Controls on carbonate preservation: implications for the skeletal record and the carbon cycle

骨骼碳酸盐是我们获得古生物信息的主要来源，也是碳从大气-海洋转移到岩石圈的主要途径。因此，控制其保存和保真度的过程（即埋藏学）对于解释化石记录和碳循环至关重要。我的研究量化了从个体环境到跨纬度的尺度上的地语学过程和潜在的保存偏差，重点关注沿海环境作为全球元素交换和人为影响的主要场所。在过去的15年里，已经收集了来自热带、温带和极地的样本和数据，为这些纬度比较奠定了基础。作为拟议研究的一部分，将扩大从关键的北极环境（快速环境变化和冰冲刷的地点）获得的初步死亡组合，并辅以实验。此外，还将通过VENUS海底观测系统获得时间序列实验数据，以便更密切地跟踪埋藏过程的性质和偶然性。

Skeletal carbonate is our primary source of paleo-biological information, and the primary means by which carbon is transferred from the atmosphere-ocean to the lithosphere. As such, processes which control its preservation and fidelity (i.e. taphonomy) are of primary importance to interpreting the fossil record and the carbon cycle. My research quantifies taphonomic processes and potential preservation biases at scales ranging from within individual environments to across latitudes, with a focus on coastal settings as the main locus of global elemental exchange and anthropogenic impact. Over the past 15 years samples and data from tropical, temperate, and now polar locations have been collected to form the foundation for these latitudinal comparisons. As part of the proposed research, preliminary death assemblages from the key Arctic setting (site of rapid environmental change and ice-scouring) will be expanded and complimented with experiments. Also, time-series experimental data will be obtained through the VENUS sub-sea observatory system in order to more closely track the nature and episodicity of taphonomic processes.