh, Eugene [5 ]
Laflamme, Marc [6 ]
Darroch, Simon A. F. [1 ,2 ,7 ]
机构
[1] Vanderbilt Univ, Dept Earth & Environm Sci, Nashville, TN 37235 USA
[2] Vanderbilt Univ, Evolutionary Studies Inst, Nashville, TN 37232 USA
[3] Univ Missouri, Dept Geol Sci, Columbia, MO USA
[4] Natl Pk Serv, Grand Canyon Natl Pk, Flagstaff, AZ USA
[5] North West Univ, Dept Geol, Unit Environm Sci & Management, Potchefstroom, South Africa
[6] Univ Toronto Mississauga, Dept Chem & Phys Sci, Mississauga, ON, Canada
[7] Museum Nat Hist, D-60325 Frankfurt, Germany
基金
加拿大自然科学与工程研究理事会;
关键词
ecosystem engineering; Ediacaran-Cambrian transition; Nama Group; ichnology; TRACE FOSSILS; NAMA GROUP; SHELLY FOSSILS; BOUNDARY; STRATIGRAPHY; WORMS; SEDIMENT; NITRIFICATION; BIOTURBATION; EMPHASIS;
D O I
10.1002/spp2.1546
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Following various assignments to Archaeocyatha, worm tubes, and finally incertae sedis, the enigmatic Ediacaran-Cambrian taxon Archaeichnium haughtoni has in recent years come to represent somewhat of a wastebasket taxon to which the indeterminate tapering tubular forms common across this interval are assigned. This 'catch-all' status has been aided in part by both suboptimal specimen photography and the temporary loss of the holotype after its second redescription in 1978. Recent rediscovery of the A. haughtoni holotype in the collections of the Iziko South African Museum in Cape Town has enabled a much-needed re-assessment of this critical and cryptic taxon, with results suggesting that this material from the latest Ediacaran or earliest Cambrian of Namibia is among the earliest fossil record examples of marine worm burrow linings, and the oldest examples of linings robust enough to withstand exhumation and current transport. These traces indicate the emergence of this important animalian ecosystem engineering behaviour closer to the Ediacaran-Cambrian boundary than previously thought.
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页数:17
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