Max Planck Institute for Chemistry, Hahn-Meitner-Weg 1, 55128, Mainz, Germany.
Institute of Earth Sciences, Ruprechts-Karls-Universität Heidelberg, Im Neuenheimer Feld 234, 69120, Heidelberg, Germany.
Sci Data. 2024 Jun 4;11(1):583. doi: 10.1038/s41597-024-03402-0.
Mg/Ca is an independent proxy in paleoceanography to reconstruct past seawater temperature. Femtosecond Laser Ablation Inductively Coupled Plasma Mass Spectrometry (fs-LA-ICP-MS) was employed to determine the Mg/Ca composition of tests (shells) of the planktic foraminifer species Globigerinoides ruber albus (white chromotype) and G. ruber ruber (red/pink chromotype) sampled alive from the temperate to subtropical eastern North Atlantic with the research sailing yacht Eugen Seibold. Mg/Ca data are compared to (i) the measured in-situ temperature of ambient seawater, (ii) average mixed layer temperature, and (iii) sea surface temperature (SST). The pooled mean chamber Mg/Ca from each plankton tow site exhibits a positive relationship with SST. Two chamber-specific calibrations are derived, which are consistent with previous calibration equations for comparable paleo-archives. The results confirm fs-LA-ICP-MS as reliable method for determining Mg/Ca in G. ruber, and both the penultimate and antepenultimate chambers of adult specimens may provide comprehensible Mg/Ca temperatures of the surface ocean.
镁钙比是古海洋学中重建过去海水温度的独立示踪剂。飞秒激光烧蚀电感耦合等离子体质谱法(fs-LA-ICP-MS)被用于测定从东大西洋温带到亚热带海域采集的浮游有孔虫Globigerinoides ruber albus(白变种)和 G. ruber ruber(红/粉红变种)的活标本(贝壳)的镁钙比。镁钙比数据与(i)原位测量的海水温度、(ii)平均混合层温度和(iii)海面温度(SST)进行了比较。每个浮游生物拖网站点的平均腔室镁钙比与 SST 呈正相关。得出了两个腔室特异性的校准曲线,与先前类似古档案的校准方程一致。结果证实 fs-LA-ICP-MS 是测定 G. ruber 中镁钙比的可靠方法,成年标本的倒数第二和倒数第三腔室均可提供对表层海洋的可理解的镁钙比温度。