Here you can find a comprehensive list of NECCTON products. This includes selected high-level information, offering readers and product users an insightful overview of the data provided by NECCTON. Additionally, it provides identifiers for easy retrieval of both product and dataset specifications.
The demersal fish are those species that spend a fraction of their lives in close association with the seabed, feeding primarily on bottom organisms. A typical example of a demersal fish is cod (Gadus morhua). Demersal fish are often an important target of fisheries in marine shelf ecosystems. Demersal fish act as couplers of pelagic and benthic energy pathways.
The demersal fish are those species that spend a fraction of their lives in close association with the seabed, feeding primarily on bottom organisms. A typical example of a demersal fish is cod (Gadus morhua). Demersal fish are often an important target of fisheries in marine shelf ecosystems. Demersal fish act as couplers of pelagic and benthic energy pathways.
The demersal fish are those species that spend a fraction of their lives in close association with the seabed, feeding primarily on bottom organisms. A typical example of a demersal fish is cod (Gadus morhua). Demersal fish are often an important target of fisheries in marine shelf ecosystems. Demersal fish act as couplers of pelagic and benthic energy pathways.
Unspecified fish biomass are those fish species that do not fall into the categories of small pelagic species, large pelagic species or demersal fish species (both small and large). In NECCTON this would be the total biomass of all fish, i.e. include all these biological subcomponents.
Unspecified fish biomass are those fish species that do not fall into the categories of small pelagic species, large pelagic species or demersal fish species (both small and large). In NECCTON this would be the total biomass of all fish, i.e. include all these biological subcomponents.
Unspecified fish biomass are those fish species that do not fall into the categories of small pelagic species, large pelagic species or demersal fish species (both small and large). In NECCTON this would be the total biomass of all fish, i.e. include all these biological subcomponents.
Unspecified fish biomass are those fish species that do not fall into the categories of small pelagic species, large pelagic species or demersal fish species (both small and large). In NECCTON this would be the total biomass of all fish, i.e. include all these biological subcomponents.
Unspecified fish biomass are those fish species that do not fall into the categories of small pelagic species, large pelagic species or demersal fish species (both small and large). In NECCTON this would be the total biomass of all fish, i.e. include all these biological subcomponents.
Unspecified fish biomass are those fish species that do not fall into the categories of small pelagic species, large pelagic species or demersal fish species (both small and large). In NECCTON this would be the total biomass of all fish, i.e. include all these biological subcomponents.
Unspecified fish biomass are those fish species that do not fall into the categories of small pelagic species, large pelagic species or demersal fish species (both small and large). In NECCTON this would be the total biomass of all fish, i.e. include all these biological subcomponents.
Unspecified fish biomass are those fish species that do not fall into the categories of small pelagic species, large pelagic species or demersal fish species (both small and large). In NECCTON this would be the total biomass of all fish, i.e. include all these biological subcomponents.
Unspecified fish biomass are those fish species that do not fall into the categories of small pelagic species, large pelagic species or demersal fish species (both small and large). In NECCTON this would be the total biomass of all fish, i.e. include all these biological subcomponents.
Understanding the distribution of marine mammals (MM) is essential to gain insights into their ecology and population dynamics, to implement conservation and management measures and assess their effectiveness, and to project the future of the ecosystem services and goods they provide (food provisioning, top-down control of the food web, carbon regulation, tourism, and leisure). The current Copernicus Marine Service does not include any products for large marine top predators such as marine mammals. This limitation prevents Copernicus Marine Service from providing stakeholders with products to assess the role of large marine top predators on the ecosystem. NECCTON will provide a new HTL model for marine mammals with the objective of providing new useful decision-tools to all stakeholders involved in the management or conservation of high trophic levels.
Datasets ID: H12
Partners:
The National Institute of Oceanography and Applied Geophysics
Region: Adriatic Sea
Understanding the distribution of marine mammals (MM) is essential to gain insights into their ecology and population dynamics, to implement conservation and management measures and assess their effectiveness, and to project the future of the ecosystem services and goods they provide (food provisioning, top-down control of the food web, carbon regulation, tourism, and leisure). The current Copernicus Marine Service does not include any products for large marine top predators such as marine mammals. This limitation prevents Copernicus Marine Service from providing stakeholders with products to assess the role of large marine top predators on the ecosystem. NECCTON will provide a new HTL model for marine mammals with the objective of providing new useful decision-tools to all stakeholders involved in the management or conservation of high trophic levels.
A significant amount of plastics currently ends up in the marine environment, raising concern for wildlife and human health. Plastics affect marine organisms through ingestion and/or entanglement, while microplastics that represent the smaller size class (particles <5 mm), may interact with low trophic-level organisms (i.e., phytoplankton and zooplankton) and their predators, finding their way up the food chain and human diet. Microplastics are either primary (personal care products, pre-production pellets) or secondary, originating from the fragmentation of larger items. Plastics in the marine environment originate from both land-based sources (coastlines ~39-42%, rivers 12-13%) and sea-based sources (fishing activities 45-48%), with their fate being determined by various physical (waves, currents, wind) and biogeochemical (e.g., biofouling) processes. Thus, models taking into account the most important processes and source inputs provide powerful tools for the assessment of marine litter pollution.
Datasets ID: H31
Partners:
MINDS
Region: Mediterranean Sea
A significant amount of plastics currently ends up in the marine environment, raising concern for wildlife and human health. Plastics affect marine organisms through ingestion and/or entanglement, while microplastics that represent the smaller size class (particles <5 mm), may interact with low trophic-level organisms (i.e., phytoplankton and zooplankton) and their predators, finding their way up the food chain and human diet. Microplastics are either primary (personal care products, pre-production pellets) or secondary, originating from the fragmentation of larger items. Plastics in the marine environment originate from both land-based sources (coastlines ~39-42%, rivers 12-13%) and sea-based sources (fishing activities 45-48%), with their fate being determined by various physical (waves, currents, wind) and biogeochemical (e.g., biofouling) processes. Thus, models taking into account the most important processes and source inputs provide powerful tools for the assessment of marine litter pollution.
Datasets ID: H33
Partners:
UU
Region: North-West (NW) European Shelf
A significant amount of plastics currently ends up in the marine environment, raising concern for wildlife and human health. Plastics affect marine organisms through ingestion and/or entanglement, while microplastics that represent the smaller size class (particles <5 mm), may interact with low trophic-level organisms (i.e., phytoplankton and zooplankton) and their predators, finding their way up the food chain and human diet. Microplastics are either primary (personal care products, pre-production pellets) or secondary, originating from the fragmentation of larger items. Plastics in the marine environment originate from both land-based sources (coastlines ~39-42%, rivers 12-13%) and sea-based sources (fishing activities 45-48%), with their fate being determined by various physical (waves, currents, wind) and biogeochemical (e.g., biofouling) processes. Thus, models taking into account the most important processes and source inputs provide powerful tools for the assessment of marine litter pollution.
Datasets ID: H34
Partners:
UU
Region: Arctic
Reflectance (RRS) is the ratio of the electromagnetic flux reflected by a surface to the total electromagnetic flux incident on the surface. Water reflectance, as a function of the wavelength of electromagnetic radiation, provides useful information about the different types of suspended and dissolved components of matter in the ocean. It is used to identify various spectral features through the analysis of their inherent optical properties (i.e., absorption and backscattering). RRS is used to derive chlorophyll using empirical algorithms.
Datasets ID: H5
Partners:
BSH
Region: Baltic Sea
This product will provide maps of the vertically integrated carbon content in sediment for the North, Baltic, Black and Mediterranean Seas. Sedimentary carbon content provides information on the amount of food available to support the benthic food web and diagenetic processes. Its spatial distribution offers information on the functioning of benthic organisms (suspension versus deposit feeding).
Datasets ID: H3
Partners:
UoL
Region: Black Sea
This product will provide maps of the vertically integrated carbon content in sediment for the North, Baltic, Black and Mediterranean Seas. Sedimentary carbon content provides information on the amount of food available to support the benthic food web and diagenetic processes. Its spatial distribution offers information on the functioning of benthic organisms (suspension versus deposit feeding).
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
This product will provide maps of the vertically integrated carbon content in sediment for the North, Baltic, Black and Mediterranean Seas. Sedimentary carbon content provides information on the amount of food available to support the benthic food web and diagenetic processes. Its spatial distribution offers information on the functioning of benthic organisms (suspension versus deposit feeding).
Datasets ID: H5
Partners:
BSH
Region: Baltic Sea
The macrozoobenthos, usually defined as benthic macrofauna larger than 1 mm in size, is an essential element in benthic-pelagic coupling, because it mediates particulate and solute fluxes between the water column and sediments. It degrades organic matter that sinks to the bottom, changes biogeochemical properties of sediments via bioturbation and bioirrigation, affecting, for instance, rates of microbial oxidation and denitrification. It also serves as a food source for higher trophic levels, thus helping to sustain fish and fisheries. Macrozoobenthic communities, in turn, respond to organic matter supplied from the water column, hydrodynamic regime, and temperature. Major feeding groups (suspension and deposit feeders) differ in diet composition and vertical habitat distribution, which defines their functioning. In turn, their environment and changes in its characteristics affect these groups differently.
Datasets ID: H40
Partners:
NIOZ
Region: Black Sea
The macrozoobenthos, usually defined as benthic macrofauna larger than 1 mm in size, is an essential element in benthic-pelagic coupling, because it mediates particulate and solute fluxes between the water column and sediments. It degrades organic matter that sinks to the bottom, changes biogeochemical properties of sediments via bioturbation and bioirrigation, affecting, for instance, rates of microbial oxidation and denitrification. It also serves as a food source for higher trophic levels, thus helping to sustain fish and fisheries. Macrozoobenthic communities, in turn, respond to organic matter supplied from the water column, hydrodynamic regime, and temperature. Major feeding groups (suspension and deposit feeders) differ in diet composition and vertical habitat distribution, which defines their functioning. In turn, their environment and changes in its characteristics affect these groups differently.
Datasets ID: H2
Partners:
UKMO/PML
Region: North-West (NW) European Shelf
The macrozoobenthos, usually defined as benthic macrofauna larger than 1 mm in size, is an essential element in benthic-pelagic coupling, because it mediates particulate and solute fluxes between the water column and sediments. It degrades organic matter that sinks to the bottom, changes biogeochemical properties of sediments via bioturbation and bioirrigation, affecting, for instance, rates of microbial oxidation and denitrification. It also serves as a food source for higher trophic levels, thus helping to sustain fish and fisheries. Macrozoobenthic communities, in turn, respond to organic matter supplied from the water column, hydrodynamic regime, and temperature. Major feeding groups (suspension and deposit feeders) differ in diet composition and vertical habitat distribution, which defines their functioning. In turn, their environment and changes in its characteristics affect these groups differently.
Datasets ID: H40
Partners:
NIOZ
Region: Black Sea
Benthic flora are essential elements in benthic-pelagic coupling and in carbon sequestration (blue carbon). Besides uptake of inorganic carbon and production of oxygen, the most important species of flora are habitat builders that often help stabilise sediment (e.g., seagrasses) and provide shelter, spawning, and nursery ground for multiple species, including some of commercial interest. Moreover, benthic flora typically supports high associated biodiversity.
Benthic flora are essential elements in benthic-pelagic coupling and in carbon sequestration (blue carbon). Besides uptake of inorganic carbon and production of oxygen, the most important species of flora are habitat builders that often help stabilise sediment (e.g., seagrasses) and provide shelter, spawning, and nursery ground for multiple species, including some of commercial interest. Moreover, benthic flora typically supports high associated biodiversity.
This product will provide maps of carbon sequestration (I.e. carbon burial) and denitrification rates (NO3 removal) in Black Sea sediment.
Datasets ID: H40
Partners:
UoL
Region: Black Sea
This product will provide maps of carbon sequestration (I.e. carbon burial) and denitrification rates (NO3 removal) in Black Sea sediment.
Datasets ID: H40
Partners:
UoL
Region: Black Sea
Small pelagic fishes (SPF) are a key component of marine food webs, often present with a large but fluctuating biomass of mid-trophic level fish, therefore making the link between primary and secondary productions and top predators. They also constitute a group of major economic importance for several countries. Implementing operational models for such organisms is a challenge due to the complexity of biological systems, which results in a large diversity of models allowing to address multiple questions for management and conservation, ranging from ecosystem services to catch quotas or fishing area closures for specific species or fisheries.
Small pelagic fishes (SPF) are a key component of marine food webs, often present with a large but fluctuating biomass of mid-trophic level fish, therefore making the link between primary and secondary productions and top predators. They also constitute a group of major economic importance for several countries. Implementing operational models for such organisms is a challenge due to the complexity of biological systems, which results in a large diversity of models allowing to address multiple questions for management and conservation, ranging from ecosystem services to catch quotas or fishing area closures for specific species or fisheries.
The current Copernicus Marine Service does not include operational models for large pelagic fish species and other higher trophic levels of marine ecosystems (HTL). This limitation prevents Copernicus Marine Service from providing stakeholders with products to assess the diversity and biomass of commercial or endangered marine species. Implementing operational models for HTL is a challenge due to the complexity of biological systems and hence their modelling. HTL models are also more diverse than physical or biogeochemical models since they target multiple questions for management and conservation, ranging from ecosystem services to catch quotas or fishing area closures for specific species or fisheries. NECCTON propose new developments enabling Copernicus Marine Service to model and deliver HTL products by all MFCs with the objective of providing new useful decision-tools to all stakeholders involved in the management of fisheries and conservation of marine ecosystems.
The current Copernicus Marine Service does not include operational models for large pelagic fish species and other higher trophic levels of marine ecosystems (HTL). This limitation prevents Copernicus Marine Service from providing stakeholders with products to assess the diversity and biomass of commercial or endangered marine species. Implementing operational models for HTL is a challenge due to the complexity of biological systems and hence their modelling. HTL models are also more diverse than physical or biogeochemical models since they target multiple questions for management and conservation, ranging from ecosystem services to catch quotas or fishing area closures for specific species or fisheries. NECCTON propose new developments enabling Copernicus Marine Service to model and deliver HTL products by all MFCs with the objective of providing new useful decision-tools to all stakeholders involved in the management of fisheries and conservation of marine ecosystems.
The current Copernicus Marine Service does not include operational models for large pelagic fish species and other higher trophic levels of marine ecosystems (HTL). This limitation prevents Copernicus Marine Service from providing stakeholders with products to assess the diversity and biomass of commercial or endangered marine species. Implementing operational models for HTL is a challenge due to the complexity of biological systems and hence their modelling. HTL models are also more diverse than physical or biogeochemical models since they target multiple questions for management and conservation, ranging from ecosystem services to catch quotas or fishing area closures for specific species or fisheries. NECCTON propose new developments enabling Copernicus Marine Service to model and deliver HTL products by all MFCs with the objective of providing new useful decision-tools to all stakeholders involved in the management of fisheries and conservation of marine ecosystems.
The demersal fish are those species that spend a fraction of their lives in close association with the seabed, feeding primarily on bottom organisms. A typical example of a demersal fish is cod (Gadus morhua). Demersal fish are often an important target of fisheries in marine shelf ecosystems. Demersal fish act as couplers of pelagic and benthic energy pathways.
The demersal fish are those species that spend a fraction of their lives in close association with the seabed, feeding primarily on bottom organisms. A typical example of a demersal fish is cod (Gadus morhua). Demersal fish are often an important target of fisheries in marine shelf ecosystems. Demersal fish act as couplers of pelagic and benthic energy pathways.
The demersal fish are those species that spend a fraction of their lives in close association with the seabed, feeding primarily on bottom organisms. A typical example of a demersal fish is cod (Gadus morhua). Demersal fish are often an important target of fisheries in marine shelf ecosystems. Demersal fish act as couplers of pelagic and benthic energy pathways.
The demersal fish are those species that spend a fraction of their lives in close association with the seabed, feeding primarily on bottom organisms. A typical example of a demersal fish is cod (Gadus morhua). Demersal fish are often an important target of fisheries in marine shelf ecosystems. Demersal fish act as couplers of pelagic and benthic energy pathways.
Reflectance (RRS) is the ratio of the electromagnetic flux reflected by a surface to the total electromagnetic flux incident on the surface. Water reflectance, as a function of the wavelength of electromagnetic radiation, provides useful information about the different types of suspended and dissolved components of matter in the ocean. It is used to identify various spectral features through the analysis of their inherent optical properties (i.e., absorption and backscattering). RRS is used to derive chlorophyll using empirical algorithms.
Datasets ID: H3
Partners:
UoL
Region: Black Sea
Reflectance (RRS) is the ratio of the electromagnetic flux reflected by a surface to the total electromagnetic flux incident on the surface. Water reflectance, as a function of the wavelength of electromagnetic radiation, provides useful information about the different types of suspended and dissolved components of matter in the ocean. It is used to identify various spectral features through the analysis of their inherent optical properties (i.e., absorption and backscattering). RRS is used to derive chlorophyll using empirical algorithms.
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
Suspended particulate matter (SPM) is a collective term for the inorganic (e.g., mineral) and organic (e.g., detritus; see next section) particulates that are suspended in the water column. It is an indicator of sediment transport, water clarity and quality; and has important implications for pelagic and benthic productivity and erosion. It can also act as a vector for the transfers of pollutants and contaminants.
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
Suspended particulate matter (SPM) is a collective term for the inorganic (e.g., mineral) and organic (e.g., detritus; see next section) particulates that are suspended in the water column. It is an indicator of sediment transport, water clarity and quality; and has important implications for pelagic and benthic productivity and erosion. It can also act as a vector for the transfers of pollutants and contaminants.
Datasets ID: H3
Partners:
UoL/Hereon
Region: Black Sea
Bottom Oxygen concentration is an indicator of ecosystem health and particularly the presence of coastal hypoxia that often occurs at the bottom.
Datasets ID: H3
Partners:
UoL
Region: Black Sea
Bottom Oxygen concentration is an indicator of ecosystem health and particularly the presence of coastal hypoxia that often occurs at the bottom.
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
Bottom Oxygen concentration is an indicator of ecosystem health and particularly the presence of coastal hypoxia that often occurs at the bottom.
Datasets ID: H5
Partners:
BSH
Region: Black Sea
Bottom Oxygen concentration is an indicator of ecosystem health and particularly the presence of coastal hypoxia that often occurs at the bottom.
Datasets ID: H5
Partners:
BSH
Region: Baltic Sea
Potential Hydrogen, better known as pH, is a measure of acidity/ basicity of a solution expressed on a logarithmic scale; a pH of 7 denotes a neutral solution whereas lower and higher values characterise more acidic and alkaline waters, respectively, compared to the neutral state. Studies generally report pH on a concentration scale representing a measure of proton activity. As a measure of acidification, pH represents an important indicator of ecosystem health.
Datasets ID: H6
Partners:
OGS
Region: Mediterranean Sea
Potential Hydrogen, better known as pH, is a measure of acidity/ basicity of a solution expressed on a logarithmic scale; a pH of 7 denotes a neutral solution whereas lower and higher values characterise more acidic and alkaline waters, respectively, compared to the neutral state. Studies generally report pH on a concentration scale representing a measure of proton activity. As a measure of acidification, pH represents an important indicator of ecosystem health.
Datasets ID: H3
Partners:
UoL
Region: Black Sea
Potential Hydrogen, better known as pH, is a measure of acidity/ basicity of a solution expressed on a logarithmic scale; a pH of 7 denotes a neutral solution whereas lower and higher values characterise more acidic and alkaline waters, respectively, compared to the neutral state. Studies generally report pH on a concentration scale representing a measure of proton activity. As a measure of acidification, pH represents an important indicator of ecosystem health.
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
Potential Hydrogen, better known as pH, is a measure of acidity/ basicity of a solution expressed on a logarithmic scale; a pH of 7 denotes a neutral solution whereas lower and higher values characterise more acidic and alkaline waters, respectively, compared to the neutral state. Studies generally report pH on a concentration scale representing a measure of proton activity. As a measure of acidification, pH represents an important indicator of ecosystem health.
Datasets ID: H5
Partners:
BSH
Region: Arctic
Bottom light availability is an important environmental information in determining regions where marine flora; seaweeds, seagrasses and microphytobenthos; can develop. We will deliver the bottom light product as Photosynthetic Active Radiation (PAR), which includes radiation wavelengths between 400-700 nm.
Datasets ID: H6
Partners:
OGS
Region: Mediterranean Sea
Bottom light availability is an important environmental information in determining regions where marine flora; seaweeds, seagrasses and microphytobenthos can develop. We will deliver the bottom light product as Photosynthetic Active Radiation (PAR), which includes radiation wavelengths between 400-700.
Datasets ID: H41
Partners:
UoL
Region: Black Sea
Bottom light availability is an important environmental information in determining regions where marine flora; seaweeds, seagrasses and microphytobenthos; can develop. We will deliver the bottom light product as Photosynthetic Active Radiation (PAR), which includes radiation wavelengths between 400-700 nm.
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
Bottom light availability is an important environmental information in determining regions where marine flora; seaweeds, seagrasses and microphytobenthos; can develop. We will deliver the bottom light product as Photosynthetic Active Radiation (PAR), which includes radiation wavelengths between 400-700 nm.
Datasets ID: H5
Partners:
BSH
Region: Baltic Sea
The flux of organic carbon to the bottom critically drives benthic ecosystems through the benthic food chain, diagenesis, and quantity of carbon sequestration through burial. The difficulty of in-situ determination greatly limits Information on carbon flow to the bottom at the ecosystem scale. Models can provide important information on carbon flux to the bottom at ecosystem scale and on its spatial and temporal variation.
Datasets ID: H6
Partners:
OGS
Region: Mediterranean Sea
The flux of organic carbon to the bottom critically drives benthic ecosystems through the benthic food chain, diagenesis, and quantity of carbon sequestration through burial. The difficulty of in-situ determination greatly limits Information on carbon flow to the bottom at the ecosystem scale. Models can provide important information on carbon flux to the bottom at ecosystem scale and on its spatial and temporal variation.
Datasets ID: H3
Partners:
UoL
Region: Black Sea
The flux of organic carbon to the bottom critically drives benthic ecosystems through the benthic food chain, diagenesis, and quantity of carbon sequestration through burial. The difficulty of in-situ determination greatly limits Information on carbon flow to the bottom at the ecosystem scale. Models can provide important information on carbon flux to the bottom at ecosystem scale and on its spatial and temporal variation.
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
The flux of organic carbon to the bottom critically drives benthic ecosystems through the benthic food chain, diagenesis, and quantity of carbon sequestration through burial. The difficulty of in-situ determination greatly limits Information on carbon flow to the bottom at the ecosystem scale. Models can provide important information on carbon flux to the bottom at ecosystem scale and on its spatial and temporal variation.
Datasets ID: H5
Partners:
BSH
Region: Baltic Sea
Mesozooplankton are heterotrophic organisms in the size range from 0.2 to 20 mm. Mesozooplankton move with ocean currents but can migrate vertically in the water column. Mesozooplankton generally feed on primary producers, microzooplankton and detritus particles. They are an important prey for fish larva and planktivorous fish and therefore represent an important link between primary producers and higher trophic levels.
Datasets ID: H4
Partners:
NERSC
Region: Arctic
Mesozooplankton are heterotrophic organisms in the size range from 0.2 to 20 mm. Mesozooplankton move with ocean currents but can migrate vertically in the water column. Mesozooplankton generally feed on primary producers, microzooplankton and detritus particles. They are an important prey for fish larva and planktivorous fish and therefore represent an important link between primary producers and higher trophic levels.
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
Mesozooplankton are heterotrophic organisms in the size range from 0.2 to 20 mm. Mesozooplankton move with ocean currents but can migrate vertically in the water column. Mesozooplankton generally feed on primary producers, microzooplankton and detritus particles. They are an important prey for fish larva and planktivorous fish and therefore represent an important link between primary producers and higher trophic levels.
Datasets ID: H5
Partners:
BSH
Region: Baltic Sea
Mesozooplankton are heterotrophic organisms in the size range from 0.2 to 20 mm. Mesozooplankton move with ocean currents but can migrate vertically in the water column. Mesozooplankton generally feed on primary producers, microzooplankton and detritus particles. They are an important prey for fish larva and planktivorous fish and therefore represent an important link between primary producers and higher trophic levels.
Datasets ID: H1
Partners:
Moi
Region: Global
Mesozooplankton are heterotrophic organisms in the size range from 0.2 to 20 mm. Mesozooplankton move with ocean currents but can migrate vertically in the water column. Mesozooplankton generally feed on primary producers, microzooplankton and detritus particles. They are an important prey for fish larva and planktivorous fish and therefore represent an important link between primary producers and higher trophic levels.
Datasets ID: H36
Partners:
CLS
Region: Iberia-Biscay-Ireland
Micronekton is a group of marine organisms characterized by a size range from 2 to 20 cm. It gathers various taxa and encompasses crustaceans, fish, and cephalopods. It constitutes an intermediate compartment of the oceanic trophic web as it feeds on zooplankton and it is the main prey of larger marine predators. Micronekton is considered to be a key player in the biological pump. It performs diurnal vertical migration (DVM) based on predation pressure. These organisms migrate every day between the surface where they feed during the night, and the deep ocean where they hide from predators during the day.
Datasets ID: H15
Partners:
CLS
Region: Global
Micronekton is a group of marine organisms characterized by a size range from 2 to 20 cm. It gathers various taxa and encompasses crustaceans, fish, and cephalopods. It constitutes an intermediate compartment of the oceanic trophic web as it feeds on zooplankton and it is the main prey of larger marine predators. Micronekton is considered to be a key player in the biological pump. It performs diurnal vertical migration (DVM) based on predation pressure. These organisms migrate every day between the surface where they feed during the night, and the deep ocean where they hide from predators during the day.
Datasets ID: H36
Partners:
CLS
Region: Iberia-Biscay-Ireland
Suspended particulate matter (SPM) is a collective term for the inorganic (e.g., mineral) and organic (e.g., detritus; see next section) particulates that are suspended in the water column. It is an indicator of sediment transport, water clarity and quality; and has important implications for pelagic and benthic productivity and erosion. It can also act as a vector for the transfers of pollutants and contaminants.
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
Suspended particulate matter (SPM) is a collective term for the inorganic (e.g., mineral) and organic (e.g., detritus; see next section) particulates that are suspended in the water column. It is an indicator of sediment transport, water clarity and quality; and has important implications for pelagic and benthic productivity and erosion. It can also act as a vector for the transfers of pollutants and contaminants.
Datasets ID: H3
Partners:
UoL
Region: Black Sea
Particulate Organic Matter (POM) in the ocean is operationally defined as all combustible organic matter that can be retained on a filter (Kharbush et al. 2020). The filter mesh size is typically 0.7. It is often discussed in terms of Particulate Organic Carbon (POC), which reflects the important role POC plays in the ocean carbon cycle. The definition explicitly excludes Particulate Inorganic Carbon (PIC). The finite mesh size means the contribution of organisms smaller than 0.7 including most photosynthetic and non-photosynthetic prokaryotes is not captured in measurements. At the other end of the size spectrum, the contribution of large, motile zooplankton is also not measured. Such organisms are either intentionally removed through filtering, or through sampling techniques which are designed to exclude larger, swimming organisms. The operational definition of POM and POC contrasts with the definition used in most marine ecosystem and biogeochemical models. In marine ecosystem models, POM tends to be exclusively made up of non-living detrital material, including faecal pellets, the bodies of dead organisms, or other aggregations of organic matter.
Datasets ID: H4
Partners:
NERSC
Region: Arctic
Particulate Organic Matter (POM) in the ocean is operationally defined as all combustible organic matter that can be retained on a filter (Kharbush et al. 2020). The filter mesh size is typically 0.7. It is often discussed in terms of Particulate Organic Carbon (POC), which reflects the important role POC plays in the ocean carbon cycle. The definition explicitly excludes Particulate Inorganic Carbon (PIC). The finite mesh size means the contribution of organisms smaller than 0.7 including most photosynthetic and non-photosynthetic prokaryotes is not captured in measurements. At the other end of the size spectrum, the contribution of large, motile zooplankton is also not measured. Such organisms are either intentionally removed through filtering, or through sampling techniques which are designed to exclude larger, swimming organisms. The operational definition of POM and POC contrasts with the definition used in most marine ecosystem and biogeochemical models. In marine ecosystem models, POM tends to be exclusively made up of non-living detrital material, including faecal pellets, the bodies of dead organisms, or other aggregations of organic matter.
Datasets ID: H6
Partners:
OGS
Region: Mediterranean Sea
Particulate Organic Matter (POM) in the ocean is operationally defined as all combustible organic matter that can be retained on a filter (Kharbush et al. 2020). The filter mesh size is typically 0.7 It is often discussed in terms of Particulate Organic Carbon (POC), which reflects the important role POC plays in the ocean carbon cycle. The definition explicitly excludes Particulate Inorganic Carbon (PIC). The finite mesh size means the contribution of organisms smaller than 0.7 including most photosynthetic and non-photosynthetic prokaryotes is not captured in measurements. At the other end of the size spectrum, the contribution of large, motile zooplankton is also not measured. Such organisms are either intentionally removed through filtering, or through sampling techniques which are designed to exclude larger, swimming organisms. The operational definition of POM and POC contrasts with the definition used in most marine ecosystem and biogeochemical models. In marine ecosystem models, POM tends to be exclusively made up of non-living detrital material, including faecal pellets, the bodies of dead organisms, or other aggregations of organic matter.
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
Particulate Organic Matter (POM) in the ocean is operationally defined as all combustible organic matter that can be retained on a filter (Kharbush et al. 2020). The filter mesh size is typically 0.7. It is often discussed in terms of Particulate Organic Carbon (POC), which reflects the important role POC plays in the ocean carbon cycle. The definition explicitly excludes Particulate Inorganic Carbon (PIC). The finite mesh size means the contribution of organisms smaller than 0.7 including most photosynthetic and non-photosynthetic prokaryotes is not captured in measurements. At the other end of the size spectrum, the contribution of large, motile zooplankton is also not measured. Such organisms are either intentionally removed through filtering, or through sampling techniques which are designed to exclude larger, swimming organisms. The operational definition of POM and POC contrasts with the definition used in most marine ecosystem and biogeochemical models. In marine ecosystem models, POM tends to be exclusively made up of non-living detrital material, including faecal pellets, the bodies of dead organisms, or other aggregations of organic matter
Datasets ID: H5
Partners:
BSH
Region: Arctic
Dissolved Organic Matter (DOM) is dissolved matter originating from living matter that operationally is not retained by filtration. It can be produced in situ from phytoplankton, zooplankton and bacteria and can also be of terrestrial origin. It is further modified through bacterial utilisation. Dissolved organic carbon is often separated into different fractions based on decomposition timescales into labile, semi-labile, semi-refractory and refractory pools. Commonly the refractory pool is not included within models as its turnover time is on the order of 100-1000s of years.
Datasets ID: H4
Partners:
NERSC
Region: Arctic
Dissolved Organic Matter (DOM) is dissolved matter originating from living matter that operationally is not retained by filtration. It can be produced in situ from phytoplankton, zooplankton and bacteria and can also be of terrestrial origin. It is further modified through bacterial utilisation. Dissolved organic carbon is often separated into different fractions based on decomposition timescales into labile, semi-labile, semi-refractory and refractory pools. Commonly the refractory pool is not included within models as its turnover time is on the order of 100-1000s of years.
Datasets ID: H2
Partners:
UKMO
Region: North-West (NW) European Shelf
Dissolved Organic Matter (DOM) is dissolved matter originating from living matter that operationally is not retained by filtration. It can be produced in situ from phytoplankton, zooplankton and bacteria and can also be of terrestrial origin. It is further modified through bacterial utilisation. Dissolved organic carbon is often separated into different fractions based on decomposition timescales into labile, semi-labile, semi-refractory and refractory pools. Commonly the refractory pool is not included within models as its turnover time is on the order of 100-1000s of years.
Datasets ID: H5
Partners:
BSH
Region: Arctic
Reflectance (RRS) is the ratio of the electromagnetic flux reflected by a surface to the total electromagnetic flux incident on the surface. Water reflectance, as a function of the wavelength of electromagnetic radiation, provides useful information about the different types of suspended and dissolved components of matter in the ocean. It is used to identify various spectral features through the analysis of their inherent optical properties (i.e., absorption and backscattering). RRS is used to derive chlorophyll using empirical algorithms.
Datasets ID: O1
Partners:
CNR
Region: North-West (NW) European Shelf
Reflectance (RRS) is the ratio of the electromagnetic flux reflected by a surface to the total electromagnetic flux incident on the surface. Water reflectance, as a function of the wavelength of electromagnetic radiation, provides useful information about the different types of suspended and dissolved components of matter in the ocean. It is used to identify various spectral features through the analysis of their inherent optical properties (i.e., absorption and backscattering). RRS is used to derive chlorophyll using empirical algorithms.
Datasets ID: O2
Partners:
CNR
Region: Black Sea
Reflectance (RRS) is the ratio of the electromagnetic flux reflected by a surface to the total electromagnetic flux incident on the surface. Water reflectance, as a function of the wavelength of electromagnetic radiation, provides useful information about the different types of suspended and dissolved components of matter in the ocean. It is used to identify various spectral features through the analysis of their inherent optical properties (i.e., absorption and backscattering). RRS is used to derive chlorophyll using empirical algorithms.
Datasets ID: O3
Partners:
CNR
Region: Black Sea
Reflectance (RRS) is the ratio of the electromagnetic flux reflected by a surface to the total electromagnetic flux incident on the surface. Water reflectance, as a function of the wavelength of electromagnetic radiation, provides useful information about the different types of suspended and dissolved components of matter in the ocean. It is used to identify various spectral features through the analysis of their inherent optical properties (i.e., absorption and backscattering). RRS is used to derive chlorophyll using empirical algorithms.
Datasets ID: H6
Partners:
OGS
Region: Mediterranean Sea
The workshop, titled ‘Introduction to new capabilities in marine biogeochemical and ecosystem modelling,’ aimed to equip scientists of all levels with advanced models and tools. NECCTON’s involvement was crucial in providing insights into innovative ecosystem models, supporting both theoretical and practical sessions....
Learn moreOur team has delivered a number of insightful talks and presented informative posters, significantly contributing to the international ecosystem modelling community. This engagement has provided an excellent opportunity for networking and building collaborations with other researchers from around the world....
Learn moreNECCTON’s scientific lead, Stefano Ciavatta from Mercator Ocean joined the Conference to highlight NECCTONs contribution to tackle the challenges 2 (Protect and restore ecosystems and biodiversity), 3 (Sustainably feed the global population) and 5 (Unlock ocean-based solutions to climate change), as project endorsed by the UN Ocean Decade....
Learn more...
Learn moreNECCTON Project Endorsed by UN Ocean Decade Programme: Advancing Marine Biodiversity Conservation...
Learn moreThe project coordinator Stefano Ciavatta joined the second Digital Ocean Forum (DOF2), organized by the EU DG MARE and DG RTD, in Brussels on the 14th and 15th June 2023....
Learn more