Geochemists have long considered Li isotope composition of marine carbonates as one of
the most straightforward oceanic archives, tracing climate regulation by continental silicate …

Characterizing past climate states is crucial for understanding the future consequences of
ongoing greenhouse gas emissions. Here, we revisit the benchmark time series for deep …

Cold-water coral mounds are key hot-spots of deep ocean biodiversity and also important
archives of past climatic conditions. Nonetheless, the paleo-oceanographic setting in which …

Subsurface water masses formed at high latitudes impact the latitudinal distribution of heat
in the ocean. Yet uncertainty surrounding the timing of low-latitude warming during the last …

The distribution of dissolved iodine in seawater is sensitive to multiple biogeochemical
cycles, including those of nitrogen and oxygen. The iodine-to-calcium ratio (I/Ca) of marine …

Atmospheric CO2 rise in post‐industrial era has resulted in decline in surface ocean pH,
commonly known as “ocean acidification (OA),” which has become a threat to marine …

The boron isotopic ratio of 11B/10B (δ11BSRM951) and trace element composition of
marine carbonates are key proxies for understanding carbon cycling (pH) and …

The concentration of dissolved barium in seawater ([Ba] SW) is influenced by both primary
productivity and ocean circulation patterns. Reconstructing past subsurface [Ba] SW can …

The impact of warming, acidification, and deoxygenation on deep-sea environments is a
growing concern. Historical records are sparse, particularly at high latitudes, making climate …

The chemical and isotopic composition of stony coral skeletons form an important archive of
past climate. However, these reconstructions are largely based on empirical relationships …