Jena, Partha SarathiPartha SarathiJenaBhushan, RaviRaviBhushanAjay, ShivamShivamAjayDabhi, Ankur J.Ankur J.DabhiGaddam, MaheshMaheshGaddamSudheer, A. K.A. K.Sudheer2025-08-312025-08-312023-07-2010.1016/j.marchem.2023.1042752-s2.0-85164220589http://repository.iitgn.ac.in/handle/IITG2025/26718Quaternary paleoclimatic and paleomagnetic reconstructions using marine sediment cores require appropriate dating techniques in order to build the chronology. Due to the widespread use of the radiocarbon dating method, the majority of studies focusing on paleo reconstructions are restricted to the last 50 ka. There are very few methods those can be used to obtain chronology beyond the radiocarbon dating limit. Marine sediment cores as old as 10–12 Ma can be dated using <sup>10</sup>Be because of its comparatively long half-life of 1.39 Ma. However, there are various intricacies which restrict this method to date young marine sediment cores (<1 Ma). In this study, we provide the findings of measurements obtained for beryllium isotopes (<sup>10</sup>Be and <sup>9</sup>Be) in a sediment core from the central Indian Ocean. It was observed that the changes associated with the decay of <sup>10</sup>Be are much smaller than the Be isotopic fluctuations related to variations in geomagnetic field intensity. While ignoring the points showing high anomalous <sup>10</sup>Be/<sup>9</sup>Be ratios, a continuous decrease in the <sup>10</sup>Be/<sup>9</sup>Be ratio with depth was observed as a function of the decay of <sup>10</sup>Be. Based on the decay of <sup>10</sup>Be, the sediment core was dated to be ∼350 ka (at 570 cm depth) with an average sedimentation rate of 1.6 cm/ka. Radiocarbon dating in conjunction with beryllium isotope data were employed to decipher the past <sup>10</sup>Be production changes due to variations in geomagnetic field intensity over the last 45 ka. A drastic increase in the <sup>10</sup>Be/<sup>9</sup>Be ratio at 41.4 ka was attributed to the Laschamp geomagnetic excursion event. About 40% increase in the <sup>10</sup>Be/<sup>9</sup>Be ratio (hence, <sup>10</sup>Be production) was observed during this event. Another anomalous increase in the <sup>10</sup>Be/<sup>9</sup>Be ratio was observed at ∼300 cm depth, possibly representing the Iceland Basin event. This study highlights the importance of <sup>10</sup>Be as a chronological tool and the limitations associated due to various anomalous excursions associated with <sup>10</sup>Be production and/or environmental modulations.false10Be | Geomagnetic field intensity | Laschamp geomagnetic excursion | Meteoric 10Be datingApplicability of meteoric 10Be in dating marine sediment coresArticle20 July 20233104275arJournal3