Articles tagged with Phytoplankton
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.
Researchers found that mussels on restored oyster reefs can filter up to two-fold more plankton than oysters alone, significantly enhancing water quality. This discovery could increase the 'return on investment' for oyster-reef restoration projects.
Researchers discovered that E. huxleyi can grow without thiamine and prefers precursor chemical HMP instead, re-evaluating the importance of vitamin B1 in regulating algal communities. This finding has implications for understanding climate change's impact on marine ecosystems and predicting global carbon cycles.
Researchers found that ocean oxygen increased from 1950 to 1990, contrary to conventional wisdom, due to weaker trade winds. Now, climate change may cause the tropical anoxic zone to shrink as trade wind speed decreases.
A long-term study of the West Antarctic Peninsula finds that changes in climate and sea-ice cover impact the entire polar food web, from single-celled algae to penguins. The study shows how a stable water column favors phytoplankton growth, which is essential for krill recruitment.
A new study reveals that phytoplankton in the Sargasso Sea store more polyphosphate when phosphorus is scarce than expected. The researchers found that polyphosphate is recycled from sinking particles in low-phosphorus environments, making it available for phytoplankton use.
Globally, phytoplankton and zooplankton biomass are projected to decrease by 6% and 11%, respectively, due to rising sea temperatures. This reduction in primary and secondary production will have a negative impact on fish biomass, particularly pelagic species.
The OCULLAR instrument can measure ocean color under low-light conditions, allowing scientists to monitor the health and chemistry of the oceans around the clock. This capability will enable researchers to study phytoplankton, microscopic ocean plants that form the base of the oceanic food web.
Researchers found that both denitrification and anammox are at work in the oceans, with a 70-30 ratio of nitrogen removal. The study settles a decades-long debate over how nitrogen is removed from the ocean and has real-world applications for understanding global climate and productivity.
Phytoplankton release dimethyl sulfide, a chemical signal that attracts krill-eating birds, while also promoting cloud formation. This connection highlights the importance of marine top predators in regulating climate.
The global atlas, MAREDAT, provides unprecedented insights into oceanic plankton diversity and biomass across 500,000 locations worldwide. It reveals surprising findings, such as zooplankton having more biomass than phytoplankton in some regions.
Research shows that phytoplankton form concentrated patches in turbulent ocean water, counterintuitive to expectations of uniform distribution. This phenomenon, known as 'turbulent un-mixing,' helps phytoplankton find cells of the same species without sensory information.
Researchers found that a transient 'perfect storm' of nutrients and light led to the brief bloom of phytoplankton 14,000 years ago. The study resolves conflicting ideas about the relationship between iron and biological productivity in the North Pacific, with implications for geo-engineering efforts to curb climate change.
An international team of biologists led by IU has identified the enzyme and molecular mechanism controlling chromatic acclimation in Synechococcus, a cyanobacteria that maximizes light harvesting for photosynthesis. This discovery has implications for healthcare and climate change research.
Researchers predict warmer oceans will cause phytoplankton to thrive near the poles and shrink in equatorial waters due to temperature changes. This shift could lead to a decline in global carbon cycle and climate change.
Research shows that warmer oceans will cause phytoplankton populations to thrive near the poles and shrink in equatorial waters, leading to significant changes in the food chain and global carbon cycles. This shift could have measurable consequences for the world's climate.
Researchers observed phytoplankton fleeing from zooplankton and even from chemical scents of predators. Fleeing helps the alga survive and makes a difference between life and death.
A team led by USC scientists has identified long-hypothesized vitamin B deficient zones in the ocean using a new analytical technique. These 'vitamin deserts' may inhibit phytoplankton growth and affect the ocean's food chain. The discovery could lead to complex interactions among microbial populations.
Scientists discover that ocean eddies, not sunlight, trigger the annual bloom of tiny plants in the North Atlantic, causing it to occur three weeks earlier than expected. This finding has significant implications for marine life, as many small sea animals rely on the phytoplankton for food and their timing is critical.
Researchers found a massive under-ice phytoplankton bloom in the Arctic, with levels four times greater than neighboring ice-free waters. The bloom extended over 100 kilometers and was fueled by transient skylights and nutrient-rich deep waters.
A new study found that each step of the marine food chain is controlled by the trophic level below it, with prey distribution playing a crucial role. The research reveals that the spatial pattern of resources, or patchiness, is more important than the overall abundance of food.
Researchers discover that phytoplankton release their toxic cargo when exposed to blue light, which stimulates a process called exocytosis. This discovery provides a handle on understanding the development of huge phytoplankton blooms and affects several square miles of ocean's upper surface.
Researchers, led by Canada Excellence Research Chair Marcel Babin, are studying Arctic micro-organisms to better understand their response to environmental changes. The findings suggest that phytoplankton blooms are occurring earlier and more frequently, which could impact the entire food chain.
Phytoplankton, tiny single-celled algae, act as a natural sponge for carbon dioxide and are critical to the global carbon cycle. Research by Canada Research Chair Maria Maldonado has shown that phytoplankton adapt to iron limitation by increasing copper uptake, leading to more efficient carbon absorption.
A team of scientists has discovered that marine plankton, specifically coccolithophores, employ a similar pH-regulation mechanism as vertebrate cells to combat ocean acidification. The armour scales formed by these phytoplankton are found to be dependent on external pH levels.
Researchers discovered that Antarctic icebergs raise chlorophyll levels, increasing carbon dioxide absorption in the Southern Ocean. The findings indicate a new dimension to previous research on icebergs' role in polar ecosystems and global carbon cycling.
Researchers used satellite data to observe and monitor ice-edge blooms across the whole Arctic region. They found that ice-edge blooms occurred in all seasonally ice-covered areas and from spring to late summer.
Researchers at Scripps Institution of Oceanography found phytoplankton bloom timing has progressed up to 50 days earlier in the Arctic Ocean, with unknown impacts on the food chain. The shift may have consequences for the entire ecosystem and global carbon cycle.
The VIMS team is studying the Arctic coastal ecosystem, focusing on nutrient inputs and microbial community changes in response to climate change. Warmer temperatures, increased runoff, and larger ice-free areas may shift productivity from phytoplankton to bacteria, threatening native ecosystems.
A study led by Dr. Stuart Painter identifies five distinct water masses controlling coccolithophore blooms off the southeast coast of South America, highlighting the region's complexity and productivity. The research cruise measured salinity, chemistry, and nutrient levels, confirming that specific conditions foster bloom formation.
A 2008 Kasatochi volcano eruption sparked a record-breaking phytoplankton bloom in the North Pacific Ocean, with iron-laden ash from the eruption taking up only a modest amount of atmospheric CO2
A new device, SeaFlow, detects and tracks microscopic algae that take up 50% of the world's ocean carbon dioxide. This discovery challenges traditional knowledge of ocean ecosystems and highlights the importance of monitoring phytoplankton communities for global carbon cycle understanding.
The quagga mussel's voracious appetite for phytoplankton is causing a decline in its abundance, which in turn is affecting the food chain and fisheries in southern Lake Michigan. As a result, zooplankton populations are dwindling, and fish species such as alewives, chubs, and Atlantic salmon are facing extinction.
A new study reveals a global decline of marine phytoplankton over the past century, with declines of about 1% per year. The decline is strongly correlated with rising sea surface temperatures and changing ocean conditions.
A new study challenges the long-held critical depth hypothesis, which suggests that phytoplankton bloom in temperate oceans due to improving light conditions. Instead, researchers found that winter storms play a key role in creating blooms, and warmer ocean temperatures may actually curtail productivity.
A study found that iron availability plays a crucial role in controlling coccolithophore growth and calcification. Coccolithophores are globally important species of marine algae responsible for massive blooms in oceans worldwide.
A new study suggests that adding nutrients to the sea could lower viral infection rates among phytoplankton, enhancing the biological carbon pump. This process involves transferring carbon from the atmosphere to the deep ocean, potentially helping mitigate global warming.
Computer simulations reveal how ocean stirring and mixing create filamentary structures in plankton patches, resisting dispersal. The research, supported by the Natural Environmental Research Council and the Engineering and Physical Sciences Research Council, provides new insights into plankton patchiness.
Research reveals that increased acidity in Chesapeake Bay is reducing rates of juvenile oyster shell formation, highlighting the need for better monitoring and measurement protocols. Acidity levels vary across different regions of the Bay, with some areas becoming more acidic and others more alkaline.
The study aims to understand how changing climate affects phytoplankton growth and organic carbon distributions. Researchers will collect data on sea surface temperatures, salinities and chlorophyll levels to refine biogeochemistry models.
Scientists at Rutgers University and Woods Hole Oceanographic Institution discover a previously unknown lipid that causes rapid death of phytoplankton in the North Atlantic. The lipid may also hold promise in cancer research by inducing programmed cell death in healthy cells.
A collaborative project between NOAA, the Town of Riverhead, and a commercial oyster farmer is measuring the effect of a FLUPSY on water quality and sediment characteristics in Riverhead's East Creek. The study aims to determine the impact of floating shellfish nurseries on the local environment.
A new study has solved a ten-year-old mystery about the source of an essential nutrient in the ocean. Researchers have discovered that Trichodesmium, a marine phytoplankton group, produces and consumes phosphonate, a rare form of organic phosphorus. This finding is important for understanding the global carbon and nitrogen cycles.
A new study by Florida State University researchers found that low river flow can lead to a decrease in phytoplankton concentration on the continental shelf, affecting food availability for young fish larvae. This could have significant implications for offshore fisheries.
Researchers have analyzed ocean plant health using a NASA satellite, detecting red light emitted by phytoplankton and assessing their productivity. The findings provide insights into the impact of climate change on ocean ecosystems and can help track long-term trends.
Researchers have successfully measured marine phytoplankton physiology through satellite measurements of fluorescence, providing a reasonably accurate picture of the ocean's health and productivity. This will help evaluate the impact of global warming, climate change, and desertification on oceans.
Researchers found phytoplankton levels decreasing in northern part of peninsula and increasing in southern part over past 30 years. This shift may contribute to decline of penguin populations.
Dr. Rosalind Rickaby, a biogeochemist at Oxford University, has been awarded the 2009 Rosenstiel Award for her groundbreaking research on marine phytoplankton and their impact on the Earth's climate. Her innovative approaches are helping to establish a record of the influences these microorganisms have had on the planet.
Researchers discovered that dust from certain regions can be toxic to marine phytoplankton, leading to negative effects on the ocean food web. Copper was found to be a primary cause of toxicity, with varying levels of sensitivity among different species.
Phytoplankton in tropical and subtropical seas use non-phosphorus containing 'substitute lipids' that utilize sulfur instead of phosphorus, allowing them to continue growing under phosphorus stress conditions. This unique strategy has implications for the future structure and biodiversity of Hawaiian marine ecosystems.
Scientists at MIT explain how thin layers of single-celled organisms form at sea and can trap phytoplankton, leading to harmful algal blooms. This research brings the scientific community closer to predicting these events and has implications for other ecological phenomena.
Researchers have discovered phytoplankton in the Sargasso Sea that build cell membranes without phospholipids, using substitute lipids instead. This finding has significant implications for our understanding of cell biochemistry and could lead to rewriting fundamental principles.
Scientists found that natural iron fertilization enhanced phytoplankton growth and productivity in the Southern Ocean, leading to two to three times more carbon export to the deep ocean. The research suggests that ocean islands are a key source of iron for these blooms.