Age: 343-337Ma
Viséan
Middle Mississippian Epoch
Carboniferous Period - Giant arthropods and amphibians, early reptiles, most plants fern or lycophyte-like, known for tropical forests and seas
Paleozoic Era - pre-Dinosaurs
Location: Hurst Green (Stonyhurst)
Hodder Place
Stonyhurst Bathing Hut remains by the riverbanks of the Hodder
Rock Type: Red Brook Mudstone Member within the Pendleside Limestone Formation.
Specimen: A tiny pygidium, roughly 1cm across, heavily worn so few identifying features may be seen. Family inferred by rock formation. The trilobate form of the trilobite is clear though, along with the shape of the fused yet still reconsigably inndividual segment within the pygidium.
Species:
Phillipsiidae belongs to the order Proetida, which was one of the last surviving trilobite orders, persisting through the Carboniferous and into the Permian period. Proetida is characterized by trilobites with relatively simple morphology compared to earlier, more elaborate forms. Trilobites of this order generally had well-developed, crescent-shaped eyes, a smooth to moderately ornamented exoskeleton, and thoracic segments that were often fewer in number. Proetida trilobites were highly adaptable, allowing them to survive in a range of marine environments, from shallow waters to deeper offshore areas. The order’s members were predominantly benthic, meaning they lived on or near the seafloor, scavenging or grazing on organic matter.
Within Proetida, the family Phillipsiidae is particularly notable for its survival into the Permian, the final period before trilobites went extinct. Phillipsiidae species had distinct features like smooth glabellae, large, crescent-shaped compound eyes, and moderately fused pygidia. The genera Phillipsia, Cummingella, Eocyphinium, and others within this family are typical examples, often small to medium in size, and generally found in shallow marine environments.
Phillipsiidae trilobites, along with other Proetida, are among the last remnants of trilobite evolution. While the earlier Cambrian and Ordovician trilobites often had more elaborate exoskeletons and complex ornamentation, the trilobites of the Carboniferous and Permian periods, such as those found in the Pendleside Limestone Formation, generally exhibit more conservative body plans. Their adaptability and relatively simple body structure may have contributed to their survival up until the mass extinction event at the end of the Permian, which saw the final disappearance of trilobites from the fossil record.
Trilobites are an extinct group of marine arthropods that first appeared during the early Cambrian period, approximately 521 million years ago, and thrived until their extinction at the end of the Permian period, around 252 million years ago. Over 22,000 species have been individually identified. Their name, "trilobite," comes from the three longitudinal lobes that run along their body—the central axial lobe and the two pleural lobes on either side.
Trilobites are placed within the phylum Arthropoda, which also includes modern insects, arachnids, and crustaceans. Their closest living relatives are believed to be the chelicerates, a group that includes horseshoe crabs, spiders, and scorpions. They could also be compared to modern isopods such as woodlice, in a form of convergent evolution.
Trilobites had a segmented body divided into three main parts longitudunally (in comparison to their three lobes laterally): the cephalon (head), the thorax (mid-body), and the pygidium (tail). The cephalon housed the mouthparts, antennae, and compound eyes, which were among the most advanced of their time. Some trilobite eyes were capable of sophisticated vision, with calcite lenses that allowed them to see well underwater. The thorax was composed of multiple articulated segments, allowing some trilobites to roll up as a defense mechanism, similar to modern pill woodlice. The pygidium was formed of fused segments appearing much like a stiffened extension of the thorax, but peresrving much more reliably, it varied in size and shape across different species and is an important feature for identifying trilobites in the fossil record.
Trilobites were incredibly diverse, both in form and ecology. Early trilobites were relatively simple in structure, but over time, they evolved a wide variety of adaptations. Some species developed spines, ridges, or ornamentation, which likely served as defense against predators or for burrowing. They ranged in size from just a few millimeters to over 70cm in length. They inhabited a variety of marine environments, from shallow coastal waters to deeper ocean floors. Most trilobites were benthic, living on or near the seafloor, where they scavenged for food or grazed on microbial mats.
Throughout their long evolutionary history, trilobites experienced significant changes in morphology and ecological roles. During the Cambrian period, trilobites were among the dominant marine organisms, diversifying rapidly in a period known as the Cambrian Explosion. By the Ordovician period, they had reached their peak in diversity, with a wide range of ecological niches and adaptations. However, trilobite diversity began to decline after the late Devonian mass extinction, and by the Permian period, only a few specialized groups remained. The end-Permian mass extinction, the largest extinction event in Earth's history, ultimately wiped out the last of the trilobites.
Trilobites are divided into several orders, with the most notable being Agnostida, Redlichiida, Phacopida, and Proetida. These orders are distinguished by differences in body morphology, particularly in the cephalon and pygidium. Agnostids, for example, were small, often blind trilobites with only two thoracic segments, while phacopids are known for their large, well-developed compound eyes and distinctively shaped pygidia.
