OCB Science Highlights

OCB Science Highlights

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OA could boost carbon export by appendicularia

December 4, 2024

Gelatinous zooplankton comprise a widespread group of animals that are increasingly recognized as important components of pelagic ecosystems. Historically understudied, we have little knowledge of how much key taxa contribute to carbon fluxes. Likewise, there’s a critical knowledge gap of the impact of ocean change on these taxa. Appendicularia are the most abundant gelatinous zooplankton […]

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Quantifying uncertainties in future projections of Chesapeake Bay Hypoxia

December 4, 2024

Climate change is expected to especially impact coastal zones, worsening deoxygenation in the Chesapeake Bay by reducing oxygen solubility and increasing remineralization rates of organic matter. However, simulated responses of this often fail to account for uncertainties embedded within the application of future climate scenarios. Recent research published in Biogeosciences and in Scientific Reports sought […]

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Swirling Currents: How Ocean Mesoscale Affects Air-Sea CO2 Exchange

October 25, 2024

Due to a sparsity of in‐situ observations and the computational burden of eddy‐resolving global simulations, there has been little analysis on how mesoscale processes (e.g., eddies, meanders—lateral scales of 10s to 100s km) influence air‐sea CO2 fluxes from a global perspective. Recently, it became computationally feasible to implement global eddy‐resolving [O (10) km] ocean biogeochemical […]

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How tiny teeth and their prey shape ocean ecosystems

October 25, 2024

It has long been suggested that diatoms, microscopic algae enclosed in silica-shells, developed these structures to defend against predators like copepods, small crustaceans that graze diatoms. Copepods evolved silica-lined teeth presumably to counteract this. But actual evidence for how this predator-prey relationship may drive natural selection and evolutionary change has been lacking. A recent publication […]

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Fast-sinking salp and fish detritus impacts OMZ size and ocean biogeochemical cycles

September 12, 2024

Marine fishes and filter-feeding gelatinous zooplankton such as salps and pyrosomes generate detritus in the form of poop and dead carcasses, which sink ~10 times faster than other oceanic detritus. This detritus is hypothesized to have a disproportionally large impact on the marine biological pump as it sequesters carbon and nutrients deeper in the water […]

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The fate of the 21st century marine carbon cycle could hinge on zooplankton’s appetite

September 11, 2024

Both climate change and the efforts to abate have the potential to reshape phytoplankton community composition, globally. Shallower mixed layers in a warming ocean and many marine CO2 removal (CDR) technologies will shift the balance of light, nutrients, and carbonate chemistry, benefiting certain species over others. We must understand how such shifts could ripple through […]

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Plankton plummet in one of the world’s longest time series

August 2, 2024

Phytoplankton are the main primary producers in the ocean and fuel marine food webs. Long-term shifts in phytoplankton biomass are useful for understanding the context of short-term changes and for examining the relationships between climate indices and phytoplankton dynamics. However, current monitoring programs often offer too short a time frame to disentangle these relationships. In […]

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A New Insight into Ocean Carbon Sequestration

August 1, 2024

How does the microbial carbon pump (MCP) redefine our understanding of oceanic carbon sequestration and climate change mitigation? A recent study published in Nature Reviews Microbiology reviews the pivotal role of the microbial carbon pump (MCP) a novel concept differing from the known mechanisms for carbon sequestration in the ocean, the Biological Carbon Pump (BCP), […]

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Out of sight, out of mind: extreme signals of ocean acidification hidden in the mesopelagic

July 31, 2024

Ocean Acidification (OA), caused by the air-to-sea transfer of anthropogenic carbon (Cant), is intuitively thought to be a surface-intensified process, which makes sense because the concentration of Cant is greatest near the ocean surface and decreases with depth. But this intuition is not correct for multiple metrics of OA that are less commonly studied below […]

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An unexpected shift to a later phytoplankton bloom in the West Antarctic Peninsula

May 29, 2024

Polar regions are changing: warming, losing sea ice, and experiencing shifts in the phenology of seasonal events. Global models predict that phytoplankton blooms will start earlier in these warming polar environments. What we don’t know is will this be true for all high-latitude regions? Is the timing of phytoplankton growing season moving earlier in the […]

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