The NE Pacific has one of the longest open ocean time series, primarily as a result of the weathership station at Station P from the 1950s to 1981. In the 1960s and 70s, the observation that nitrate was never depleted by phytoplankton in summer, was explained by extensive zooplankton grazing and cloudy weather (light limitation). This turned out to be the wrong explanation because certain critical measurements were not available. In the mid 1980s, the late John Martin made the first relatively uncontaminated measurements of iron and revealed that iron concentrations were very low and limited phytoplankton growth. This was a revolutionary discovery, because up to that point, we thought that oceanic productivity was mainly limited by macronut...
Microbial activity is a fundamental component of oceanic nutrient cycles. Photosynthetic microbes, c...
Marine, Asian-derived aerosols are composed of macronutrients, trace metals, organic compounds and m...
Session C32-poster W125A abstract, World Climate Research Programme (WCRP) Open Science Conference (...
The ocean contains about 50 times the amount of carbon in the atmosphere, and currently takes up ab...
Abstract: In order for Fe contained in aeolian dust to act as a micronutrient for oceanic phytoplank...
The limitation of iron (Fe) makes the North Pacific a typically high-nitrate, low-chlorophyll (HNLC)...
The worlds upwelling regions bring nutrient rich water to the euphotic zone and make up the most pri...
This study investigates the effect of iron (FeCl3) incubation on phytoplankton growth in the western...
For Fe contained in long-range transported acolian dust to act as a micronutrient for oceanic phytop...
Dust deposition can supply nutrients to the ocean and affect phytoplankton growth. However, the impa...
Dust is a major source of nutrients to remote ocean environments, influencing primary productivity (...
Dissolved iron is an essential micronutrient for marine phytoplankton, and its availability has cont...
Dust is produced primarily in desert regions and transported long distances through the atmosphere t...
A global marine ecosystem mixed-layer model is used to study iron cycling and nutrient-limitation pa...
<div><p>Although iron is the fourth most abundant element in the Earth's crust, bioavailable iron li...
Microbial activity is a fundamental component of oceanic nutrient cycles. Photosynthetic microbes, c...
Marine, Asian-derived aerosols are composed of macronutrients, trace metals, organic compounds and m...
Session C32-poster W125A abstract, World Climate Research Programme (WCRP) Open Science Conference (...
The ocean contains about 50 times the amount of carbon in the atmosphere, and currently takes up ab...
Abstract: In order for Fe contained in aeolian dust to act as a micronutrient for oceanic phytoplank...
The limitation of iron (Fe) makes the North Pacific a typically high-nitrate, low-chlorophyll (HNLC)...
The worlds upwelling regions bring nutrient rich water to the euphotic zone and make up the most pri...
This study investigates the effect of iron (FeCl3) incubation on phytoplankton growth in the western...
For Fe contained in long-range transported acolian dust to act as a micronutrient for oceanic phytop...
Dust deposition can supply nutrients to the ocean and affect phytoplankton growth. However, the impa...
Dust is a major source of nutrients to remote ocean environments, influencing primary productivity (...
Dissolved iron is an essential micronutrient for marine phytoplankton, and its availability has cont...
Dust is produced primarily in desert regions and transported long distances through the atmosphere t...
A global marine ecosystem mixed-layer model is used to study iron cycling and nutrient-limitation pa...
<div><p>Although iron is the fourth most abundant element in the Earth's crust, bioavailable iron li...
Microbial activity is a fundamental component of oceanic nutrient cycles. Photosynthetic microbes, c...
Marine, Asian-derived aerosols are composed of macronutrients, trace metals, organic compounds and m...
Session C32-poster W125A abstract, World Climate Research Programme (WCRP) Open Science Conference (...