Bryozoans (also known as ectoprocts or moss animals) are aquatic, dominantly sessile, filter-feeding lophophorates that construct an organic or calcareous modular colonial (clonal) exoskeleton1,2,3. The presence of six major orders of bryozoans with advanced polymorphisms in lower Ordovician rocks strongly suggests a Cambrian origin for the largest and most diverse lophophorate phylum2,4,5,6,7,8. However, a lack of convincing bryozoan fossils from the Cambrian period has hampered resolution of the true origins and character assembly of the earliest members of the group. Here we interpret the millimetric, erect, bilaminate, secondarily phosphatized fossil Protomelission gatehousei9 from the early Cambrian of Australia and South China as a potential stem-group bryozoan. The monomorphic zooid capsules, modular construction, organic composition and simple linear budding growth geometry represent a mixture of organic Gymnolaemata and biomineralized Stenolaemata character traits, with phylogenetic analyses identifying P. gatehousei as a stem-group bryozoan. This aligns the origin of phylum Bryozoa with all other skeletonized phyla in Cambrian Age 3, pushing back its first occurrence by approximately 35 million years. It also reconciles the fossil record with molecular clock estimations of an early Cambrian origination and subsequent Ordovician radiation of Bryozoa following the acquisition of a carbonate skeleton10,11,12,13.
The Cambrian fossil record chronicles in exceptional detail the emergence of major bilaterian clades and continues to provide chronological constraints on the evolutionary diversification of disparate metazoans from a common ancestor12,13,14,15. Nearly all animal phyla, including soft-bodied Deuterostoma14, Entoprocta16, Phoronida17 and Priapulida12, made their first appearance during the Cambrian evolutionary radiation12,13,18. A key exception is the ‘missing’ colonial lophotrochozoan phylum Bryozoa, in which six of the eight recognized orders belonging to the classes Stenolaemata and Gymnolaemata appear abruptly with considerable diversity during the early Ordovician period6,7,19,20. Furthermore, there is a major time gap (approximately 44 million years) between the first fossil record of unequivocal bryozoans in the earliest Ordovician (Tremadocian)4,7 and the deeper origination in the early Cambrian (Terreneuvian) estimated using modern molecular clock analyses10,11,12,21.
Bryozoa is the most speciose of the lophophorate phyla firmly nested within Lophotrochozoa, characterized by iterated units (zooids) demonstrating hierarchical levels of modularity, and (apart from one genus) is the only exclusively colonial group of metazoans1,22,23,24. The key innovation of modularity initiated a novel pattern of colonial growth that led directly to a burst of morphological diversification and subsequent ecosystem proliferation, especially during the Great Ordovician Biodiversification Event1,18,25,26. Increased fossil sampling has gradually pushed back the oldest occurrence of bryozoans19,20, most recently into the early Tremadocian4, while the bryozoan affinity of the late Cambrian (Furongian) genus Pywackia remains highly debated2,4,7,18. Hence, a Cambrian origin for Bryozoa is not completely unpredicted and many authors have suggested a non-mineralized organic colony might explain the lack of a Cambrian record for the group3,4,5,6,7,19,20.
Here we describe rare but exquisitely preserved specimens of a millimetric modular fossil, Protomelission gatehousei9 from the early Cambrian of Australia and South China (Extended Data Fig. 1). Scanning electron microscopy (Figs. 1, 2, Extended Data Figs. 2, 3) and X-ray tomographic microscopy (Fig. 3, Extended Data Fig. 4) images reveal a combination of character traits that suggest a stem-group bryozoan affinity for P. gatehousei but distinguish the taxon from all extant and extinct clades. The interpretation of this secondarily phosphatized fossil from lower Cambrian rocks of South China and South Australia as a putative bryozoan indicates that modular bryozoans evolved synchronously with most other stem-group metazoans during the Cambrian evolutionary radiation12.
The finely phosphatized millimetric colony of P. gatehousei is bifoliate, compressed, lacks bifurcation, tapers apically and has an elliptical holdfast at the base (Figs. 1a–c, 2a–c, 3a), suggesting an erect, self-supported colony anchored to the substrate (Extended Data Fig. 2a, b). Colonies range from 1.8–2.2 mm in height, 0.1–0.2 mm in thickness and 1.0–1.5 mm in width, which is very similar to the width of Ordovician erect bifoliate cryptostomes27 (2.1 mm). The erect colony is composed of two layers of zooids (Figs. 1d–e, 2b, Extended Data Figs. 2c, 3c) arranged in simple linear series as back-to-back laminae23,27 (Fig. 3a, d–g, Extended Data Fig. 4, Supplementary Videos 1-6).
The zooids are sub-hexagonal in outline and flat box-shaped (Figs. 1f, h, 2d, Extended Data Fig. 3a–c). They are uniform in size, with an average width of 174 µm and length of 220 µm (Extended Data Table 1). There are up to 100 zooids in total in the bilaminate colony (Fig. 1a). Polymorphic differentiation of the zooids is absent, and there are no diaphragm-like structures in the zooids7 (Figs. 1–3, Extended Data Figs. 2–4). Zooids are inclined at about 25° to the median lamina (mesotheca) (Fig. 3f, Extended Data Fig. 4a) and form a quincuncial pattern on the surface of the colonies (Figs. 1f, 2d, f, 3b, Extended Data Fig. 3f), with 8–11 zooids within 2 mm longitudinally, and 7, 5 or 3 primary-order modular units of zooids arranged symmetrically on either side of the main median longitudinal axis (series-3) of the colony (Figs. 1a, 2a, 3b). The inflated frontal wall is thin and convex, imperforate, apically forming part of a hemispherical dome with a circular to ovoid opening in the best-preserved specimens (Fig. 1h, i, Extended Data Fig. 3a, b, f). Fine wrinkle structures developed on the frontal wall (Figs. 2g, Extended Data Fig. 2d, h) suggest an originally organic composition with labile and ductile properties, probably secreted by an underlying epithelium2 and replicated during early diagenetic phosphatization (Extended Data Figs. 2i, j, 3h, j, k, 5c–k). The ultrastructure of the basal and frontal walls consists of diagenetic irregular apatite (Fig. 2g, Extended Data Figs. 2i, 3k), reflecting the secondary phosphatization of the original organic zooid body wall (Extended Data Fig. 5c–k). Spherulitic microstructures (Extended Data Figs. 2j, 3j) are also present and may be associated with microbially mediated phosphate replacement or diagenetic processes28.
The developmental sequence of zooidal budding consists of five or seven alternating, back-to-back linear (longitudinal) series resulting in a palmate multiserial bilaminate colony (Figs. 3a–g, 4a). New zooids were budded at the distal tip of the colony, from pre-existing parents in an upward tapering growth vector (Figs. 1e, 3f, g, 4b, c). During clonal growth, the newly formed basal wall sequentially grew into contact with the walls of three adjacent zooids, entirely partitioning the original body (Fig. 3b, d, f, Extended Data Fig. 4a, f), demonstrating a zooidal budding process1,29 (Fig. 4c, d, Extended Data Fig. 4a). As the colony grew apically, longitudinal module series of zooids on either side (series-02 and series-04) of the main median series-3 axis stopped budding to provide accommodation space for adjacent linear series of zooids to grow (Figs. 1a, 4b, d). As a consequence, the whole colony achieved a distally tapering morphology (Figs. 1a, 2a, 4a, b, Extended Data Fig. 5a, b). The exhalant currents of filtered water would probably have been vented out from the sharp colony edges by analogy with living bryozoans with palmate branches1. Compared with central series zooids, the marginal series (series-1 and series-5) demonstrate a relatively slow growth of zooids, which probably resulted from high-level control on the relative growth rates across different parts of the colony1,29 (Figs. 1b, 4a, Extended Data Fig. 6a).
Protomelission gatehousei meets almost all recognition criteria expected in fossil bryozoans2 (Extended Data Fig. 6b, Extended Data Table 2). The general morphology, zooid arrangement, budding direction and pattern are comparable to members of the Stenolaemata, which have been suggested to have been derived from a soft-bodied ctenostome-grade ancestor during the Cambrian2,5,19,30. With an originally unmineralized body-plan, phosphatized preservation and box-shaped zooids, and in keeping with its basal phylogenetic position (Fig. 4e), P. gatehousei shares traits with taxa from a number of classes within Bryozoa, including the soft-bodied Gymnolaemata (Ctenostomata)19,20,30. On the basis of phylogenetic analyses, we conclude that P. gatehousei potentially represents a stem-group bryozoan (Fig. 4e, Extended Data Fig. 8, Supplementary Data 3, 4). Notably, the erect bilaminate body-plan of P. gatehousei provides the earliest example of a colony form that has been repeatedly modified with adaptive branching structure in younger Palaeozoic bryozoans2,7,19,22,23,27 (Extended Data Fig. 7). Although the last common ancestor of total-group Bryozoa remains enigmatic, the organic nature and basal phylogenetic position of Protomelission support the interpretation that crown-group Bryozoa most probably evolved from a colonial (rather than solitary) ancestor23,24,25 with skeletal biomineralization independently evolving at least twice across two major bryozoan clades in post-Cambrian times; the Stenolaemata during the Early Ordovician and the Gymnolaemata (Cheilostomata) in the Jurassic period2,5,6,19 (Fig. 4e).
The discovery of a stem bryozoan in the Cambrian narrows the origination gap that previously existed between the known fossil record and independent molecular clock estimates11,12,21. Our results push back the fossil record of the Bryozoa by approximately 35 million years and show that the colonial body-plan of Bryozoa can be traced back to the early Cambrian (Age 3), coincident with other major metazoan phyla belonging to the deuterostomes14, lophotrochozoans16,17,21 and ecdysozoans12,25. The miniaturized body-plan, much thinner, unmineralized cuticles (compared to arthropods and ‘worms’) and hard substrate habitat of early bryozoans such as P. gatehousei explain the poor fossil record and cryptic history of bryozoan stem taxa in the Cambrian11,14,28. However, the rapid diversification of the Bryozoa6,7,30 during the Ordovician probably coincides with calcite seas5, increasing hardground development and more robust biomineralization, leading to increased bryozoan colony size (centimetre to decimetre scale) and enhancing fossilization potential4,5,8,11,20. Thus, the recognized sequence of appearance for bryozoan taxa over geological time probably does not fully convey the real evolutionary history and may not provide a comprehensive understanding of bryozoan phylogeny2,7.
The early Cambrian is recognized as an important phosphatization window for microfossil preservation11,28 and the phosphatized stem bryozoan reported here reveals a previously hidden history for Bryozoa that provides a new framework for understanding the origin and phylogeny of the phylum2,7. The honeycomb-like network of zooids in P. gatehousei demonstrates that hierarchical architecture and complexity24,29 of colonial life was also an important evolutionary innovation during the Cambrian radiation of animal life.
Secondarily phosphatized specimens were recovered through standard acetic leaching of fossiliferous limestone samples, along with abundant benthic filter-feeding brachiopods31. Fossils were manually picked from acid residues using a binocular stereo microscope. Five incomplete specimens (Sample SADME 10470, 10470-1–10470-4) were collected from nodular, sandy limestones of the lower Wirrealpa Limestone (Cambrian Stage 4) at the Ten Mile Creek section, Bunkers Graben, South Australia9. One complete specimen of P. gatehousei (Sample ELI XYB 4 AN04) was collected from grey fossiliferous limestones in the Xihaoping Member of the Dengying Formation (Cambrian Stage 3), at the Xiaoyangba section, Hanzhong, South China. The geological and geographic setting has been previously described in detail31.
Scanning electron microscopy
Identified specimens were selected for the study using a Zeiss Supra 35 VP field emission at Uppsala University, Fei Quanta 450-FEGSEM at Northwest University and JEOL JSM 7100F-FESEM at Macquarie University. Coated specimens were further analysed with Backscattered electron imaging (BSE) in Quanta FEG 450 and JEOL JSM 7100F, with attached Energy Dispersive X-ray spectrometry (EDS) system, with 20.0 kV, 60 Pa and WD 11.4 mm at Northwest University and Macquarie University.
X-ray tomographic microscopy
Two specimens were scanned using an Xradia MicroXCT-400 system (Carl Zeiss XRM) with the source operating at 80 kV, 125 µA over 180° sample rotation (−92° to 92°) at The University of Sydney. Geometric and optical magnification settings were chosen to collect projections with xy-pixel dimensions of 2.0334 µm (Samples SADME 10470 and ELI XYB 4 AN02). The projections were reconstructed using XMReconstructor Version 7.0.2817 (Carl Zeiss XRM) to produce a series of 16-bit TIFF images with a slice spacing equivalent to the pixel xy dimensions (isotropic voxels) and voxel size of 2.03 µm. The X-ray tomographic microscopy (µCT) images were visualized and segmented via thresholding using ORS Dragonfly 324 version 2020.2 (software available at http://www.theobjects.com/dragonfly). Before feature extraction, images were applied with a normalization filter, unsharp mask and mean shift filter using the image processing function of Dragonfly. Morphological features of interest were coloured separately to assist in distinguishing them from one another. Three-dimensional videos are provided in Supplementary Videos 1–6.
Measurements of the length, width and angle of different parts of P. gatehousei were performed on µCT and SEM images by TpsDig2 v. 2.16. Scatter plots of different specimens, analysed by PAST v. 3, showing morphological variations, were also constructed. Raw data are provided in Supplementary Data 1, 2. Abbreviations used in the figures: B, basal wall; F, frontal wall; H, holdfast; M, mesotheca/median lamina; Z, zooid.
Fifty-two characters were coded for Protomelission, 18 bryozoan genera and 2 outgroup taxa (a total of 21 taxa). The phylogenetic data matrix was built in Microsoft Excel 2016. The 18 bryozoan genera are exemplars of the eight major bryozoan orders, and the fossil genera chosen all occur in the Ordovician (except for Fenestrapora, which is Devonian). The two outgroup taxa (Eoobolus and Phoronis) correspond to the two major non-bryozoan clades within the Lophophorata. Character codings were based on previously published data (Supplementary Data 3). All character codings are provided in Nexus format, along with a full list of the characters used, in Supplementary Data 3, 4.
Phylogenetic trees were inferred using both maximum parsimony and Bayesian methods. Parsimony analysis was performed using PAUP* (v. 4.0a169)32. A non-parametric bootstrap search based on 1,000 replicates was conducted using a heuristic search algorithm, with starting trees built using stepwise addition and branch swapping undertaken using tree bisection and reconnection (TBR). Results of this bootstrap analysis were summarized as a 50% majority rule consensus tree (Extended Data Fig. 8). Bayesian analyses were run using MrBayes (v.3.2.7)33 and the Mkv model34, with gamma-distributed rate variation and variable coding. The analysis used a sampling frequency of 1,000, two concurrent runs, four Metropolis-coupled chains, and was run for 10 million generations. A 25% relative burn-in was implemented for all summary statistics. The resulting phylogenetic tree is presented in Fig. 4e.
Further information on research design is available in the Nature Research Reporting Summary linked to this paper.
All data analysed in this study, including the phylogenetic datasets, are available in the Article, Extended Data Figs. 1–8, Extended Data Tables 1, 2 or Supplementary Information. Raw datasets are provided in the Dryad Digital Repository (https://doi.org/10.5061/dryad.rn8pk0pbd). CT scans and parameters used for scanning of specimens in this publication can be accessed in the MorphoSource Repository (https://doi.org/10.17602/M2/M379121 and https://doi.org/10.17602/M2/M379116) and the affiliated project (https://www.morphosource.org/projects/000378949?locale=en).
McKinney, F. K. & Jackson, J. B. C. Bryozoan Evolution (Univ. Chicago Press, 1989).
Taylor, P. D. & Waeschenbach, A. Phylogeny and diversification of bryozoans. Palaeontology 58, 585–599 (2015).
Schwaha, T. F., Ostrovsky, A. N. & Wanninger, A. Key novelties in the evolution of the aquatic colonial phylum Bryozoa: evidence from soft body morphology. Biol. Rev. 95, 696–729 (2020).
Ma, J., Taylor, P. D., Xia, F. & Zhan, R. The oldest known bryozoan: Prophyllodictya (Cryptostomata) from the lower Tremadocian (Lower Ordovician) of Liujiachang, south-western Hubei, central China. Palaeontology 58, 925–934 (2015).
Taylor, P. D., Lombardi, C. & Cocito, S. Biomineralization in bryozoans: present, past and future: bryozoan biomineralization. Biol. Rev. 90, 1118–1150 (2015).
Ernst, A. Diversity dynamics of Ordovician Bryozoa. Lethaia 51, 198–206 (2018).
Hageman, S. J. & Ernst, A. The last phylum: Occupation of Bryozoa morpho-ecospace (colony growth habits) during the early phase of the Great Ordovician Biodiversification Event. Palaeogeogr. Palaeoclimatol. Palaeoecol. 534, 109270 (2019).
Ernst, A., Bogolepova, O. K., Hubmann, B., Golubkova, E. Y. U. & Gubanov, A. P. Dianulites (Trepostomata, Bryozoa) from the Early Ordovician of Severnaya Zemlya, Arctic Russia. Geol. Mag. 151, 328–338 (2014).
Brock, G. A. & Cooper, B. J. Shelly fossils from the early Cambrian (Toyonian) Wirrealpa, Aroona Creek, and Ramsay Limestones of South Australia. J. Paleontol. 67, 758–787 (1993).
Erwin, D. H. et al. The Cambrian conundrum: early divergence and later ecological success in the early history of animals. Science 334, 1091–1097 (2011).
Wray, G. A. Molecular clocks and the early evolution of metazoan nervous systems. Philos. Trans. R. 370, 20150046–20150046 (2015).
Erwin, D. H. The origin of animal body plans: a view from fossil evidence and the regulatory genome. Development 147, dev182899 (2020).
Zhang, X. & Shu, D. Current understanding on the Cambrian Explosion: questions and answers. PalZ https://doi.org/10.1007/s12542-021-00568-5 (2021).
Han, J., Morris, S. C., Ou, Q., Shu, D. & Huang, H. Meiofaunal deuterostomes from the basal Cambrian of Shaanxi (China). Nature 542, 228–231 (2017).
Wood, R. et al. Integrated records of environmental change and evolution challenge the Cambrian Explosion. Nat. Ecol. Evol. 3, 528–538 (2019).
Zhang, Z. et al. A sclerite-bearing stem group entoproct from the early Cambrian and its implications. Sci. Rep. 3, 1066 (2013).
Hou, X. et al. The Cambrian fossils of Chengjiang, China: The Flowering of Early Animal Life (John Wiley & Sons, 2017).
Landing, E. et al. Early evolution of colonial animals (Ediacaran Evolutionary Radiation–Cambrian Evolutionary Radiation–Great Ordovician Biodiversification Interval). Earth Sci. Rev. 178, 105–135 (2018).
Ernst, A. in Fossil Record and Evolution of Bryozoa (eds Helmcke, J.-G., Starck, D. & Wermuth, H.) 11–56 (De Gruyter, 2020).
Taylor, P. D. Bryozoan Paleobiology (John Wiley & Sons, 2020).
Budd, G. E. & Jackson, I. S. C. Ecological innovations in the Cambrian and the origins of the crown group phyla. Philos. Trans. R. Soc. B 371, 20150287 (2016).
Mackie, G. O. From aggregates to integrates: physiological aspects of modularity in colonial animals. Philos. Trans. R. Soc. B 313, 175–196 (1986).
Hughes, R. N. Lessons in modularity: the evolutionary ecology of colonial invertebrates. Sci. Mar. 69, 169–179 (2005).
Lidgard, S., Carter, M. C., Dick, M. H., Gordon, D. P. & Ostrovsky, A. N. Division of labor and recurrent evolution of polymorphisms in a group of colonial animals. Evol. Ecol. 26, 233–257 (2012).
Carroll, S. B. Chance and necessity: the evolution of morphological complexity and diversity. Nature 409, 1102–1109 (2001).
Lombardi, C., Cocito, S., Gambi, M. C. & Taylor, P. D. Morphological plasticity in a calcifying modular organism: evidence from an in situ transplant experiment in a natural CO2 vent system. R. Soc. Open Sci. 2, 140413 (2015).
McKinney, F. K. Historical record of erect bryozoan growth forms. Proc. R. Soc. Lond. B 228, 133–149 (1986).
Schiffbauer, J. D., Wallace, A. F., Broce, J. & Xiao, S. Exceptional fossil conservation through phosphatization. Paleontol. Soc. Pap. 20, 59–82 (2014).
Lidgard, S. Zooid and colony growth in encrusting cheilostome bryozoans. Palaeontology 28, 255–291 (1985).
Todd, J. A. The central role of ctenostomes in bryozoan phylogeny. In Proc. 11th Int. Bryozool. Assoc. Conf. 104, 104–135 (2000).
Zhang, Z. L. et al. The oldest Cambrian trilobite—brachiopod association in South China. Gondwana Res. 89, 147–167 (2021).
Swofford, D. L. Phylogenetic Analysis Using Parsimony (*and Other Methods) (Sinauer Associates, 2003).
Ronquist, F. & Huelsenbeck, J. P. MrBayes 3: Bayesian phylogenetic inference under mixed models. Bioinformatics 19, 1572–1574 (2003).
Lewis, P. O. A likelihood approach to estimating phylogeny from discrete morphological character data. Syst. Biol. 50, 913–925 (2001).
Torsvik, T. H. & Cocks, L. R. M. New global palaeogeographical reconstructions for the Early Palaeozoic and their generation. Geological Society, London, Memoirs 38, 5–24 (2013).
Betts, M. J. et al. Early Cambrian chronostratigraphy and geochronology of South Australia. Earth Sci. Rev. 185, 498–543 (2018).
Taylor, P. D. & Jenkins, H. L. Evolution of larval size in cyclostome bryozoans. Hist. Biol. 30, 535–545 (2018).
Xia, F. S., Zhang, S. G. & Wang, Z. Z. The oldest bryozoans: new evidence from the Late Tremadocian (Early Ordovician) of east Yangtze gorges in China. J. Paleontol. 81, 1308–1326 (2007).
Koromyslova, A. V., Martha, S. O. & Pakhnevich, A. V. The internal morphology of Acoscinopleura Voigt, 1956 (Cheilostomata, Bryozoa) from the Campanian–Maastrichtian of Central and Eastern Europe. PalZ 92, 241–266 (2018).
Pushkin, V. I. & Popov, L. E. Early Ordovician bryozoans from north-western Russia. Palaeontology 42, 171–189 (1999).
Porter, J. S. Morphological and genetic characteristics of erect subtidal species of Alcyonidium (Ctenostomata: Bryozoa). J. Mar. Biol. Assoc. UK 84, 243–252 (2004).
This study was supported by a Macquarie University Research Fellowship (2019 MQRF), National Natural Science Foundation of China (41720104002, 41621003, 41890844 and 41772010), Strategic Priority Research Program of Chinese Academy of Sciences (XDB26000000), Ministry of Science and 111 project of Ministry of Education of China (D17013), Thousand Talents Program and 1000 Talent Shaanxi Province Fellowship. We thank Cambridge University Press for permission to illustrate P. gatehousei in Fig. 1a, f, reproduced from ref. 9, with permission from Cambridge University Press. The palaeogeographic map in Extended Data Fig. 1 is reproduced from ref. 35 with permission from Geological Society Publishing House and Extended Data Fig. 1b is reproduced from ref. 31 with permission from Elsevier Science & Technology Journals. We thank L. E. Holmer and M. Streng at Uppsala University, Y. L. Pang at Northwest University, and S. Lindsay and C. Shen at the Microscopy Unit of Macquarie University for assistance with SEM imaging, M. Foley at University of Sydney for technical assistance with µCT imaging, X. Liu for reconstruction, Q. C. Feng for sample preparation, and J. Alroy, C. Simpson and M. Steinthorsdottir for discussion.
The authors declare no competing interests.
Peer review information Nature thanks Andrej Ernst, Juan López-Gappa and Mark Wilson for their contribution to the peer review of this work. Peer reviewer reports are available.
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Extended data figures and tables
Extended Data Fig. 2 Protomelission gatehousei from the early Cambrian Xihaoping Member of Dengying Formation, South China, ELI XYB 4 AN02.
a, Oblique lateral view of the colony; note five series of zooids. b, Oblique basal view showing the elliptical holdfast. c, Oblique view of the opposite colony surface. d, BSE imaging demonstrates distinct wrinkles along the zooid edges. e, BSE imaging, arrows demonstrate the space between adjacent zooids, box corners indicate the spherulitic microstructures shown in figure j. f, Close-up of holdfast with tailed arrows showing attached small grains. g, Enlargement of weakly phosphatized colony apex; note basal walls of three adjacent zooids indicated by tailed arrows and median mesotheca by an arrow. h, Detail of wrinkles of frontal wall. i, Enlarged diagenetic apatite of figure h. j, Enlargement of spherulitic microstructures between adjacent zooids.
Extended Data Fig. 3 Protomelission gatehousei from the early Cambrian Wirrealpa Limestone, South Australia.
a–c and j-k, SADME 10470-2. a, Front side of a broken colony, highlighting five series of zooids, upper box corners indicate the area shown in figure c, lower box corners show the microstructures in figure j. b, Oblique lateral view, with relatively well preserved frontal walls and circular orifice of zooids. c, Lateral view showing the staggered pattern of zooids in both layers of bifoliate colony; note basal walls and largely broken frontal wall (tailed arrow), and basal walls from opposite layer (arrows). d, SADME 10470-3, back view of one colonial layer with the exfoliated opposite layer, showing three broken zooids from the opposite layer (arrows) and space between adjacent zooids (tailed arrows). e-i, Holotype, SADME 10470. e, Oblique lateral view with arrows showing the median mesotheca between two layers. f, Quincuncial arrangement of box-shaped zooids, showing dome shaped frontal wall (arrow). g, Detail of spoon-shaped structure at the zooid proximal end, indicated by a tailed arrow. h, Recrystallized granules and fibres of frontal wall. i, Lateral view showing one frontal wall (arrow) and two basal walls of the same layers, and the phosphatized median mesotheca (tailed arrow). j, Spherulitic microstructures of frontal wall. k, Enlarged diagenetic apatite of basal wall. B, basal wall.
Extended Data Fig. 4 µCT images of Protomelission gatehousei from the early Cambrian of South Australia and South China.
a-f, SADME 10470. a, Longitudinal section, showing bifoliate pattern of zooids on the back-to-back layers; note the space between the frontal wall of parent and daughter zooids by arrows. b–c, Tangential section. b, Median mesotheca and curved basal walls by tailed arrows. c, Frontal walls of Series-3, demonstrating the concave centre of the back/opposite layer. d, Longitudinal section shows detail of probable colonial connection between adjacent zooids from back-to-back layers (tailed arrows) through space of median mesotheca. e–f, Transverse section showing zooids on bilaminate layers along mesotheca. e, New budding zooids indicated by arrows, and daughter basal wall overlapping parent frontal wall indicated by a tailed arrow. f, Basal walls of new budding zooids indicated by arrows. g, ELI XYB 4 AN02, transverse section showing zooids on both layers and median mesotheca of the colony. Blue, frontal wall; Green, mesotheca with secondary phosphatic cement in yellow; Red, basal wall. M, mesotheca; Z, zooid.
Extended Data Fig. 5 Relationship between colony growth and colony surface area, and elemental mapping of the zooids of Protomelission gatehousei.
a, Plots of increasing colony surface area and colony generations (1–8). b, Plots of total colony surface area and colony height, indicating a uniform increase of the colonial surface area during development. c–k, EDS elemental mapping, SADME 10470. c, SEM image. d, Elemental map of C. e, Elemental map of O. f, Elemental map of Al. g, Elemental map of Si. h, Elemental map of P. i, Elemental map of S. j, Elemental map of Ca. k, Elemental map of P, Ca and Si concentrations, noting the clastic particles adhered to the space between adjacent zooids.
Each pair of width (greatest width perpendicular to the proximal-distal axis of the zooid) and length (proximal-distal axis of the zooid) values correspond to a single zooid. a, Boxplots of zooid width for five adjacent series (different colours) from two P. gatehousei colonies from South Australia and South China, with the mean value for each series indicated by the ×. The colour of each series matches the colours used in Fig. 4d. Values for boxplots are provided in Supplementary Data 1. N = 49 biologically independent measurements of zooid size. b, Zooid length and width of different bryozoan taxa (different colours) from the literature with the geological age of each taxon indicated in the key. Raw data for scatter plots are provided in Supplementary Data 2. N = 172 biologically independent measurements of zooid size (86 zooids). Note that for Ordovician taxa, the size range is comparable to Protomelission. Red = Protomelission gatehousei (circle, SADME 10470; solid circle, ELI XYB 4 AN02); Yellow = Cyclostomata; Green = Trepostomata; Blue = Cryptostomata; Purple = Cheilostomata; Pink = Ctenostomata4,5,26,37,38,39,40,41. Є, Cambrian, O: Ordovician; J, Jurassic; K, Cretaceous, R: Recent.
Extended Data Fig. 7 Erect bifoliate bryozoan Stictopora sp. from the Late Ordovician Bowen Park Group, New South Wales, Australia.
a–d, Bowen-DQ-01. a, Front side of the colony, noting the five series of zooids and arc-shaped holdfast. b, Oblique basal view. c, Lateral view showing zooids on both layers by arrows, and arc-shaped holdfast. d, Enlarged holdfast, note the relatively smooth surface as an adaptation to a hard substrate. e–f, Bowen-DQ-02. e, Front side of a larger colony showing five series of zooids and new budding series at the apex indicated by tailed arrows. Box corners indicate the area in figure f. f, Enlargement of five series of zooids.
Extended Data Fig. 8 Phylogenetic tree inferred using parsimony based on a matrix of 21 taxa and 52 characters.
Fifty-percent majority rule bootstrap consensus tree generated using a heuristic search algorithm by PAUP*. Node values are bootstrap probabilities. Coloured areas indicate the three taxonomic classes that comprise the Bryozoa, along with the position of P. gatehousei and outgroups (see Supplementary Data 3-4 for details). Purple = outgroups; Yellow = Protomelission; Blue = Phylactolaemata; Red = Gymnolaemata; Green = Stenolaemata.
This file contains Supplementary Data 1–4. (1) Derived values for box plots of Protomelission gatehousei zooid width provided in Extended Fig. 6a. (2) Raw data of zooid width and length of 13 bryozoan taxa in Extended Fig. 6b. (3) Character trait dataset and morphological states for bryozoans. (4) Character taxon matrix in NEXUS format.
3D video of P. gatehousei SADME 10470 (full). This 59-second-3D video reveals the morphology of the external zooid arrangement, along with the transverse, tangential and longitudinal virtual dissection of the internal morphology of the colony of P. gatehousei (Specimen: SADME 10470). False colours are used to differentiate important character traits. Blue, frontal wall; Green, mesotheca with secondary phosphatic cement in yellow; Red, basal wall.
3D video of P. gatehousei SADME 10470 (longitudinal section). This 13-second-3D video reveals the longitudinal virtual dissection of the internal morphology of the colony of P. gatehousei (Specimen: SADME 10470). False colours are used to differentiate important character traits. Blue, frontal wall; Green, mesotheca with secondary phosphatic cement in yellow; Red, basal wall.
3D video of P. gatehousei SADME 10470 (tangential section). This 6-second-3D video reveals the tangential virtual dissection of the internal morphology of the colony of P. gatehousei (Specimen: SADME 10470). False colours are used to differentiate important character traits. Blue, frontal wall; Green, mesotheca with secondary phosphatic cement in yellow; Red, basal wall.
3D video of P. gatehousei SADME 10470 (transverse section). This 24-second-3D video reveals the transverse virtual dissection of the internal morphology of the colony of P. gatehousei (Specimen: SADME 10470). False colours are used to differentiate important character traits. Blue, frontal wall; Green, mesotheca with secondary phosphatic cement in yellow; Red, basal wall.
3D video of P. gatehousei SADME 10470. This 25-second-3D video reveals the external zooid arrangement and morphology of the colony of P. gatehousei (Specimen: SADME 10470).
3D video of P. gatehousei EIL XYB 4 AN02. This 22-second-3D video reveals the external zooid arrangement and morphology of the colony of P. gatehousei (Specimen: ELI XYB 4 AN02).
About this article
Cite this article
Zhang, Z., Zhang, Z., Ma, J. et al. Fossil evidence unveils an early Cambrian origin for Bryozoa. Nature 599, 251–255 (2021). https://doi.org/10.1038/s41586-021-04033-w