Search bioRxiv⌕ Search

bioRxiv · 10.1101/2025.01.24.634792

Decoding Demosponge Diversity: Bayesian Analysis of Biodiversity, Extinction Events and Environmental Influences throughout the Phanerozoic

Abstract

Sponges (phylum Porifera) have been essential to marine ecosystems for over 600 million years, contributing to nutrient cycling, reef building, and ecological stability. Despite their evolutionary importance, the drivers of their diversity dynamics remain poorly understood. This study investigates the diversification patterns of Demospongiae, the largest class of sponges with a well-documented fossil record throughout the Phanerozoic Eon (541-0 Ma). Using fossil occurrence data and a Bayesian framework, we modeled origination and extinction rates to understand their evolutionary history. Our findings reveal key extinction events, including three previously unrecognized events in the Cambrian, Late Silurian, and Late Jurassic, alongside known events such as the Permian-Triassic and Triassic-Jurassic extinctions. Notably, there was no statistical evidence for mass extinction during the Late Ordovician or Late Devonian. Additionally, Demosponges underwent a significant decline prior to the Cretaceous-Paleogene extinction. To explore abiotic influences, we applied the Multivariate Birth-Death (MBD) model across all extinction events. This analysis identified correlations between major speciation and extinction events and key variables, including temperature, continental fragmentation, oxygen levels, and sea level, as well as geochemical proxies such as sulfur and strontium, which may reflect underlying drivers like anoxia, weathering, or tectonic activity. Temperature and oxygen levels, in particular, correlated with speciation and extinction during the Permian-Triassic extinction. These findings underscore the role of environmental fluctuations in shaping demosponge diversity and highlight the complex interplay between changes in abiotic factors and sponge evolution. Our work provides critical insights into the factors driving sponge biodiversity and offers perspectives on how modern sponges might respond to ongoing climate change. Significance StatementSponges are ancient and ecologically pivotal marine organisms that have persisted through Earths major environmental upheavals. Despite their resilience, the mechanisms driving their evolutionary responses to past climate shifts remain unclear. By leveraging the fossil record of Demospongiae, this study identifies previously unrecognized extinction events and elucidates how abiotic factors, including temperature and oxygen levels, shaped their diversity during these crises. These findings enhance our understanding of sponge evolutionary dynamics and resilience, offering critical insights into the vulnerability of marine ecosystems under current and future climate change scenarios.

Explore related subjects

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

Schuster, A., Canfield, D. E.. 2025-01-27. Decoding Demosponge Diversity: Bayesian Analysis of Biodiversity, Extinction Events and Environmental Influences throughout the Phanerozoic. https://doi.org/10.1101/2025.01.24.634792

Cite the original work for its findings. Save a collection to share your selection of sources.

KEEP EXPLORING

Related preprints

Constraining Palaeogeography and Palaeotides for the Cambrian using cnidarian medusae

The ocean tides influence key Earth system processes at a range of spatial and temporal scales. It is known that the geometry of ocean basins is the leading controller of tidal energetics, so well-constrained palaeogeographic reconstructions and tidal properties for Earths past are imperative when investigating other Earth system processes. Here, we present a novel way to constrain both deep-time tidal model results and reconstructions, by combining palaeoecology with sedimentology. We compare new palaeo-tidal model simulations for the Cambrian period, significant for the early origin and radiation of major animal fauna, to tidal proxies. One of the most abundant soft-bodied organisms preserved during this time are cnidarian medusae (jellyfish). A total of 17 cnidarian medusae localities were obtained through the literature, which had an adequate global distribution and occurred at regular intervals throughout the period of study. In some locations there were also estimates of palaeo-tidal range. Our results show a good agreement between the simulations and proxy data. In the few locations where there is disagreement, it is proposed that the palaeogeographic reconstructions are missing details, e.g., island chains, and our results allow for the palaeogeographic reconstructions to be improved. The proxy method presented is promising and can be applied to other time-periods with different marine fossils, particularly at evolutionary and extinction periods where the marginal marine environment is of importance.

paleontology↗

Denisovan leg bones from Taiwan reveal large body size

Denisovans are an extinct archaic Homo group whose lineage diverged from the Neanderthal lineage approximately 550,000 years ago and were widely distributed across eastern Asia until [~]45,000 years ago1-7. Their morphological features are known directly from the existing cranio- dental and phalangeal remains1,2,8-12. However, the body size and postcranial morphology of the Denisovans remain largely unknown. We here report that hominin femoral and tibial fossils recovered from the Penghu Channel, Taiwan, are Denisovans in their proteomic profiles. Morphologically, these specimens are among the largest leg bones known in Pleistocene Homo. They exhibit generally archaic features, but also show some modern human-like morphology, including a strong femoral pilaster. Our findings demonstrate that the Denisovan population at the northern circle had larger body size than earlier Homo erectus as well as Late Pleistocene Homo sapiens in eastern Asia. This challenges the generally held expectation that Pleistocene Homo followed Bergmanns rule that anticipates latitudinal decline of body size, and suggests that the large Denisovan brain resulted from their large body size at least partly. The strong pilaster developed in the Penghu femur suggests some behavioral similarities between the Denisovans and the Upper Palaeolithic modern humans and/or gene flow from the latter to the former.

paleontology↗

Habitat and feeding ecology of a Denisovan from Late Pleistocene Taiwan

Denisovans, originally identified from ancient genome from Denisova Cave in Altai, were a sister group to the Neanderthals and were once widely distributed across diverse terrains in the north and south of eastern Asia1-5. Genomic studies suggest that there were multiple events of interbreeding between modern humans (Homo sapiens) and Denisovans somewhere in Asia6. However, little is known about Denisovan living environments, diet, ecological niche, the timing of their disappearance, and the possible coexistence with modern humans in different regions. Here we report the radiocarbon age and stable isotopic signature of Penghu 3, a large Denisovan tibia from Penghu Channel, Taiwan7. The results showed that Penghu 3 dates to approximately 45,000 years ago, the time when modern humans were already widespread in southern parts of Asia. This Denisovan individual inhabited a C4-dominated ecosystem, open environments such as savannahs and floodplains, or a mixture of both, and consumed a high proportion of animal protein similar to some European Neanderthals8-10, with no clear evidence for the use of aquatic resources. These findings have implications for the behavioral flexibility, large body size7, and eventual disappearance of the Denisovans.

paleontology↗