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Two decades of ocean acidification experiments have shown that elevated CO2 can affect many traits in fish early life stages. Only few species, however, show direct CO2-induced survival reductions. This may partly reflect a bias in our current empirical record, which is dominated by species from nearshore tropical-to-temperate environments. There, these organisms already experience highly […]
Read MoreTerrestrial forests are well known as major carbon stores and are already used in carbon credit and offset schemes. In the coastal zone, seaweeds have a similar functional role to trees (carbon dioxide fixation, primary production) and on this basis are being promoted for use as carbon offsets. However, compared to terrestrial forests in which […]
Read MoreThe eastern North Pacific subtropical gyre (NPSG) ecosystem contains a large proportion of the ocean surface, resulting in a significant impact on the global ocean primary production and export production. The NPSG is influenced by the interannual climate variabilities of the Pacific decadal oscillation and North Pacific gyre oscillation (NPGO). In particular, a recent report […]
Read MoreFree-living bacteria play a key role in cycling essential biogeochemical resources in the ocean, including iron, via their uptake, transformation, and release of organic matter throughout the water column. Bacteria process half of the ocean’s primary production, remineralize dissolved organic matter, and re-direct otherwise lost organic matter to higher trophic levels. For these reasons, it […]
Read MoreA vital part of mitigating climate change is the coastal and open ocean carbon sink, without this, it is not possible to meet the target set by the Paris Agreement. More research is needed to better understand the ocean carbon cycle and its future role in the uptake of anthropogenic carbon. A review provides an […]
Read MoreThorium-234 (234Th), a naturally radioactive element present in nature, is one of the most actively used tracers in oceanography. 234Th is widely used to study the removal rate of material on sinking particles from the upper ocean, known as “scavenging,” and for determining the downward flux of carbon. Starting in 1969, ocean measurements of the […]
Read MoreThe total pH scale used by oceanographers (for salinities 20 – 40, and temperatures 0 to 45°C) is calibrated from a combination of electromotive force measurements of artificial seawaters containing either added HCl of various molalities, or equimolal Tris and its protonated form TrisH+. In both cases, the added H+ or TrisH+ is substituted for […]
Read MoreRussia’s invasion of Ukraine brings the threat of nuclear warfare to the forefront. But how would modern nuclear detonations impact the world today? If used accidentally or intentionally, nuclear arsenals would endanger all life on Earth. A new study published in AGU Advances provides stark information on the global impact of nuclear war in a global earth system […]
Read MoreNo single program has been as transformative for ocean science over the past two decades as Argo: the fleet of robotic instruments that collect measurements of temperature and salinity in the upper 2 km of the ocean around the globe. The Argo program has been instrumental in revealing changes to ocean heat content, global sea […]
Read MoreOcean acidification research has grown over the past few decades. Much of recent research documents negative impacts of changing carbonate chemistry on calcifying marine organisms in laboratory experiments. At the 2018 Ocean Acidification PI Meeting, a group of us asked “Can these laboratory responses to ocean acidification be scaled up to accurately predict the responses […]
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