IODP3 Expedition 506S, SIGNALS (Stratigraphic InteGration of North Atlantic Legacy Sites), will integrate sediment records to reconstruct North Atlantic climate variability and ocean circulation since the late Miocene.
The North Atlantic strongly influences global climate, yet many sediment cores remain underutilized because of difficulties in correlating records and integrating datasets. SIGNALS will establish a coherent stratigraphic framework, refine age models, and synchronize climate proxy datasets across sites representing diverse climatic conditions and water depths.
Using machine learning, automated core image analysis, and signal correlation methods, the science team will generate high-resolution records and assess uncertainties in their interpretation. These records will improve understanding of major climatic transitions and support climate modelling and comparisons with other paleoclimate initiatives.
The expedition will also develop accessible computational tools, train early-career researchers, and make data publicly available. SIGNALS will strengthen the value of existing sediment archives while advancing understanding of climate feedbacks and tipping points.
IODP3 Expedition 506S, SIGNALS (Stratigraphic InteGration of North Atlantic Legacy Sites), will integrate sediment records to reconstruct North Atlantic climate variability and ocean circulation since the late Miocene.
The North Atlantic strongly influences global climate, yet many sediment cores remain underutilized because of difficulties in correlating records and integrating datasets. SIGNALS will establish a coherent stratigraphic framework, refine age models, and synchronize climate proxy datasets across sites representing diverse climatic conditions and water depths.
Using machine learning, automated core image analysis, and signal correlation methods, the science team will generate high-resolution records and assess uncertainties in their interpretation. These records will improve understanding of major climatic transitions and support climate modelling and comparisons with other paleoclimate initiatives.
The expedition will also develop accessible computational tools, train early-career researchers, and make data publicly available. SIGNALS will strengthen the value of existing sediment archives while advancing understanding of climate feedbacks and tipping points.
The North Atlantic plays a crucial role in regulating global climate due to its proximity to major ice sheets and sensitivity to changes in the Atlantic Meridional Overturning Circulation (AMOC). Over millennial and orbital timescales, the region has experienced abrupt climate shifts with significant global implications. Despite the wealth of sediment cores recovered from North Atlantic legacy sites through International Ocean Discovery Program (IODP) and predecessor programs, many remain underutilized due to challenges in stratigraphic correlation and integration. IODP3 Expedition 506S “SIGNALS – Stratigraphic InteGration of North Atlantic Legacy Sites” aims to synthesize and integrate these legacy records into a coherent, four-dimensional stratigraphic framework to provide a regional reconstruction of past climate variability on millennial to orbital timescales since the late Miocene.
SIGNALS will enhance stratigraphic correlation, refine age models, and synchronize proxy datasets for multiple legacy sites across the North Atlantic spanning a wide range of climatic and bathymetric gradients. The expedition will capitalize on advanced methods, including machine learning and signal correlation algorithms, to rapidly produce high-resolution data by automated processing of core images, point counting, and precise stratigraphic correlation. The IODP3 Expedition 506S Science Team will work collaboratively to produce training datasets to refine AI models, stratigraphic correlation methods, and age models.
SIGNALS will address methodological issues associated with estimating uncertainty in stratigraphic correlations and the limits of temporal resolution at each site given varying sedimentation rates, bioturbation, and sampling frequency. Furthermore, we will develop process models to understand how orbitally-driven climatic changes are expressed as cycles in the stratigraphic record of each site. By analyzing high-resolution geochemical and sedimentological proxies in a robust stratigraphic framework, the expedition will reconstruct climate evolution and ocean circulation changes across the North Atlantic since the late Miocene. It will focus on major climatic transitions and provide robust regional paleoclimate data for numerical modelling and assimilation studies.
Beyond research advancements, SIGNALS will foster collaboration by developing user-friendly computational tools, training early-career researchers, and making data publicly accessible through open repositories. The expedition will contribute to other programmes, such as PAGES PMIP, TIMES, Beyond-EPICA Oldest Ice, by providing robust paleoclimatic information for assimilation and comparison. SIGNALS aligns with key objectives of the 2050 Science Framework, including: Earth’s Climate System, Feedbacks in the Earth System, Tipping Points in Earth History, and Global Cycles of Energy and Matter. Additionally, it addresses the themes of Technology Development and Big Data Analytics through machine learning applications and automated data collection.