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Microcharacterisation involving optical microscopy, combined scanning electron microscopy and energy dispersive spectroscopy (SEM\u2010EDS) and nanoscale secondary ion mass spectroscopy (NanoSIMS), was undertaken to identify microbial textures and relics in stromatolite samples. Microbial textures identified are micritic streaky and micropeloidal (grumous) microstructures as well as microcolumns, micritic threads and micritised tubular outlines resembling the\n                    <jats:italic>Girvanella<\/jats:italic>\n                    calcimicrobe. Within these microbial textures, multiple biotic components are discerned, including intact and flattened tubular bacterial sheaths, smooth and nanogranular non\u2010crystalline extracellular polymeric substances (EPS), filamentous and spherical bacteriomorphs, as well as coccobacilli\u2010like moulds. The biotic\u2010mineralogical interface is characterised by microcrystalline rhombic dolomite, nano\u2010sized pyrite spheroids and nano\u2010sized flaky silicates in direct contact with biotic components. Interpreted as a mixed community of filamentous and coccoidal (cyano)bacteria, these microbes were important contributors to reef building. Preservation of microfossils was likely facilitated by synsedimentary silicification of EPS and bacterial sheaths. Microbial metabolic processes lowered kinetic barriers for authigenic precipitation of clay minerals on bacterial surfaces serving as nucleation sites. These synsedimentary clays strengthened initially soft microfabrics and potentially helped establish chemical conditions that promoted early diagenetic precipitation of protodolomite. The findings of this study show that carbonates may intricately preserve microfossils where associated with synsedimentary authigenic clays and microcrystalline dolomite. These results contribute to a deeper understanding of the formation and growth of microbial reefs during the Cryogenian interglacial period.\n                  <\/jats:p>","DOI":"10.1111\/gbi.70059","type":"journal-article","created":{"date-parts":[[2026,8,29]],"date-time":"2026-08-29T18:20:25Z","timestamp":1788027625000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":0,"title":["Dolomitic Microfossil Preservation in a Cryogenian Microbial Reef, Arkaroola (South Australia)"],"prefix":"10.1111","volume":"24","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-0479-4800","authenticated-orcid":false,"given":"France","family":"Champenois","sequence":"first","affiliation":[{"name":"School of Earth and Oceans The University of Western Australia  Perth Western Australia Australia"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-2085-4989","authenticated-orcid":false,"given":"Maree L.","family":"Corkeron","sequence":"additional","affiliation":[{"name":"School of Earth and Oceans The University of Western Australia  Perth Western Australia Australia"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-9987-6592","authenticated-orcid":false,"given":"Annette D.","family":"George","sequence":"additional","affiliation":[{"name":"School of Earth and Oceans The University of Western Australia  Perth Western Australia Australia"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"311","published-online":{"date-parts":[[2026,8,29]]},"reference":[{"key":"e_1_2_10_2_1","doi-asserted-by":"publisher","DOI":"10.2307\/3514563"},{"key":"e_1_2_10_3_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.marchem.2019.103693"},{"key":"e_1_2_10_4_1","doi-asserted-by":"publisher","DOI":"10.1346\/CCMN.2009.0570207"},{"key":"e_1_2_10_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.apgeochem.2026.106917"},{"key":"e_1_2_10_6_1","doi-asserted-by":"publisher","DOI":"10.1126\/science.1057204"},{"key":"e_1_2_10_7_1","doi-asserted-by":"publisher","DOI":"10.1306\/071002730105"},{"key":"e_1_2_10_8_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0037-0738(99)00038-X"},{"key":"e_1_2_10_9_1","doi-asserted-by":"publisher","DOI":"10.1038\/s41467-022-29223-6"},{"key":"e_1_2_10_10_1","doi-asserted-by":"publisher","DOI":"10.1180\/clm.2024.27"},{"key":"e_1_2_10_11_1","doi-asserted-by":"publisher","DOI":"10.2307\/3515192"},{"key":"e_1_2_10_12_1","doi-asserted-by":"publisher","DOI":"10.2110\/pec.00.67.0059"},{"key":"e_1_2_10_13_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0016-7037(03)00488-5"},{"key":"e_1_2_10_14_1","doi-asserted-by":"publisher","DOI":"10.1111\/j.1365-3091.2009.01121.x"},{"key":"e_1_2_10_15_1","doi-asserted-by":"publisher","DOI":"10.2110\/jsr.2005.015"},{"key":"e_1_2_10_16_1","doi-asserted-by":"publisher","DOI":"10.1306\/111302730485"},{"issue":"5","key":"e_1_2_10_17_1","first-page":"443","article-title":"Stevensite in the Microbialites of Clifton South Lagoon, Western Australia: Evidence of the Low\u2010Temperature Formation of Hydrous Magnesium Silicate","volume":"12","author":"Burne R. 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