Iron (Fe) bioavailability limits phytoplankton growth in vast ocean regions. Iron-rich dust
uplifted from deserts is transported in the atmosphere and deposited on the ocean surface …

Abstract The εNd and Mg/Ca compositions of terrigenous material from a meridional transect
of seven marine sediment cores located between the northern Red Sea and the Gulf of …

Dust is an important iron (Fe) source to the ocean, but its utilization by phytoplankton is
constrained by rapid sinking and slow dissolution dust-bound iron (dust-Fe). Colonies of the …

The high iron (Fe) demands of Trichodesmium, a keystone nitrogen‐fixing cyanobacterium,
are often met by dust deposition at the ocean surface. Following up on our findings of unique …

Trichodesmium, a globally important, N 2-fixing, and colony-forming cyanobacterium,
employs multiple pathways for acquiring nutrients from air-borne dust, including active dust …

Climate change‐related increase in seawater temperature has become a leading cause of
coral bleaching and mortality. However, corals from the northern Red Sea show high …

Marine particulate fluxes were studied between 2014 and 2017 in the oligotrophic Gulf of
Aqaba (GOA), northern Red Sea. A bottom tethered mooring mounted with 5 sediment trap …

Corals in the Gulf of Aqaba (GoA) in the northern Red Sea show high thermal tolerance. The
GoA has therefore been suggested as a coral reef refuge from climate change. However, as …

Mussels are considered highly efficient marine biomonitors, tracing anthropogenic and
natural variations in heavy metals and various organic compounds. While heavy metals …

Dissolved aluminium (Al) is a primary tracer of atmospheric deposition to the open ocean.
However, the impact of short-term environmental perturbations such as dust storms …