Penny A M, Wood R A, Zhuravlev A Yu, Curtis A, Bowyer F, Tostevin R
School of GeoSciences, Grant Institute, University of Edinburgh, Edinburgh, UK.
Department of Biological Evolution, Faculty of Biology, Lomonosov Moscow State University, Moscow, Russia.
Geobiology. 2017 Jan;15(1):81-93. doi: 10.1111/gbi.12205. Epub 2016 Sep 28.
Namacalathus hermanastes is one of the oldest known skeletal metazoans, found in carbonate settings of the terminal Ediacaran (550-541 million years ago [Ma]). The palaeoecology of this widespread, goblet-shaped, benthic organism is poorly constrained yet critical for understanding the dynamics of the earliest metazoan communities. Analysis of in situ assemblages from the Nama Group, Namibia (548-541 Ma), shows that Namacalathus exhibited size variation in response to differing water depths, hydrodynamic conditions and substrate types. In low-energy, inner ramp environments, Namacalathus attains the largest average sizes but grew in transient, loosely aggregating, monospecific aggregations attached to microbial mats. In high-energy mid-ramp reefs, Namacalathus spatially segregated into different palaeoecological habitats with distinct size distributions. In outer ramp environments, individuals were small and formed patchy, dense, monospecific aggregations attached to thin microbial mats. Asexual budding is common in all settings. We infer that variations in size distribution in Namacalathus reflect differences in habitat heterogeneity and stability, including the longevity of mechanically stable substrates and oxic conditions. In the Nama Group, long-lived skeletal metazoan communities developed within topographically heterogeneous mid-ramp reefs, which provided diverse mechanically stable microbial substrates in persistently oxic waters, while inner and outer ramp communities were often ephemeral, developing during fleeting episodes of either oxia and/or substrate stability. We conclude that Namacalathus, which forms a component of these communities in the Nama Group, was a generalist that adapted to various palaeoecological habitats within a heterogeneous ecosystem landscape where favourable conditions persisted, and was also able to opportunistically colonise transiently hospitable environments. These early skeletal metazoans colonised previously unoccupied substrates in thrombolitic reefs and other microbial carbonate settings, and while they experienced relatively low levels of interspecific competition, they were nonetheless adapted to the diverse environments and highly dynamic redox conditions present in the terminal Ediacaran.
纳马卡拉图斯虫(Namacalathus hermanastes)是已知最古老的具骨骼后生动物之一,发现于埃迪卡拉纪末期(约5.5亿至5.41亿年前)的碳酸盐环境中。这种广泛分布的杯状底栖生物的古生态学研究尚不充分,但对于理解最早的后生动物群落动态至关重要。对纳米比亚纳马组(约5.48亿至5.41亿年前)原位组合的分析表明,纳马卡拉图斯虫会因水深、水动力条件和基质类型的不同而出现大小变化。在低能量的内缓坡环境中,纳马卡拉图斯虫平均体型最大,但生长在附着于微生物垫的短暂、松散聚集的单物种聚集体中。在高能量的中缓坡礁中,纳马卡拉图斯虫在空间上分隔成具有不同大小分布的不同古生态栖息地。在外缓坡环境中,个体较小,形成附着于薄微生物垫的斑块状、密集的单物种聚集体。无性出芽在所有环境中都很常见。我们推断,纳马卡拉图斯虫大小分布的变化反映了栖息地异质性和稳定性的差异,包括机械稳定基质的寿命和有氧条件。在纳马组中,长寿的具骨骼后生动物群落发育于地形异质的中缓坡礁内,这些礁在持续有氧的水域中提供了多样的机械稳定微生物基质,而内缓坡和外缓坡群落往往是短暂的,在短暂的有氧和/或基质稳定期发育。我们得出结论,纳马卡拉图斯虫作为纳马组这些群落的一个组成部分,是一种通才,能够适应异质生态系统景观中各种古生态栖息地,在有利条件持续存在的地方生存,并且还能够机会性地定殖于短暂适宜居住环境。这些早期具骨骼后生动物在凝块石礁和其他微生物碳酸盐环境中定殖于先前未被占据的基质上,虽然它们经历的种间竞争水平相对较低,但它们仍然适应了埃迪卡拉纪末期存在的多样环境和高度动态的氧化还原条件。