Apatite transformations in banded iron formations from the Kongling Group: Insights into metamorphism and ancient seawater conditions
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Abstract
Apatite, a key phosphate mineral, is important for understanding geological processes and ancient sedimentary environments due to its ability to incorporate various trace elements. Despite extensive studies on apatite in Precambrian settings, the effects of metamorphic processes on its geochemical and petrographic characteristics in banded iron formations (BIFs) are still poorly understood. Here, we present results of petrographic and geochemical studies of apatite in BIFs from the Mesoarchaean Yemadong and Huanglianghe formations of the Kongling Group in the northern Yangtze Craton, South China. We employed a range of analytical techniques, including micro-Raman spectroscopy, scanning electron microscopy (SEM), laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS), U-Pb dating, TESCAN Integrated Mineral Analyzer (TIMA) and cathodoluminescence (CL) to characterize the apatite samples, identifying three distinct types (A, B and C) of apatite. Type A apatite has a large grain size and is surrounded by quartz and magnetite, occurring in bands within the BIF. It exhibits positive Eu anomalies, a REE distribution pattern similar to Archaean seawater, and is rich in hydroxyl groups compared to other types of apatite. Type B shows moderate alteration has a relatively small grain size and exhibits anhedral shapes, characterized by negative Eu anomalies, enrichment in fluorine relative to other types of apatite and presence of cracks and inclusions. Type C exhibits high manganese content, relative enrichment of chlorine contrast to other types of apatite and depletion of heavy rare earth elements (HREE), pointing to metamorphic recrystallization in equilibrium with garnet under granulite-facies conditions. Our observations may reveal how metamorphic processes affect the mineralogy and geochemistry of sedimentary apatite, providing insights into the evolution of BIFs and the nature of ancient marine environments.
Keywords
apatite,Banded iron formations,metamorphic processes,mesoarchaean
Speaker
Shuang Shi
Doctoral student China university of geoscience (Wuhan)

Submission Author
Shuang Shi China university of geoscience (Wuhan)
Tongxuan Du China University of Geosciences (Wuhan)
Kenan Cao China University of Geosciences (Wuhan)
Tianyang Li China university of geosicences (Wuhan)
Zhenbing She China university of geosciences (Wuhan)
Dominic Papineau Institute of Deep Sea Science and Engineering
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Important Date
  • Conference Date

    Jun 10

    2025

    to

    Jun 13

    2025

  • Apr 15 2025

    Draft paper submission deadline

Sponsored By
National Natural Science Foundation of China
Geobiology Society
National Committee of Stratigraphy of China
Ministry of Science and Technology
Geological Society of China
Paleontological Society of China
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (CAS)
Institute of Vertebrate Paleontology and Paleoanthropology, CAS
International Commission on Stratigraphy
International Paleontological Association
Organized By
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (CUG, Wuhan)
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