Articles tagged with Phytoplankton
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Researchers found that Earth's oceans already contain just the right amount of iron, making it unlikely to improve carbon dioxide absorption. Phytoplankton growth is more dependent on organic compounds called ligands, which regulate iron availability.
A new study using a neural network-driven Earth system model predicts an increase in phytoplankton biomass in low-latitude regions by 2100. The team found that the traditional assumption of declining biomass due to climate change is not supported, and instead, phytoplankton may actually thrive in warmer waters.
A new study reveals that phytoplankton in the tropics absorbed high levels of CO2 during Ice Ages due to iron-rich dust. This discovery explains almost all of the additional CO2 transported into oceans via the biological pump, improving climate models and understanding ocean processes.
Research found that sulphur production by tiny marine algae decreased during glacial periods, challenging conventional wisdom. This decrease in sulphur emissions may be linked to changes in climate rather than just the amount of dust in the air, suggesting a closer relationship between phytoplankton and climate.
A rapid-response oceanographic expedition studied the Kilauea Volcano's impact on marine ecosystems. High concentrations of nitrate in seawater triggered a strong phytoplankton bloom, contrary to expectations that lava would contain little nitrogen.
Researchers at Stanford University discovered an aquatic highway that lets nutrients from Earth's belly reach surface waters off Antarctica, stimulating explosive growth of microscopic ocean algae. Hydrothermal vents may affect life near the ocean's surface and global carbon cycle more than previously thought.
Researchers from ETH Zurich have modeled the spatial and temporal distribution of over 530 species of phytoplankton using 700,000 water samples. The study reveals that tropical waters hold the richest diversity of species at all times of the year, while mid-latitudes exhibit lower biodiversity due to strong currents and turbulence.
A new study proposes using iron powder produced by bacteria to stimulate growth of phytoplankton in the ocean, which can help remove carbon dioxide from the atmosphere. This approach aims to supplement decreasing carbon emissions and mitigate climate change by fertilizing microscopic ocean plants.
Researchers developed a new statistical tool to observe interaction among variables influencing phytoplankton abundance over time. They identified a synergistic effect between water temperature and phytoplankton predation, providing insights into spatial synchrony of phytoplankton blooms.
A new study reveals the microbial food web in Amazonian waters, consisting of 20% of the whole Amazon, produces 10 times more CO2 than the classical food chain by decomposing organic matter. This accounts for most of the carbon circulating in lakes, floodplains, and wetlands.
A newly discovered parasitic arsenic cycle in which bacteria keep phytoplankton on an energy-sapping treadmill of nutrient detoxification may offer a glimpse into what further ocean warming will bring. This process could explain the success of SAR11 bacteria, which surpass all other plankton in numbers.
A Norwegian University of Science and Technology (NTNU) team deployed an autonomous underwater vehicle to collect data on phytoplankton, which form the base of the marine food chain. The AUV created a 3-D map of hot spots, providing clues about declining seabird populations.
A new study predicts that over 50% of the world's oceans will shift in color by the year 2100, with blue regions intensifying and green ones deepening. The changes are caused by climate-driven changes in phytoplankton communities and can be detected using satellite measurements.
A new study using Argo floats has gathered unprecedented data on the phytoplankton community beneath the Greenland Sea ice. The research found that half of ocean energy production occurs beneath the sea ice in late winter and early spring, with the other half occurring at the edge of the ice in spring.
The study examines how ocean acidification affects iron availability to phytoplankton, a critical nutrient for marine productivity. Researchers aim to develop proxies for quantifying iron availability under present and future ocean acidification conditions.
New research reveals Arctic phytoplankton blooms are expanding northward at a rate of 1 degree of latitude per decade. The decline in sea ice creates open water areas where phytoplankton can thrive, leading to increased primary productivity and potential changes to the food web.
Bioavailable iron in glacial dust supports phytoplankton growth and enhances climate feedback by removing carbon dioxide. During glacial periods, 25-45% of iron is bioavailable, whereas interglacial periods have only 5-10%.
Harmful algal blooms have become a serious problem for marine life, affecting humans and wildlife. UCLA researchers created a new flow cytometer that analyzes water samples instantly, providing real-time insight into algal bloom locations and severity.
A recent study found that when phytoplankton is infected with a virus, it releases large amounts of chalky particles into the air, affecting cloud properties and Earth's energy balance. The research suggests that these emissions play a significant role in shaping atmospheric conditions.
Phytoplankton, tiny plant-like organisms, play a key role in removing carbon dioxide from the atmosphere through photosynthesis. The EXPORTS team is studying the pathways, fates, and carbon cycle impacts of phytoplankton and zooplankton using advanced underwater robotics and satellite imagery.
A new study predicts that global fisheries will be 20% less productive in 2300, with the North Atlantic and western Pacific experiencing significant declines. Climate change is expected to alter wind patterns, boost ocean temperatures, and melt sea ice, leading to a reduction in phytoplankton growth and nutrient transfer.
Researchers at the University of East Anglia have discovered a key gene responsible for synthesizing dimethylsulfoniopropionate (DMSP), an important nutrient in marine environments. The discovery could allow scientists to better predict the impact of climate change on DMSP production and its effects on the global sulfur cycle.
Researchers found that over broad regions of the South Atlantic, a combination of two or three nutrients was needed to stimulate phytoplankton growth. This study provides experimental evidence for widespread nutrient co-limitation, which has implications for global ocean models and predictions about nutrient limitation.
A VIMS study suggests that a common measure of fish health can help gauge the overall health of the Chesapeake Bay. The researchers found that annual trends in fish condition were surprisingly consistent among diverse species, with correlations between condition and changes in water quality, food availability, and climatic factors.
Researchers from the University of Exeter have discovered a virus that can reprogram ocean plankton to absorb certain nutrients, potentially affecting carbon storage in the ocean. The study found that infected phytoplankton cells become more competitive and grow faster before being killed by the virus.
NASA has adopted a 'sneaker depth' method to visualize and communicate water clarity, inspired by Bernie Fowler's data. The algorithm relates satellite measurements of red light reflection to physical measurements of shoe visibility.
Research suggests that phytoplankton can rapidly adapt to global warming by increasing photosynthesis rates, leading to increased oxygen production and a more stable food supply for aquatic life. The study monitored green algae in waters warmed by four degrees centigrade above ambient temperature over ten years.
A new study by Nereus Program researchers found that climate change will affect energy flows in ocean ecosystems, leading to decreased fish catch in some areas. The authors used a mathematical model to explore the processes that mediate the transfer of energy from phytoplankton growth to fish growth.
Two new phytoplankton groups have been found to favor warmer oceans, defying the expectation that eukaryotic species decline in these conditions. The discovery was made using over 6,000 RNA sequences and time-series sampling, providing insight into future ocean ecosystems.
A space-based sensor has provided a continuous look at phytoplankton boom-bust cycles, revealing they are more tied to the push-pull relationship between predators and prey. The study suggests blooms start when growth rates are slow, not when rates reach a threshold rate.
Scientists at NASA's Goddard Space Flight Center are developing a new method to track ocean heat using satellite magnetic field observations. The approach relies on the electrical conductivity of seawater and its temperature fluctuations, which can be detected from subtle changes in Earth's magnetic field lines.
A recent study found significant correlations between East Asian dust events and chlorophyll a concentration in the North Pacific Ocean and Chinese marginal seas. Dust fertilization on marine biological productivity was also observed, with phytoplankton growth related to dust deposition in the Yellow Sea.
A new study reveals that temperature-induced increases in cell division are the primary driver of phytoplankton blooms. The analysis of nearly 13 years of data from an in situ device found a direct correlation between temperature and cell division rates, with losses due to viruses and predators following closely behind.
A new multiyear study found that warmer ocean temperatures cause Synechococcus cells to divide faster, leading to earlier annual blooms. Despite this, the overall size of the bloom remains stable, and the balance between producers and consumers is maintained through a tight lockstep.
Researchers found that short-lived physical barriers in the ocean caused by temperature or salinity changes influence phytoplankton communities. This provides insight into maintaining high biodiversity of phytoplankton and its impact on the food web.
The KORUS-OC expedition will study the daily changes of the seas surrounding South Korea, focusing on phytoplankton and their role in Earth's carbon cycle. The research aims to better understand how oxygen and carbon flow between the ocean and atmosphere.
Phytoplankton can spread globally in under a decade, while pollution can become a problem within years. The study's model, using Dijkstra's algorithm, confirmed travel times for real-world objects like plastic debris and radioactive particles.
Researchers map phytoplankton blooms using NASA satellite data, revealing El Nino's effect on the marine food web. Phytoplankton populations drop during El Nino events due to disrupted upwelling, impacting fisheries and fish populations.
Researchers at Woods Hole Oceanographic Institution discover that phytoplankton, microscopic plant-like organisms, produce massive amounts of methanol in the ocean, rivaling or exceeding land-based production. This finding challenges previous thinking on oceanic methanol sources and has implications for biofuel applications.
A new study reveals that algal blooms like 'red tides' are home to a complex war between microscopic organisms, with the dominant species changing daily. The research sheds light on the ocean's role in carbon fixation and climate change.
The Island Mass Effect hypothesis explains why seas surrounding islands are more productive. Phytoplankton growth creates a self-sustaining cycle, supporting life from small fish to top predators.
A study published in Nature Communications reveals that coral reef islands and atolls create 'biological hotspots' in the Pacific Ocean due to increased phytoplankton biomass, supporting enhanced food-webs and local fisheries. The Island Mass Effect drives ecosystem productivity and has significant implications for resource management.
In a groundbreaking discovery, scientists found phytoplankton populations double in size above natural oil seeps in the Gulf of Mexico. Turbulence from rising oil and gas bubbles brings up deep-water nutrients that phytoplankton need to grow.
A new study reveals that giant icebergs in the Southern Ocean contribute significantly to carbon sequestration, with enhanced phytoplankton productivity extending hundreds of kilometers beyond the iceberg's length. This process helps slow global warming by storing atmospheric carbon dioxide.
Researchers found that warming ponds had 70% more species and higher rates of photosynthesis in phytoplankton, which could remove more CO2 from the atmosphere. Phytoplankton communities were more species-rich and dominated by larger species, with increased biodiversity and evenness.
Phytoplankton play a crucial role in the ocean's food web and contribute to climate change by removing carbon from the atmosphere. Research reveals complex patterns of response to changing variables like nutrients, light, and ocean stratification, with predictions that global phytoplankton production will decrease.
Researchers from the University of Leicester warn that a six-degree Celsius increase in ocean temperature could stop oxygen production by phytoplankton, leading to catastrophic consequences. This would result in the depletion of atmospheric oxygen on a global scale, causing mass mortality of animals and humans.
Phytoplankton subjected to warmed water initially failed to thrive but evolved tolerance to temperatures expected by the end of the century. The shift enabled them to convert carbon dioxide into new biomass and improve models describing ecological effects of climate change.
Research suggests certain types of carbon-intensive algae are flourishing as carbon pumps, removing CO2 from the atmosphere. A shift in phytoplankton dominance occurred over the past millennium, with a more recent transition happening in less than 200 years.
International workshop highlights need for better forecasting of long-term trends in harmful algal blooms, which threaten wildlife and economies. Research priorities focus on understanding phytoplankton community structure and developing ecological models to prepare for future scenarios.
A 2009 dust storm known as Red Dawn transported soil out to sea, causing a significant marine biological response in the Tasman Sea. The study found that phytoplankton growth was stimulated by iron-rich dust, with positive chlorophyll anomalies reaching up to 0.5mg m-3.
A new MIT study finds that large seasonal changes in desert dust can dramatically affect surface phytoplankton, which rely on iron as a main nutrient for growth. The team determined that iron has a very short residence time in ocean waters, lasting only six months before sinking into the deep ocean.
Researchers found that phytoplankton exposed to fluctuating CO2 levels adapted more to future changes than those grown in stable conditions. However, the adapted algae evolved more and were smaller, potentially impacting marine animal feeding and carbon sequestration.
A recent study by POSTECH researchers suggests that phytoplankton may amplify Arctic warming under greenhouse conditions, contrary to previous assumptions. The growth of phytoplankton is triggered by the melting of sea ice, leading to a positive feedback loop that warms the ocean surface and amplifies climate change.
A massive spring plankton bloom in the North Atlantic Ocean is transported downward by ocean eddies, releasing oxygen and absorbing carbon dioxide. This 'biological pump' helps the oceans absorb CO2 from the atmosphere, mitigating climate change.
A study published in Science reveals that swirling ocean currents, known as eddies, play a significant role in delivering carbon from phytoplankton blooms to the deep ocean. The research, led by Melissa Omand, found that these currents transport small, non-sinking phytoplankton cells to depths of up to 1,000 meters.
Phytoplankton in the open ocean are responsible for half of global oxygen production, but how they assimilate limited nutrients was unclear. A new framework describes how microbial biodiversity affects phytoplankton's ability to take up phosphorus, a key nutrient.
A new study reveals that iron fertilization in the Southern Ocean may reduce the biological carbon pump's ability to transport carbon dioxide into the deep ocean. This process, which draws carbon dioxide from the atmosphere into the sea, is crucial for mitigating climate change.
Phytoplankton, tiny photosynthetic organisms, play a crucial role in regulating the Earth's carbon content. A new study reveals that viruses can rapidly wipe out blooms, fixing large amounts of organic carbon in the process.
Phytoplankton are crucial for fish populations and Earth's carbon cycle, with a perpetual dance between predators and prey affecting their growth cycles. Tiny imbalances in this relationship cause massive phytoplankton blooms, impacting ocean productivity, fisheries, and carbon cycling.