Ecotoxicology: In-Depth Description

Ecotoxicology is the scientific study of the effects of toxic chemicals on biological organisms, specifically at the population, community, and ecosystem levels. The field integrates toxicology and ecology to assess how natural and synthetic pollutants disrupt biological functions, impact biodiversity, and alter ecological dynamics. The primary goal of ecotoxicology is to understand the mechanisms of toxicity and the movement of contaminants through the biosphere, allowing scientists to predict, assess, and mitigate the adverse impacts of environmental stressors before they cause irreversible damage to natural ecosystems.

What Is: The Virome

Scientific Frontline: Extended "At a Glance" Summary: The Virome

The Core Concept: The virome refers to the vast, complex, and heterogeneous collection of all viruses that are found in or on an organism, or within a specific environmental ecosystem.

Key Distinction/Mechanism: Historically relegated to the domain of clinical pathology and infectious disease, viruses are now understood to be the most abundant and influential biological entities on Earth, serving as architects of human physiology and ultimate regulators of global biogeochemical cycles. Rather than exclusively causing overt clinical disease, commensal viruses establish long-term, asymptomatic, and mutualistic relationships that act as continuous, low-level stimulants to the host's immune system, revealing a trans-kingdom functional redundancy that challenges the bacterial-centric view of the microbiome.

Major Frameworks/Components:

• Eukaryotic Viruses: These agents establish persistent or latent infections that constantly shape the host's immunophenotype, conferring basal levels of innate resistance against novel external pathogens.
• Bacteriophages: Functioning as the apex predators of the microscopic world, phages exclusively infect bacteria to rigorously regulate bacterial population density, mediate the horizontal transfer of genetic material, and form protective antimicrobial layers on mucosal surfaces.
• Archaeal Viruses: These distinct entities specifically infect the archaeal domain, deeply influencing archaeal population dynamics and participating in metabolic regulation within complex ecological niches like the deep gastrointestinal tract.
• Endogenous Retroviruses (HERVs): These ancient viral sequences retain potent regulatory functions and have been domesticated for critical life-sustaining processes, such as mammalian placentation via the syncytin protein. Conversely, the aberrant expression of these ancient viral elements is now heavily implicated in severe, progressive neurodegenerative diseases such as Multiple Sclerosis (MS) and Amyotrophic Lateral Sclerosis (ALS).

Not all icebergs are equal – and that matters for the climate, new study finds

Photo Credit: Courtesy of British Antarctic Survey

Scientific Frontline: Extended "At a Glance" Summary: Giant Icebergs and Climate Impact

The Core Concept: Not all giant icebergs, or "megabergs," release fertilizing nutrients into the ocean as they melt; their capacity to stimulate marine life and absorb atmospheric carbon varies drastically depending on their individual life cycles and histories.

Key Distinction/Mechanism: While some icebergs act as "phytoplankton factories" by releasing trapped nutrients and triggering upwelling from deeper waters, others have no measurable biological effect. For example, an iceberg that remains grounded for decades may shed its nutrient-rich outer layers through melting before it drifts into open waters, rendering it unable to fuel ocean blooms compared to a recently calved iceberg.

Major Frameworks/Components:

• Nutrient Release: The biological process by which melting icebergs release essential "fertilizers" into the ocean, providing the foundation for marine food chains.
• Upwelling: A physical mechanism where the meeting of melting ice and deep water draws deeper, nutrient-dense water (rich in nitrogen, phosphorus, and iron) up to the surface.
• Carbon Sequestration: The biological pump where growing phytoplankton absorb atmospheric carbon and subsequently sink to the ocean depths when they die, regulating Earth's climate.
• Biogeochemical Cycling: The overall cycle and movement of carbon and nutrients in the Southern Ocean, heavily influenced by glacial dynamics.

Andes volcanoes – the missing link between algae blooms, whales and climate millions of years ago

Researchers work in the field at Cerro Ballena near Caldera, Chile, as part of a study showing that an increase in volcanic activity in the Andes in the Late Miocene Epoch likely resulted in a cooling of the Earth between 5.4 million and 7 million years ago. From left are team members Carolina Gutstein, Mark Clementz, Barbara Carrapa, Whitney Worrell, Priscilla Martinez and Fabían Muñoz.
Photo Credit: Carolina Gutstein

Scientific Frontline: Extended "At a Glance" Summary: Andes Volcanoes and the Late Miocene Marine-Climate Link

The Core Concept: During the Late Miocene epoch, massive volcanic eruptions in the Andes deposited nutrient-rich ash into the Southern Ocean, triggering widespread marine algae blooms that simultaneously fueled the evolution of gigantic whales, caused localized mass mortality events, and significantly cooled the Earth by drawing atmospheric carbon dioxide into the sea.

Key Distinction/Mechanism: While volcanic activity is traditionally understood as a driver of global warming through the emission of carbon dioxide, this mechanism demonstrates the opposite effect. The volcanic ash delivered vital nutrients (iron, phosphorus, and silicon) to the ocean, hyper-fertilizing primary producers like diatoms. This biological explosion sequestered vast amounts of carbon dioxide from the atmosphere, creating a cooling feedback loop, while simultaneously producing neurotoxins in certain localized blooms that proved fatal to marine mammals.

Major Frameworks/Components: 

• Ocean Geochemistry & Fertilization: The role of volcanic ash in altering ocean chemistry by distributing trace elements like iron, which act as a critical limiting nutrient for marine primary producers.
• The Biological Pump: The process by which photosynthetic phytoplankton (such as diatoms) absorb atmospheric carbon dioxide and sequester it in the deep ocean, driving global temperature reductions.
• Paleoclimatic Modeling: The integration of fossil evidence, geologic geochronology, and computer simulations to test how oceanic biology responds to deliberate volcanic nutrient input.
• Evolutionary Gigantism: The correlation between highly productive, nutrient-rich marine environments and the evolutionary trend toward immense body sizes in baleen whales.

What Is: Phytoplankton

Image Credit: Scientific Frontline

Scientific Frontline: Extended "At a Glance" Summary: Phytoplankton

The Core Concept: Phytoplankton are microscopic, single-celled autotrophs that drift within the sunlit upper layers of the global ocean. They form the foundational base of the marine food web and act as the primary drivers of planetary-scale biogeochemical cycles.

Key Distinction/Mechanism: Unlike mature terrestrial ecosystems, such as the Amazon Rainforest, which consume nearly all the oxygen they generate through aerobic and heterotrophic respiration, phytoplankton enable a permanent net accumulation of atmospheric oxygen. When they die, a fraction of their organic carbon sinks and is buried in anoxic ocean sediments, decoupling it from the biological carbon cycle and leaving the synthesized oxygen in the atmosphere.

Origin/History: Ancestral cyanobacteria evolved the capacity for oxygen-producing photosynthesis between 2.9 and 2.5 billion years ago. This biological innovation eventually triggered the Great Oxidation Event (2.4 to 2.1 billion years ago), fundamentally altering Earth's atmosphere and allowing for the eventual evolution of complex aerobic life.

Climate change may produce “fast-food” phytoplankton

As sea surface temperatures rise over the next century, phytoplankton in polar regions will adapt to be less rich in proteins, heavier in carbohydrates, and lower in nutrients overall. “We’re moving in the poles toward a sort of fast-food ocean,” says MIT postdoc Shlomit Sharoni.
Image Credits: Jose-Luis Olivares, MIT; iStock
(CC BY-NC-ND 3.0)

Scientific Frontline: Extended "At a Glance" Summary: Fast-Food Phytoplankton

The Core Concept: As ocean temperatures rise and sea ice diminishes due to climate change, marine phytoplankton are adapting by shifting from a protein-rich nutritional profile to a carbohydrate- and lipid-heavy composition, effectively becoming a less nutritious "fast food" for the marine ecosystem.

Key Distinction/Mechanism: While previous ecological studies primarily focused on how climate change affects the population sizes and distribution of phytoplankton, this research explicitly models their internal macromolecular readjustment. As sea ice melts and sunlight becomes more abundant in polar regions, phytoplankton require fewer light-harvesting proteins to perform photosynthesis, resulting in a proportional increase in carbohydrates and lipids.

Origin/History: The findings were published in Nature Climate Change on March 31, 2026, by a research team led by MIT postdoctoral researcher Shlomit Sharoni. The conclusions were derived from synthesizing historical field sample data with advanced climate projections extending to the year 2100.

Major Frameworks/Components:

• Macromolecular Composition Modeling: A quantitative framework simulating how marine microalgae balance essential macromolecules (proteins, lipids, carbohydrates, and nucleic acids) under varying environmental conditions.
• Ocean Circulation Dynamics: The integration of lab-based biological data with established ocean circulation models to predict the impact of a 3-degree Celsius sea surface temperature rise, reduced sea ice, and restricted nutrient upwelling.
• Latitudinal Divergence: The model predicts distinct regional adaptations; polar phytoplankton will experience up to a 30 percent decline in protein content, whereas subtropical populations—facing reduced nutrient upwelling—may shift to deeper waters and adopt a slightly more protein-rich composition to maximize limited sunlight.

Bacteria hitching a ride on “marine snow” may slow the ocean’s carbon sink

Marine snow is organic debris and fecal pellets that clump together to form millimeter-long flakes as they fall through the water column.
Photo Credit: ©Woods Hole Oceanographic Institution

Scientific Frontline: Extended "At a Glance" Summary: Marine Snow and the Biological Carbon Pump

The Core Concept: Marine snow is the continuous drift of organic debris—such as dead plankton and fecal pellets—from the ocean's surface down to the deep sea, serving as a primary mechanism for long-term carbon sequestration.

Key Distinction/Mechanism: Rather than sinking passively via gravity, these particles host microbial hitchhikers that actively dissolve calcium carbonate, the mineral acting as the particles' ballast. This localized chemical reshaping makes the particles lighter, causing them to break down at shallower depths and ultimately slowing the efficiency of the ocean's carbon sink.

Origin/History: The discovery of this microbial influence was published on March 11, 2026, in the Proceedings of the National Academy of Sciences by researchers from the Woods Hole Oceanographic Institution (WHOI), MIT, and Rutgers University. It solves a decades-old puzzle regarding why calcium carbonate dissolves in relatively shallow waters despite seemingly stable chemical conditions.

Biogeochemistry: In-Depth Description

Biogeochemistry is the interdisciplinary scientific study of the chemical, physical, geological, and biological processes and reactions that shape the natural environment. By integrating the principles of biology, geology, and chemistry, its primary goal is to understand the flow, transformation, and cycling of essential chemical elements—such as carbon, nitrogen, phosphorus, and sulfur—between the living (biotic) and non-living (abiotic) components of the Earth system.

Understanding how “marine snow” acts as a carbon sink

Hitchhiking bacteria dissolve essential ballast in “marine snow” particles, which could counteract the ocean’s ability to sequester carbon, according to a new study.
Photo Credit: MIT News; iStock
(CC BY-NC-ND 3.0)

Scientific Frontline: Extended "At a Glance" Summary: Marine Snow and Carbon Sequestration

The Core Concept: Marine snow is a continuous shower of organic dust and detritus that falls from the upper layers of the ocean to the seafloor, acting as a vital "biological pump" that transports and stores atmospheric carbon in the deep ocean.

Key Distinction/Mechanism: While it was previously assumed that the calcium carbonate ballast weighing down marine snow remained intact until reaching profound depths, recent findings reveal a microscale disruption. Bacteria hitchhiking on these sinking particles consume organic material and excrete acidic waste, which dissolves the calcium carbonate ballast, slowing the particles' descent and prematurely releasing carbon dioxide back into the shallow ocean.

Major Frameworks/Components: 

• The Biological Pump: The overarching macroscale process by which phytoplankton absorb atmospheric carbon dioxide and convert it into sinking organic matter and calcium carbonate.
• Microbial Dissolution Feedback: The microscale localized chemical reaction where bacterial metabolic waste creates an acidic environment that erodes inorganic calcium carbonate.
• Sinking "Sweet Spot" Dynamics: A hydrodynamic framework demonstrating that dissolution peaks at intermediate sinking speeds, where bacteria remain sufficiently oxygenated but their acidic waste is not flushed away too rapidly by surrounding currents.
  

What Is: Abyssopelagic Zone

A master of abyssopelagic survival, the anglerfish overcomes absolute darkness and sparse food supplies with a specialized, light-producing appendage designed to mimic prey.
Image Credit: Scientific Frontline

Scientific Frontline: Extended "At a Glance" Summary: Abyssopelagic Zone

The Core Concept: The abyssopelagic zone, derived from the Ancient Greek word for "bottomless," is a massive deep-water layer of the pelagic ocean located between 4,000 and 6,000 meters (approximately 13,100 to 19,700 feet) below the sea surface. Covering approximately 83 percent of the total global ocean area, it constitutes the largest single continuous ecosystem on Earth, characterized by near-freezing temperatures, extreme hydrostatic pressures, and the total absence of sunlight.

Key Distinction/Mechanism: Unlike sunlit upper ocean layers, the abyssopelagic zone is completely devoid of solar radiation and autotrophic photosynthesis. Instead, its ecosystem and metabolic processes rely entirely on the downwelling of cold, oxygenated surface waters via global circulation patterns, and the influx of sinking particulate organic carbon (known as "marine snow") falling from the euphotic zone above.

Origin/History: During the foundational oceanographic voyages of the HMS Challenger in the late 19th century, this region was historically conceptualized as a dark, static, and barren wasteland. Modern deep-sea research and long-term sensor mooring have fundamentally reclassified the abyss as an extraordinarily complex, highly dynamic biome.

Positive Interactions Dominate Among Marine Microbes, Six-Year Study Reveals

Lead study author Ewa Merz conducting maintenance on a pump below the Scripps Pier, which brings seawater to the surface for sampling.
Photo Credit: Riley Hale

Scientific Frontline: "At a Glance" Summary

• Main Discovery: Marine microbial communities are driven primarily by positive, mutually beneficial interactions rather than competition, a trend that intensifies during periods of elevated ocean temperature.
• Methodology: Scientists utilized a six-year time series of high-frequency seawater sampling from Scripps Pier combined with DNA sequencing and computational analysis to map interactions among 162 abundant microbial taxa.
• Key Data: Analysis revealed that 78% of microbial associations were positive; specifically, warmer waters caused a 33% drop in total interactions but drove an 11% shift toward facilitation among the remaining connections.
• Significance: These findings challenge the traditional ecological emphasis on competition and predation, suggesting that cooperative networks are critical for microbiome stability and ecosystem function.
• Future Application: Integrating these positive interaction dynamics into climate models will enhance the accuracy of predictions regarding carbon cycling and food web stability in warming oceans.
• Branch of Science: Marine Microbial Ecology
• Additional Detail: The study identified specific "keystone" microbes that disproportionately influence community structure, noting that the identity of these critical species shifts in response to temperature changes.

What Is: Invasive Species

Image Credit: Scientific Frontline / stock image

Scientific Frontline: Extended "At a Glance" Summary

The Core Concept: Invasive species are non-native organisms that, upon introduction to a new environment, escape the evolutionary checks of their native ranges to cause significant ecological, economic, or human health harm. This phenomenon represents a systemic disruption of biophysical systems rather than merely the presence of an unwanted plant or animal.

Key Distinction/Mechanism: The defining characteristic separating "invasive" from "non-native" is impact; while many non-native species (like agricultural crops) are beneficial, invasive species actively dismantle native ecosystems. They often succeed via the Enemy Release Hypothesis, flourishing because they have left behind natural predators and diseases, or through Priority Effects, such as leafing out earlier than native flora to monopolize resources.

Origin/History: While natural translocation has occurred for eons, the current crisis is driven by the "relentless engine of human globalization" in the Anthropocene. The concept is underscored by the "Ten Percent Rule," a statistical filter noting that roughly 10% of transported species survive, 10% of those establish, and 10% of those become destructive invaders.

What Is: Nuclear Winter

A Planetary System Collapse
Image Credit: Scientific Frontline

Scientific Frontline: Extended"At a Glance" Summary

The Core Concept: A severe, prolonged, and global climatic cooling effect hypothesized to occur following widespread urban firestorms ignited by a large-scale nuclear exchange. It represents a fundamental decoupling of the Earth’s climate from its current stable equilibrium, resulting in sub-freezing terrestrial temperatures and precipitation collapse.

Key Distinction/Mechanism: Unlike the immediate, localized destruction of blast waves and radiation, nuclear winter is a planetary-scale environmental catastrophe. The primary mechanism is the injection of millions of tons of black carbon soot into the stratosphere via "pyrocumulonimbus" (fire-driven storm) clouds; this soot intercepts solar radiation, heating the upper atmosphere while plunging the surface into darkness and cold.

Origin/History: The term was coined in the early 1980s (notably associated with the TTAPS studies) and has been rigorously re-examined in the 2020s, culminating in a landmark 2025 consensus study by the National Academies of Sciences, Engineering, and Medicine (NASEM).

Major Frameworks/Components:

• Urban Fuel Loading: Modern cities act as dense reservoirs of combustible mass (plastics, hydrocarbons), capable of fueling firestorms with higher soot yields than mid-20th-century targets.
• Self-Lofting Microphysics: Black carbon particles absorb sunlight and heat the surrounding air, causing the soot plume to rise deeper into the stratosphere (40–50 km) where it persists for years.
• The "Nuclear Niño": A feedback loop where unequal cooling between land and oceans disrupts the Walker Circulation, triggering a seven-year El Niño-like state that collapses marine ecosystems.
• Hydrological Collapse: The stabilization of the atmosphere and reduction in surface evaporation could reduce global precipitation by 40% to 50%, causing a "cold drought."
• "UV Spring": As the soot clears, a severely depleted ozone layer (destroyed by stratospheric heating and nitrogen oxides) exposes the surface to dangerous levels of UV-B radiation.

Why It Matters: Nuclear winter is identified as the primary mechanism of destruction in a nuclear conflict, potentially killing up to 5 billion people through starvation rather than blast effects. It triggers a "system of systems" failure—collapsing agriculture, energy grids, and global trade—that creates an "energy trap" from which civilization may not be able to recover.

The mystery of the missing deep ocean carbon fixers

Alyson Santoro Associate Professor Ecology, Evolution, and Marine Biology
Alyson Santoro's research focuses on microbes involved in nutrient cycling in the ocean, especially of the element nitrogen. This research combines laboratory experiments with field observations, and to date has used genomics, transcriptomics, proteomics and stable isotope geochemistry as tools to uncover the activity of microbes in the mesopelagic ocean.
Photo Credit: Courtesy of University of California, Santa Barbara

In a step toward better understanding how the ocean sequesters carbon, new findings from UC Santa Barbara researchers and collaborators challenge the current view of how carbon dioxide is “fixed” in the sunless ocean depths. UCSB microbial oceanographer Alyson Santoro and colleagues, publishing in the journal Nature Geoscience, present results that help to reconcile discrepancies in accounting for nitrogen supply and dissolved inorganic carbon (DIC) fixation at depth.

“Something that we’ve been trying to get a better handle on is how much of the carbon in the ocean is getting fixed,” Santoro said. “The numbers work out now, which is great.”  

Marine Biology: In-Depth Description

Photo Credit: Neeraj Pramanik

Marine Biology is the scientific study of organisms in the ocean and other brackish bodies of water. This discipline encompasses a vast spectrum of life forms, ranging from microscopic picoplankton to the blue whale, the largest animal on Earth. It is an integrative field that combines elements of geology, chemistry, physical oceanography, and biology to understand the physiology, behavior, and ecological roles of marine organisms, as well as their complex interactions with the high-salinity environment.

Antarctic mountains could boost ocean carbon absorption

Glaciers transport sediments from Antarctica to the coast.
Photo Credit: Dr Kate Winter, Northumbria University

Research involving scientists from Newcastle University has revealed new hope in natural environmental systems found in Antarctica which could help mitigate the overall rise of carbon dioxide. 

As Antarctica's ice sheets thin due to climate change, newly exposed mountain peaks could significantly increase the supply of vital nutrients to the Southern Ocean which surrounds the continent, potentially enhancing its ability to absorb atmospheric carbon dioxide over long timescales, according to the research published in Nature Communications. 

Led by Northumbria University, a team of scientists looked at analysis of sediment samples from East Antarctica's Sør Rondane Mountains. They discovered that weathered rocks exposed above the ice surface contain iron concentrations up to ten times higher than previously reported from the Antarctic continent. This bioavailable iron is transported to the ocean by glaciers and icebergs, where it fuels the growth of phytoplankton – microscopic marine organisms that absorb CO₂ through photosynthesis. 

What Is: A Greenhouse Gas

Image Credit: Skeptical Science
(CC BY 4.0)

A greenhouse gas (GHG) is a constituent of the atmosphere that absorbs and emits longwave radiation, impeding the flow of heat from the Earth's surface into space. This process is the physical basis of the greenhouse effect, formally defined as "the infrared radiative effect of all infrared absorbing constituents in the atmosphere," which includes greenhouse gases, clouds, and some aerosols.

It is essential to distinguish between two distinct phenomena:

The Natural Greenhouse Effect: This is the baseline, life-sustaining process. Greenhouse gases, particularly water vapor and carbon dioxide, are a crucial component of the climate system. Without this natural insulating layer, the heat emitted by the Earth would "simply pass outwards... into space," and the planet's average temperature would be an uninhabitable -20°C.

The Enhanced Greenhouse Effect: This refers to the anthropogenic, or human-caused, intensification of the natural effect. The accumulation of greenhouse gases in the atmosphere, primarily from the burning of fossil fuels and other industrial and agricultural activities, is trapping additional heat, driving the rapid warming of the planet's surface and lower atmosphere.

The term "greenhouse" is a persistent and somewhat misleading analogy. A physical greenhouse primarily works by a mechanical process: its glass walls stop convection, preventing the warm air inside from rising and mixing with the colder air outside. The Earth's greenhouse effect is not a physical barrier; it is a radiative one. Greenhouse gases do not trap air. Instead, they absorb outgoing thermal radiation and re-radiate a portion of it back toward the surface, slowing the planet's ability to cool itself. This radiative mechanism, not a convective one, is how a relatively tiny fraction of the atmosphere can have a planet-altering effect.

Retreating Glaciers May Send Fewer Nutrients to the Ocean

Northwestern Glacier in Alaska has retreated approximately 15 kilometers (nine miles) since 1950.
Photo Credit: Kiefer Forsch/Scripps Institution of Oceanography.

The cloudy, sediment-laden meltwater from glaciers is a key source of nutrients for ocean life, but a new study suggests that as climate change causes many glaciers to shrink and retreat their meltwater may become less nutritious. 

Led by scientists at UC San Diego’s Scripps Institution of Oceanography, the study finds that meltwater from a rapidly retreating Alaskan glacier contained significantly lower concentrations of the types of iron and manganese that can be readily taken up by marine organisms compared to a nearby stable glacier. These metals are scarce in many parts of the ocean including the highly productive Gulf of Alaska, and they are also essential micronutrients for phytoplankton, the microorganisms that form the base of most marine food webs.

What Is: El Niño, La Niña, and a Climate in Flux

Image Credit: Scientific Frontline / NOAA

The Planet's Most Powerful Climate Cycle

In 1997, a climatic event of unprecedented scale began to unfold in the tropical Pacific Ocean. Dubbed the "El Niño of the century," it triggered a cascade of extreme weather that reshaped global patterns for over a year. It unleashed devastating floods and droughts, sparked massive forest fires, decimated marine ecosystems, and crippled national economies. By the time it subsided in 1998, the event was estimated to have caused more than 22,000 deaths and inflicted over $36 billion in damages worldwide. Nearly two decades later, the powerful 2015-16 El Niño, supercharged by a background of long-term global warming, helped propel 2016 to become the hottest year on record and directly impacted the lives and livelihoods of over 60 million people.

These catastrophic events are not random acts of nature but manifestations of the planet's most powerful and influential climate cycle: the El Niño-Southern Oscillation (ENSO). This naturally occurring phenomenon is a periodic, irregular fluctuation of sea surface temperatures and atmospheric pressure across the vast expanse of the equatorial Pacific Ocean. At its heart are two opposing phases: El Niño ("The Little Boy" in Spanish), a significant warming of the ocean surface, and La Niña ("The Little Girl"), a countervailing cooling. Together with a neutral "in-between" state, they form a planetary-scale pendulum that swings irregularly every two to seven years, dictating patterns of drought and flood, storm and calm, across the globe.

Volcanic ash may enhance phytoplankton growth in the ocean over 100 km away

Nishinoshima Island, located in the Ogasawara Islands of Japan, is home to an active volcano. Ash from volcanic eruptions there in 2020 could have led to a temporary surge in phytoplankton levels in the seawater 130 km away.
Photo Credit: Ogasawara Village Tourism Bureau

A research group in Japan has suggested that ash released from volcanic eruptions on Nishinoshima Island—part of Japan's Ogasawara Islands—led to a temporary surge in phytoplankton levels in the seawater around Mukojima Island, which is located 130 km northeast of Nishinoshima and is also part of the Ogasawara Islands.

Mukojima lies within the subtropical gyre, a region known for low nutrient and low chlorophyll conditions. The study indicates that ash from the Nishinoshima eruptions was transported by wind and ocean currents to the waters around Mukojima, serving as a nutrient source for phytoplankton growth in that area.