Remediation of nitrate pollution of Earth's rivers and aquifers is hampered by cumulative
biogeochemical processes and nitrogen sources. Isotopes (δ 15N, δ 18O) help unravel …

The hydrography of the Arctic Seas is being altered by ongoing climate change, with knock‐
on effects to nutrient dynamics and primary production. As the major pathway of exchange …

A multi-isotopes approach involving the use of stable nitrate isotopes (δ 15 N NO3 and δ 18
O NO3) combined with stable water isotopes (δ 18 O H2O and δ 2 H H2O) as tracers can …

As the world's largest marginal sea, biogeochemical cycling of nitrite (NO2−) in the South
China Sea (SCS) is still unclear. NO2− concentration generally shows a peak at or near the …

Abstract Nitrite (NO2−) is a crucial compound in the N soil cycle. As an intermediate of nearly
all N transformations, its isotopic signature may provide precious information on the active …

Ocean–atmosphere gas exchange in the Arctic Ocean is sensitive to global warming
because the decrease of sea‐ice covered area enhances the exchange. Melting sea ice …

The flow of Pacific water to the North Atlantic exerts a globally significant control on nutrient
balances between the two ocean basins and strongly influences biological productivity in …

Streams play a critical role in attenuating the excess reactive nitrogen (N) generated from
human activities. Consequently, streams can also emit significant amounts of the potent …

Climate change is expected to drastically alter the input of inorganic nitrogen (N) sources in
the Eastern Canadian Arctic Archipelago (ECAA) with increasing discharge from glacial …

Abstract Iron (and silicate)(co-) limitation of phytoplankton is considered a primary cause of
the Southern Ocean's inefficient biological pump. However, the role of phytoplankton …