Marine microbes play a vital role in ocean health, climate regulation, biodiversity, and the blue bioeconomy. They drive processes including nutrient cycling, carbon sequestration, and primary productivity. AMI recommends acknowledging their importance in European ocean policy to ensure a healthy, resilient, and sustainable ocean.
Researchers at Kyoto University found that viral infection enhances plankton cell lysis, increasing dissolved organic carbon production rates by up to 302-fold. This discovery sheds light on the mechanisms behind marine ecosystems and provides valuable insights for understanding material flows within aquatic environments.
A new mesocosm experiment on Gran Canaria is testing whether concrete rubble can increase ocean alkalinity, mimicking natural rock weathering to absorb CO2 from the atmosphere. The study aims to standardize measurement methods for Ocean Alkalinity Enhancement (OAE) and assess its ecological acceptability.
Scientists used chemical clues in microscopic fossils to find evidence that ocean acidification caused one of the largest extinction events in planktic foraminifera history. The study suggests that volcanic eruptions and rising CO2 levels led to a decrease in shell-building ability, ultimately contributing to the extinction.
Researchers have discovered a complex layering system around phytoplankton cells, with water-repellent substances concentrated near the surface. This finding has significant implications for models of interactions between phytoplankton and bacteria, and could improve our understanding of the oceans' carbon cycle.
Declining plankton abundance across the North East Atlantic poses a significant threat to ocean health, impacting marine food webs and carbon cycling. The study found six pelagic habitat-region combinations rated as 'Not Good' and three as 'Uncertain', highlighting the need for climate change mitigation and reduced nutrient pollution.
Researchers have published a new checklist of 924 diatom taxa alongside a curated dataset of 11,469 records in the open-access journal Biodiversity Data Journal, providing a long-needed foundation for environmental monitoring across the region. This dataset directly answers a key recommendation from the UN Plankton Manifesto and will s...
A study has mapped changes in the distributions of two phytoplankton groups, Pseudo-nitzschia and Dinophysis, which produce toxins that can harm human health and marine ecosystems. The research reveals significant shifts over six decades, with changes aligned more closely with climate-driven ocean physical shifts.
A new study suggests that climate change will shift the balance of macromolecules in phytoplankton from proteins to carbohydrates and lipids, with a 20% increase expected by 2100. This could lead to an unbalanced diet for marine life, with implications for ocean health and human consumption.
A study from the University of California, Davis, reveals that managed wetlands in Suisun Marsh produce 11-22 times more zooplankton than tidal habitats. Zooplankton are crucial for fish diets and increase in response to controlled floods.
Researchers have completed the most comprehensive survey of DNA associated with plankton in the Southern Ocean, revealing a vast genetic diversity that affects the carbon cycle. The study sheds light on the role of microbial ecosystems in climate change and highlights the need to understand how these genes control ocean chemistry.
A new study by University of California San Diego researchers found that fossil fuel plastics can amplify harmful algae blooms by killing off zooplankton, leading to an increase in algal concentrations. In contrast, biodegradable plastics had a smaller impact on zooplankton and algal communities.
New research reveals that life rebounded astonishingly quickly after the asteroid impact, with new species of plankton emerging in fewer than 2,000 years. The study uses an isotope marker to determine the age of sediments and finds that complex life reestablished within a geologic heartbeat.
A new study found that marine heatwaves impact the base of ocean food webs, changing carbon cycling in the process. However, the effects of the two heatwaves were not consistent, with one causing a 'conveyor belt' to jam and increasing the risk of carbon returning to the atmosphere.
A study has found that high-latitude phytoplankton communities responded to a pre-PETM warming event, highlighting the importance of examining background intervals in determining ecosystem change. The results suggest even small environmental changes can have dramatic impacts on marine ecosystems.
A recent study found that the 2014-2016 Northeast Pacific marine heatwave caused unprecedented ecological disturbance, resulting in widespread kelp and seagrass declines and mass mortality events. The research highlights cascading impacts on species interactions, plankton communities, and offshore ocean productivity.
Researchers discovered Polarella, a type of dinoflagellate, in the Eastern Tropical North Pacific Ocean, which contributes significantly to global primary production. The study found increased stress response genes and opportunistic lifestyle in Polarella, suggesting its ecological and biogeochemical role in tropical oceans.
A groundbreaking study reveals that small zooplankton like copepods and krill enhance carbon sequestration through seasonal migrations. These tiny creatures store around 65 million tonnes of carbon annually in the deep ocean.
The Barents Sea system – gateway to the changing Arctic book documents six years of interdisciplinary research on the Barents Sea. Researchers used various platforms, including drones, satellites, and underwater robots, to collect data and make predictions about future changes.
New study reveals insights into giant viruses and their role in marine ecosystems, including photosynthesis manipulation and public health hazards. The discovery of 230 novel giant viruses has significant implications for predicting and managing harmful algal blooms.
Phytoplankton biomass in the North Atlantic has declined by up to 2% per year over six decades, potentially affecting the entire ocean's ecosystem. This decrease may have significant consequences under climate change.
The global ocean has experienced a significant reduction in the depth of its photic zones, home to 90% of all marine life, leading to widespread ocean darkening. This change could have profound implications for the planet's marine species and ecosystem services.
Researchers found that gradual warming causes significant changes in the plankton community, while heatwaves amplify these effects. The study used historical data and an experiment to simulate future warmer scenarios with and without heatwaves.
Researchers warn that artificial oxygen input cannot replace comprehensive water protection strategies. Technical approaches have shown promise, but risks include intensifying greenhouse gases and disrupting marine habitats. Climate protection and reducing nutrient inputs remain crucial for mitigating ocean oxygen loss.
Researchers from the University of Oxford challenge the long-held assumption that water temperature determines the efficiency of ocean carbon capture. The study highlights the need for standardized data collection methods and improved monitoring in polar regions to better understand this critical process.
The study highlights the potential of novel techniques to collect and analyse plankton data more efficiently, filling knowledge gaps and generating complete pictures of plankton dynamics. However, integrating old and new methods is crucial to ensure accurate assessments of marine biodiversity.
A new study found that a unique population of large fish-eating herring has evolved in the Baltic Sea, exhibiting faster growth rates and lower levels of pollutants. These herring have adapted to the brackish water by switching from plankton-eating to a fish diet, with potential benefits for human consumption.
A Dartmouth-led study suggests using clay to convert CO2 into food for zooplankton, which expel it as carbon-filled feces in the deep sea. This method accelerates the ocean's natural cycle for removing carbon from the atmosphere.
Marine plankton's ability to absorb CO2 is influenced by ocean density, with denser waters leading to reduced calcification and increased alkalinity. This discovery reframes our understanding of the complex interplay between marine life and the global climate system.
A recent study reveals that oceans produce a previously unknown sulfur gas called methanethiol, which cools the climate by increasing aerosol formation and reflecting solar radiation. This new compound is found to have a greater cooling capacity than dimethyl sulphide and its impact on climate models.
The MIT team fabricated a simple water filter modeled after the mobula ray's plankton-filtering features and studied its performance. They found that the ray's filtering features are broadly similar to industrial cross-flow filters, which could inform design of water treatment systems.
Many planktonic foraminifera species may face unprecedented environmental conditions by the end of this century, leading to further extinctions and impacting marine ecosystems. Despite shifts in migration patterns and depth, foraminifera populations have declined by 25% over the past 80 years.
A new study reveals that tiny ocean organisms called plankton are struggling to adapt to the current speed of temperature rises, putting marine life at peril. The research highlights the urgent need for collective action to reduce carbon emissions and limit global warming to below 2°C.
The world's freshwater lakes are freezing over for shorter periods due to climate change, affecting more than a billion people worldwide. Changes in ice duration have major implications for human safety, water quality, biodiversity, and global nutrient cycles.
Scientists have discovered microscopic marine organisms producing 'parachute-like' mucus structures that slow their sinking, stalling carbon dioxide absorption from the atmosphere. This finding may have overestimated the ocean's carbon sequestration potential, but also paves the way for improving climate models.
Researchers propose eight research questions to improve mixoplankton classification and study their role in the food web. This knowledge is crucial for predicting ocean ecosystem changes under climate change.
Ancient marine plankton communities showed subtle changes before major extinctions, serving as an early warning system for future ocean life loss. These findings offer new insight into how biodiversity responds to global warming and its relevance to worst-case scenarios.
A study published in Nature found that changes in marine plankton communities can precede mass extinctions. Researchers used a database of fossil records to analyze how plankton responded to climate change over millions of years, revealing that community shifts often occur before losses of biodiversity.
Researchers found a symbiotic relationship between cyanobacteria UCYN-A and marine algae, B. bigelowii, where UCYN-A fix nitrogen gas into ammonium without regulating dinitrogen use. This suggests they may be on the path to becoming organelle-like structures.
Researchers at MSU and Carnegie Science have developed a model connecting microscopic plankton relationships to predictably affect food webs on an ecosystem level. This new model could deepen understanding of nature's laws and create opportunities in ecosystem management.
Research by University of Illinois Urbana-Champaign suggests that phosphorus legacy in riverbeds can delay water quality improvements in the Gulf of Mexico. It may take years or even decades for the reductions to be seen at the Gulf, according to a study published in Science of the Total Environment.
Marine plankton sense external water pressure through the same cells that detect light, triggering them to swim upwards. The larvae respond to increased pressure by swimming faster and in a straighter trajectory.
A new study reveals tiny plankton (0.02mm) make up majority of ocean plankton, playing critical role in ecosystem health and oxygen production. The research emphasizes the need to take these tiny organisms seriously and incorporate them into global ocean policy.
Scientists discover new sulfur cycle mechanism in Lake Superior's ancient waters, highlighting the crucial role of organic sulfur compounds. The findings provide insight into how sulfur was cycled in Earth's oceans billions of years ago.
Researchers isolated five strains of Minorisa from Japanese coastlines and identified three new species: M. fusiformis, M. magna, and M. megafusiformis. These discoveries reveal the previously unknown diversity within the genus Minorisa and provide opportunities to study their ecological role.
Two studies by UPV/EHU researchers analyze recent and past oceanographic information off the Basque coast based on microfauna present in sediments. The research found that planktonic foraminifera assemblages are good indicators of ocean currents and water masses reaching the Basque continental shelf today.
Researchers at UC Santa Barbara found that diatoms and coccolithophores, two key phytoplankton groups, can tolerate increased ocean alkalinity without significant harm. The treatment can speed up the geologic process of carbon sequestration, reducing acidity in oceans.
Researchers found that warming conditions can shift mixotrophic microbes from carbon sinks to carbon emitters, potentially accelerating warming and creating a positive feedback loop. These tiny microbes, abundant in freshwater and marine environments, could act as early warning signals for climate change tipping points.
Researchers have uncovered a previously unknown process in marine phytoplankton that accounts for between 7% to 25% of all oxygen produced and carbon fixed in the ocean. This discovery sheds light on how tiny organisms contribute to global oxygen production, with potential implications for our understanding of evolution.
Research suggests that rapid ocean warming could force plankton to move away from the tropics, negatively affecting marine food chains. The study used microfossils to track the history of zooplankton and found that tropical plankton populations lived in waters more than 2,000 miles from their current location 8 million years ago.
A recent study using planktonic foraminifera fossils found a global clade-wide shift in marine latitudinal zones towards the Equator. The researchers discovered that this shift was not tied to species diversity or functional traits, but rather ecological and morphological characteristics of the organisms.
UC San Diego researchers analyzed plankton samples from the Continuous Plankton Recorder Survey to reconstruct historical marine pollution trends. They found rising levels of manmade chemicals in oceans, which may be used to monitor ecosystem health and study connections between ocean pollution and human chronic illnesses.
A 12,000-year analysis of El Niño's impact on animal communities reveals a tipping point where five or more major events per century lead to dramatic changes in eastern Pacific ecosystems. This finding suggests that strong El Niño events will play an increasingly important role in shaping future ecosystems.
A new study by researchers at University of California - Riverside found that the position of continents can have a devastating effect on deep ocean creatures. Continental movement can cause a sudden collapse in global water circulation, leading to a stark separation between oxygen levels in the upper and lower depths.
Scientists have developed a new model incorporating the day/night cycle into a global ocean biogeochemistry model to investigate its effects on phytoplankton. The study found that diel light cycles significantly impact phytoplankton competition, particularly at lower latitudes.
A Tel Aviv University study reveals that corals' fluorescence serves as a lure for plankton, which are then consumed by predators like corals. The researchers found that green-fluorescent corals were 25% more preyed upon than yellow-fluorescent ones.
A new study reveals the Gulf of Maine is being increasingly influenced by warm water from the North Atlantic, leading to significant changes in its food web. The warming is driven by an influx of North Atlantic water, which has raised temperatures and salinity levels, impacting marine life.
An international team of scientists has discovered a new type of fossilization that provides evidence of plankton resilience during past global warming events. The study found abundant ghost fossils of coccolithophores, which were previously thought to be severely affected by climate change and ocean acidification.
Researchers have developed a model to predict Vibrio vulnificus abundance in the canal by analyzing rainfall, water temperature, dissolved nutrients and organic matter. The study found that warmer waters due to climate change may lead to an increase of twice or three times current levels of bacteria by the end of the century.
Scientists confirm a brief rise in CO2 emissions before the Paleocene-Eocene Thermal Maximum (PETM), an abrupt global warming event. The study reveals unique insights into how Earth's current climate could respond to continued carbon emissions.