<bib>
<comment>
This file was created by the TYPO3 extension publications
--- Timezone: CEST
Creation date: 2026-04-23
Creation time: 09:51:00
--- Number of references
7
</comment>
<reference>
<bibtype>article</bibtype>
<citeid>FAN2026105284</citeid>
<title>Carbonate-associated phosphate evidence for a small inorganic phosphorus reservoir in the terminal Ediacaran ocean</title>
<abstract>The terminal Ediacaran (ca. 551–533 Ma) was characterized by profound biological innovations and environmental upheavals, in which phosphorus (P)—the ultimate limiting nutrient for marine productivity—is postulated to have played a key role. However, P availability in the terminal Ediacaran ocean remains uncertain due to the lack of an appropriate proxy record. To better reconstruct seawater P levels during this time interval, we analyzed carbonate-associated phosphate [CAP; expressed as CAP/(Ca + Mg)], a new proxy for P availability in ancient oceans, in three upper Ediacaran successions: the Nama Group (Namibia), the Shibantan Member of the Dengying Formation (Wuhe, South China), and the Algal Dolomite, Gaojiashan and Beiwan members of the Dengying Formation (Gaojiashan, South China). Our results reveal consistently low CAP/(Ca + Mg) values (range: 0.02–0.69 mmol/mol, mean: 0.13 ± 0.01 mmol/mol, 2σ, the same below) for all study sections, falling at the lower end of modern marine carbonate values. Lithofacies, carbonate oxygen isotopes, Mn/Sr and Mg/(Mg + Ca) ratios indicate possible influences from release of Fe-bound P, meteoric diagenesis, recrystallization or dolomitization. The low CAP/(Ca + Mg) values thus represent a maximum estimate for the seawater P availability. The low CAP values from two geographically separated cratons likely reflect a generally small oceanic inorganic P reservoir at least in shelves. This study provides insights into the interplay between nutrient cycling, redox dynamics, and biological evolution during one of the most pivotal transitional periods in Earth history.</abstract>
<year>2026</year>
<issn>0921-8181</issn>
<DOI>https://doi.org/10.1016/j.gloplacha.2026.105284</DOI>
<journal>Global and Planetary Change</journal>
<volume>258</volume>
<pages>105284</pages>
<keywords>Redox conditions, Nama Assemblage, Biomineralization, Oxygen level, Marine productivity, South China</keywords>
<file_url>https://www.sciencedirect.com/science/article/pii/S0921818126000056</file_url>
<authors>
<person>
<fn>Yonghan</fn>
<sn>Fan</sn>
</person>
<person>
<fn>Meng</fn>
<sn>Cheng</sn>
</person>
<person>
<fn>Xinyang</fn>
<sn>Chen</sn>
</person>
<person>
<fn>Catherine</fn>
<sn>Rose</sn>
</person>
<person>
<fn>Haiyang</fn>
<sn>Wang</sn>
</person>
<person>
<fn>Zihu</fn>
<sn>Zhang</sn>
</person>
<person>
<fn>Thomas J.</fn>
<sn>Algeo</sn>
</person>
<person>
<fn>Chao</fn>
<sn>Li</sn>
</person>
</authors>
</reference>
<reference>
<bibtype>article</bibtype>
<citeid>Fernandes2025</citeid>
<title>Coevolution of life and environment during the Ediacaran-Cambrian transition: Clues from litho-, bio-, and chemostratigraphy of the Corumbá Group, Brazil</title>
<type>Article</type>
<year>2025</year>
<DOI>10.1016/j.precamres.2025.107887</DOI>
<journal>Precambrian Research</journal>
<volume>427</volume>
<file_url>https://www.scopus.com/inward/record.uri?eid=2-s2.0-105012164684&amp;doi=10.1016%2fj.precamres.2025.107887&amp;partnerID=40&amp;md5=811262222d0f89a5ce73fd15268519b4</file_url>
<note>Cited by: 0</note>
<authors>
<person>
<fn>Henrique Albuquerque</fn>
<sn>Fernandes</sn>
</person>
<person>
<fn>Gustavo</fn>
<sn>Paula Santos</sn>
</person>
<person>
<fn>Luiz Gustavo</fn>
<sn>Pereira</sn>
</person>
<person>
<fn>Leonardo Thomaz</fn>
<sn>Rimi</sn>
</person>
<person>
<fn>Thales</fn>
<sn>Pescarini</sn>
</person>
<person>
<fn>Eric</fn>
<sn>Elias</sn>
</person>
<person>
<fn>Carolina</fn>
<sn>Bedoya Rueda</sn>
</person>
<person>
<fn>Vinícius</fn>
<sn>Cardoso Lucas</sn>
</person>
<person>
<fn>Larissa</fn>
<sn>Rodrigues</sn>
</person>
<person>
<fn>Karina</fn>
<sn>Mazzamuto</sn>
</person>
<person>
<fn>Ligia</fn>
<sn>Stama</sn>
</person>
<person>
<fn>Sergio</fn>
<sn>Caetano Filho</sn>
</person>
<person>
<fn>Marly</fn>
<sn>Babinski</sn>
</person>
<person>
<fn>Paulo César</fn>
<sn>Boggiani</sn>
</person>
<person>
<fn>Juliana de Moraes</fn>
<sn>Leme</sn>
</person>
<person>
<fn>Fred</fn>
<sn>Bowyer</sn>
</person>
<person>
<fn>Catherine V.</fn>
<sn>Rose</sn>
</person>
<person>
<fn>Ricardo Ivan Ferreira</fn>
<sn>Trindade</sn>
</person>
</authors>
</reference>
<reference>
<bibtype>article</bibtype>
<citeid>Bowyer2025</citeid>
<title>Foundational uncertainties in terminal Ediacaran chronostratigraphy revealed by high-precision zircon U-Pb geochronology of the Nama Group, Namibia</title>
<type>Review</type>
<year>2025</year>
<DOI>10.1016/j.earscirev.2025.105169</DOI>
<journal>Earth-Science Reviews</journal>
<volume>268</volume>
<file_url>https://www.scopus.com/inward/record.uri?eid=2-s2.0-105006603327&amp;doi=10.1016%2fj.earscirev.2025.105169&amp;partnerID=40&amp;md5=b5194e3156879c66347080ba771fc812</file_url>
<note>Cited by: 3; All Open Access, Green Open Access, Hybrid Gold Open Access</note>
<authors>
<person>
<fn>Fred T.</fn>
<sn>Bowyer</sn>
</person>
<person>
<fn>Fabio</fn>
<sn>Messori</sn>
</person>
<person>
<fn>Rachel</fn>
<sn>Wood</sn>
</person>
<person>
<fn>Ulf</fn>
<sn>Linnemann</sn>
</person>
<person>
<fn>Esther</fn>
<sn>Rojo-Perez</sn>
</person>
<person>
<fn>Mandy</fn>
<sn>Zieger-Hofmann</sn>
</person>
<person>
<fn>Johannes</fn>
<sn>Zieger</sn>
</person>
<person>
<fn>Junias</fn>
<sn>Ndeunyema</sn>
</person>
<person>
<fn>Martin</fn>
<sn>Shipanga</sn>
</person>
<person>
<fn>Bontle</fn>
<sn>Mataboge</sn>
</person>
<person>
<fn>Dan</fn>
<sn>Condon</sn>
</person>
<person>
<fn>Catherine V.</fn>
<sn>Rose</sn>
</person>
<person>
<fn>Collen-Issia</fn>
<sn>Uahengo</sn>
</person>
<person>
<fn>Sean P.</fn>
<sn>Gaynor</sn>
</person>
<person>
<fn>Inigo A.</fn>
<sn>Müller</sn>
</person>
<person>
<fn>Gerd</fn>
<sn>Geyer</sn>
</person>
<person>
<fn>Torsten</fn>
<sn>Vennemann</sn>
</person>
<person>
<fn>Joshua H.F.L.</fn>
<sn>Davies</sn>
</person>
<person>
<fn>Maria</fn>
<sn>Ovtcharova</sn>
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</authors>
</reference>
<reference>
<bibtype>article</bibtype>
<citeid>Pescarini2025</citeid>
<title>Magnetic Mineralogy and Paleomagnetic Record of the Nama Group, Namibia: Implications for the Large-Scale Remagnetization of West Gondwanaland and Its Tectonic Evolution</title>
<type>Article</type>
<year>2025</year>
<DOI>10.1029/2024JB030612</DOI>
<journal>Journal of Geophysical Research: Solid Earth</journal>
<volume>130</volume>
<number>3</number>
<file_url>https://www.scopus.com/inward/record.uri?eid=2-s2.0-105000239297&amp;doi=10.1029%2f2024JB030612&amp;partnerID=40&amp;md5=e50dc5cd3cf3581c64140f12d2739944</file_url>
<note>Cited by: 2</note>
<authors>
<person>
<fn>Thales</fn>
<sn>Pescarini</sn>
</person>
<person>
<fn>Ricardo I. F.</fn>
<sn>Trindade</sn>
</person>
<person>
<fn>David A. D.</fn>
<sn>Evans</sn>
</person>
<person>
<fn>Joseph L.</fn>
<sn>Kirschvink</sn>
</person>
<person>
<fn>James</fn>
<sn>Pierce</sn>
</person>
<person>
<fn>Henrique A.</fn>
<sn>Fernandes</sn>
</person>
</authors>
</reference>
<reference>
<bibtype>article</bibtype>
<citeid>Gong2025</citeid>
<title>Magnetic susceptibility cyclostratigraphy of the lower Schwarzrand Subgroup in southern Namibia refines temporal calibration of late Ediacaran bilaterian radiation</title>
<type>Article</type>
<year>2025</year>
<DOI>10.1016/j.gloplacha.2024.104668</DOI>
<journal>Global and Planetary Change</journal>
<volume>245</volume>
<file_url>https://www.scopus.com/inward/record.uri?eid=2-s2.0-85211358096&amp;doi=10.1016%2fj.gloplacha.2024.104668&amp;partnerID=40&amp;md5=fcfe82e0215c7c6274e741dd975dcbb1</file_url>
<note>Cited by: 5; All Open Access, Green Open Access</note>
<authors>
<person>
<fn>Zheng</fn>
<sn>Gong</sn>
</person>
<person>
<fn>Iona</fn>
<sn>Baillie</sn>
</person>
<person>
<fn>Lyle L.</fn>
<sn>Nelson</sn>
</person>
<person>
<fn>Stacey H.</fn>
<sn>Gerasimov</sn>
</person>
<person>
<fn>Catherine</fn>
<sn>Rose</sn>
</person>
<person>
<fn>Emily F.</fn>
<sn>Smith</sn>
</person>
</authors>
</reference>
<reference>
<bibtype>article</bibtype>
<citeid>RN257</citeid>
<title>Project Report: Grinding Through the Ediacaran-Cambrian Transition</title>
<type>Journal Article</type>
<year>2019</year>
<journal>Communications of the Geological Survey of Namibia</journal>
<volume>21</volume>
<pages>1-14</pages>
<file_url>https://www.mme.gov.na/files/publications/78e_GSN%20Comms%2021_1_Rose%20et%20al%20GRIND-ECT.pdf</file_url>
<authors>
<person>
<fn>C. V.</fn>
<sn>Rose</sn>
</person>
<person>
<fn>A.R.</fn>
<sn>Prave</sn>
</person>
<person>
<fn>K. D.</fn>
<sn>Bergmann</sn>
</person>
<person>
<fn>D. J.</fn>
<sn>Condon</sn>
</person>
<person>
<fn>S. A.</fn>
<sn>Kasemann</sn>
</person>
<person>
<fn>F. A.</fn>
<sn>MacDonald</sn>
</person>
<person>
<fn>K.-H.</fn>
<sn>Hoffmann</sn>
</person>
<person>
<fn>R. I. F.</fn>
<sn>Trindade</sn>
</person>
<person>
<fn>M.</fn>
<sn>Zhu</sn>
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</authors>
</reference>
<reference>
<bibtype>article</bibtype>
<citeid>Condon201517</citeid>
<title>Accelerating Neoproterozoic research through scientific drilling</title>
<year>2015</year>
<language>English</language>
<issn>18168957</issn>
<DOI>10.5194/sd-19-17-2015</DOI>
<journal>Scientific Drilling</journal>
<volume>19</volume>
<publisher>Copernicus GmbH</publisher>
<pages>17-25</pages>
<affiliation>NERC Isotope Geoscience Facilities, British Geological Survey, Nottingham, United Kingdom; Instituto de Geociências, Universidade de São Paulo, São Paulo, Brazil; Department of Earth and Planetary Sciences, Washington UniversityWA, United States; Department of Earth and Planetary Sciences, McGill University, Montreal, Canada; Department of Geosciences, University of Bremen, Bremen, Germany; Department of Earth and Planetary Sciences, Harvard University, Cambridge, United States; Department of Earth and Environmental Sciences, University of St Andrews, St Andrews, United Kingdom; State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, China</affiliation>
<keywords>Energy resources;  Mechanical engineering, Neoproterozoic;  Scientific drilling, Drilling</keywords>
<file_url>https://www.scopus.com/inward/record.uri?eid=2-s2.0-84930403996&amp;doi=10.5194%2fsd-19-17-2015&amp;partnerID=40&amp;md5=a64ef5596da10477bab5a1df8581307c</file_url>
<note>cited By 5</note>
<authors>
<person>
<fn>D.J.</fn>
<sn>Condon</sn>
</person>
<person>
<fn>P.</fn>
<sn>Boggiani</sn>
</person>
<person>
<fn>D.</fn>
<sn>Fike</sn>
</person>
<person>
<fn>G.P.</fn>
<sn>Halverson</sn>
</person>
<person>
<fn>S.</fn>
<sn>Kasemann</sn>
</person>
<person>
<fn>A.H.</fn>
<sn>Knoll</sn>
</person>
<person>
<fn>F.A.</fn>
<sn>Macdonald</sn>
</person>
<person>
<fn>A.R.</fn>
<sn>Prave</sn>
</person>
<person>
<fn>M.</fn>
<sn>Zhu</sn>
</person>
</authors>
</reference>
</bib>
