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DiatomBase
Citable as data publication
Kociolek, J.P.; Blanco, S.; Coste, M.; Ector, L.; Liu, Y.; Karthick, B.; Kulikovskiy, M.; Lundholm, N.; Ludwig, T.; Potapova, M.; Rimet, F.; Sabbe, K.; Sala, S.; Sar, E.; Taylor, J.; Van de Vijver, B.; Wetzel, C.E.; Williams, D.M.; Witkowski, A.; Witkowski, J. (2022). DiatomBase. Accessed at https://www.diatombase.org on yyyy-mm-dd. https://doi.org/10.14284/504
Contact:
Kociolek, John Patrick
Availability: This dataset is licensed under a Creative Commons Attribution 4.0 International License.
Description
A world checklist of Diatoms, compiled by taxonomic experts and based on peer-reviewed literature. more
The diatoms are an amazing group of organisms, part of the Stremenopile lineage of life. These photosynthetic unicells (ranging from 1 µm to over 1 mm in size) have chlorophylls a and c, and a complement of accessory pigments that include xanthophylls and carotenoids, making the living cells golden-brown in color. They produce bipartite glass cell walls and their products from photosynthesis are lipids. Some have suggested diatoms have the most efficient photosynthetic machinery of any group of organisms. Diatoms are found in marine, estuarine and freshwater ecosystems, inhabiting a wide range of environmental conditions. Because they are found in almost any place that has, or has had, water, and due to their efficient photosynthetic processes, they are important players in the global cycling of carbon and oxygen. And because they require silicon dioxide for cell division, they are also important players in the global cycling of silica. So, despite their small size they are important components in resource cycling globally.
In most aquatic ecosystems, diatoms along with other algae are the base of the food chain. As primary producers, they are important links between the abiotic and biotic worlds. In that crucial position (in addition to their short generation times), they can be important indicators of environmental change (see below). Diatoms are preferentially selected by primary consumers, in part due to the rich oil they produce.
The group, overall, occupies tremendous ecological breadth. In inland systems, diatoms can be found all over the world, from the tropics to the poles, across a wide range of habitats included many lentic environments such as large to small lakes, bogs, springs and fens, and in lotic environments, from headwater streams to the mouth of great rivers. Along a temperature gradient, they have been recognized growing in ice, and are some of the first eukaryotes to be found in hot springs. In terms of salinity, they have been found in salty inland lakes, where the salinity can be several times greater that the ocean, and in some of the most dilute freshwaters. Diatoms are found in some of the most natural, pristine environments, and in the outfalls of primary sewage treatment plants. They have been found over eight orders of magnitude relative to hydrogen ion concentration, in very low pH waters (ca. 2.5 in acid mine drainage) to alkaline systems where the pH is above 10 (above this pH the silica in their cell walls dissolves).
Due to their siliceous cell walls, an extensive fossil record of diatoms has been developed, in both marine and freshwaters. The marine fossil diatom record extends back to the Jurassic. Fossil outcrops of the marine record occur on every continent, and many cores from the oceans, taken during the Deep-Sea Drilling program and Ocean Drilling Programs. There are many more genera of marine diatoms than freshwater diatoms. In the freshwater realm, the record is much younger, with the oldest known records occurring from the Eocene. Marine and freshwater deposits can be extensive in area and depth, and many economically-valuable resources are derived from these diatomaceous deposis.
In addition to these wide spectra of environmental conditions, diatoms occupy a wide range of physical niches in aquatic ecosystems. They have adaptations for existing in the plankton, floating or drifting near the surface of waters of lakes and large rivers. They are found in high-energy zones of shorelines and fast-flowing water, attached by a variety of mechanisms to stones, rocks, wood and other plant-life and algae. In more quiescent waters, diatoms can inhabit the benthic environment, either as resting spores or in some cases, those species with a raphe can move, micro-positioning themselves in the sediments or other substrates.
In addition to the physical and chemical components of the habitats where diatoms occur, there are biological elements as well. For example, diatoms may use different carbon sources and there are a few species that are entirely heterotrophic, living amongst the muco-polysaccharides of seaweeds. They may be involved in a variety of symbioses, either loose associations (for example inhabiting the mucilage of colonial protozoans), being harbored by organisms (such as dinoflagellates) or harboring blue-green algae (some diatoms even integrating their symbionts as nitrogen-fixing organelles).
Given the global distribution, wide ecological breadth, and important ecological roles, it should be no surprise that the diatoms are phylogenetically diverse. There have been over 75,000 named taxa in the group, and some estimates suggest there might exist over 200,000 species. One Order, the Bacillariales, for example, has more described species than all of the mammals combined.
While as a group the diatoms are widely distributed, individual species have their own preferences and tolerances to environmental conditions. Diatoms are quick responders to environmental change. Understanding individual species responses as well as community responses has been an underlying approach to using diatoms to study the status and trends of aquatic ecosystems. Diatoms have been used for more than a century to evaluate water quality and there is a tremendous body of literature on this topic across several continents and many countries, and this approach has been used for assessing current conditions in many freshwater, estuarine and marine environments. With fossils, as well as some long-term monitoring efforts, diatoms have been used not only to hindcast past conditions but to forecast trends of environmental change.
Applications of diatoms go far beyond water quality assessment. Their fossil remains (of marine and freshwater origin), known as diatomaceous earth, have many material applications, from insulation, to abrasives to filtration. Their ability to produce lipids via photosynthesis has drawn considerable attention to the use of diatoms as sources of renewable biofuels and the lipids cells for many times the price of petroleum as sources of Omega-3 oils as dietary supplements. They are being used in nanotechnology and medicine, both for their glass cell walls and for the bio-active products they produce.
Research interests with diatoms include nanotechnology, biodiversity and habitat conservation and, due to their temporal and spatial compactness, they are used to study ecological phenomenon both from theoretical and practical points of view. Molecular studies search to find and evaluate the genetic and physiological machinery for a wide range of activities, from oil production, to uptake and metabolism in responding to temperature and nutrient levels and fluctuations, to the transformation of genomes. And a revolution in our understanding of their phylogenetic relationships is taking shape, surely to upend classical approaches to their classification.
The diatoms are an amazing group of organisms, part of the Stremenopile lineage of life. These photosynthetic unicells (ranging from 1 µm to over 1 mm in size) have chlorophylls a and c, and a complement of accessory pigments that include xanthophylls and carotenoids, making the living cells golden-brown in color. They produce bipartite glass cell walls and their products from photosynthesis are lipids. Some have suggested diatoms have the most efficient photosynthetic machinery of any group of organisms. Diatoms are found in marine, estuarine and freshwater ecosystems, inhabiting a wide range of environmental conditions. Because they are found in almost any place that has, or has had, water, and due to their efficient photosynthetic processes, they are important players in the global cycling of carbon and oxygen. And because they require silicon dioxide for cell division, they are also important players in the global cycling of silica. So, despite their small size they are important components in resource cycling globally.
In most aquatic ecosystems, diatoms along with other algae are the base of the food chain. As primary producers, they are important links between the abiotic and biotic worlds. In that crucial position (in addition to their short generation times), they can be important indicators of environmental change (see below). Diatoms are preferentially selected by primary consumers, in part due to the rich oil they produce.
The group, overall, occupies tremendous ecological breadth. In inland systems, diatoms can be found all over the world, from the tropics to the poles, across a wide range of habitats included many lentic environments such as large to small lakes, bogs, springs and fens, and in lotic environments, from headwater streams to the mouth of great rivers. Along a temperature gradient, they have been recognized growing in ice, and are some of the first eukaryotes to be found in hot springs. In terms of salinity, they have been found in salty inland lakes, where the salinity can be several times greater that the ocean, and in some of the most dilute freshwaters. Diatoms are found in some of the most natural, pristine environments, and in the outfalls of primary sewage treatment plants. They have been found over eight orders of magnitude relative to hydrogen ion concentration, in very low pH waters (ca. 2.5 in acid mine drainage) to alkaline systems where the pH is above 10 (above this pH the silica in their cell walls dissolves).
Due to their siliceous cell walls, an extensive fossil record of diatoms has been developed, in both marine and freshwaters. The marine fossil diatom record extends back to the Jurassic. Fossil outcrops of the marine record occur on every continent, and many cores from the oceans, taken during the Deep-Sea Drilling program and Ocean Drilling Programs. There are many more genera of marine diatoms than freshwater diatoms. In the freshwater realm, the record is much younger, with the oldest known records occurring from the Eocene. Marine and freshwater deposits can be extensive in area and depth, and many economically-valuable resources are derived from these diatomaceous deposis.
In addition to these wide spectra of environmental conditions, diatoms occupy a wide range of physical niches in aquatic ecosystems. They have adaptations for existing in the plankton, floating or drifting near the surface of waters of lakes and large rivers. They are found in high-energy zones of shorelines and fast-flowing water, attached by a variety of mechanisms to stones, rocks, wood and other plant-life and algae. In more quiescent waters, diatoms can inhabit the benthic environment, either as resting spores or in some cases, those species with a raphe can move, micro-positioning themselves in the sediments or other substrates.
In addition to the physical and chemical components of the habitats where diatoms occur, there are biological elements as well. For example, diatoms may use different carbon sources and there are a few species that are entirely heterotrophic, living amongst the muco-polysaccharides of seaweeds. They may be involved in a variety of symbioses, either loose associations (for example inhabiting the mucilage of colonial protozoans), being harbored by organisms (such as dinoflagellates) or harboring blue-green algae (some diatoms even integrating their symbionts as nitrogen-fixing organelles).
Given the global distribution, wide ecological breadth, and important ecological roles, it should be no surprise that the diatoms are phylogenetically diverse. There have been over 75,000 named taxa in the group, and some estimates suggest there might exist over 200,000 species. One Order, the Bacillariales, for example, has more described species than all of the mammals combined.
While as a group the diatoms are widely distributed, individual species have their own preferences and tolerances to environmental conditions. Diatoms are quick responders to environmental change. Understanding individual species responses as well as community responses has been an underlying approach to using diatoms to study the status and trends of aquatic ecosystems. Diatoms have been used for more than a century to evaluate water quality and there is a tremendous body of literature on this topic across several continents and many countries, and this approach has been used for assessing current conditions in many freshwater, estuarine and marine environments. With fossils, as well as some long-term monitoring efforts, diatoms have been used not only to hindcast past conditions but to forecast trends of environmental change.
Applications of diatoms go far beyond water quality assessment. Their fossil remains (of marine and freshwater origin), known as diatomaceous earth, have many material applications, from insulation, to abrasives to filtration. Their ability to produce lipids via photosynthesis has drawn considerable attention to the use of diatoms as sources of renewable biofuels and the lipids cells for many times the price of petroleum as sources of Omega-3 oils as dietary supplements. They are being used in nanotechnology and medicine, both for their glass cell walls and for the bio-active products they produce.
Research interests with diatoms include nanotechnology, biodiversity and habitat conservation and, due to their temporal and spatial compactness, they are used to study ecological phenomenon both from theoretical and practical points of view. Molecular studies search to find and evaluate the genetic and physiological machinery for a wide range of activities, from oil production, to uptake and metabolism in responding to temperature and nutrient levels and fluctuations, to the transformation of genomes. And a revolution in our understanding of their phylogenetic relationships is taking shape, surely to upend classical approaches to their classification.
Scope
Themes:
Biology, Biology > Benthos, Biology > Ecology - biodiversity, Biology > Plankton
Keywords:
Marine/Coastal, Fresh water, Brackish water, Classification, Species, Taxonomy, World Waters, Bacillariophyceae
Geographical coverage
World Waters [Marine Regions]
Temporal coverage
From 1758 on [In Progress]
Taxonomic coverage
Bacillariophyceae [WoRMS]
Parameters
Taxonomy
Contributors
Guerrero, José María, taxonomic editor
Lamaro, Anabel, taxonomic editor
Vouilloud, Amelia Alejandra, taxonomic editor
Kociolek, John Patrick, data creator, data manager, taxonomic editor
Blanco, Saúl, data creator, taxonomic editor
Coste, Michel, data creator, taxonomic editor
Ector, Luc, data creator, taxonomic editor
Liu, Yan, data creator, taxonomic editor
Karthick, Balasubramanian, data creator, taxonomic editor
Kulikovskiy, Maxim, data creator, taxonomic editor
Lundholm, Nina, data creator, taxonomic editor
Ludwig, Thelma Veiga, data creator, taxonomic editor
Potapova, Marina, data creator, taxonomic editor
Rimet, Frédéric, data creator, taxonomic editor
Sabbe, Koen, data creator, taxonomic editor
Sala, Silvia Estela, data creator, taxonomic editor
Sar, Eugenia, data creator, taxonomic editor
Taylor, Jonathan, data creator, taxonomic editor
Van de Vijver, Bart
Wetzel, Carlos Eduardo, data creator, taxonomic editor
Williams, David M., data creator, taxonomic editor
Witkowski, Andrzej
Witkowski, Jakub, data creator, taxonomic editor
Flanders Marine Institute (VLIZ), more, database developer
Thirouin, Kevin, taxonomic editor
Related datasets
Published in:
WoRMS: World Register of Marine Species, more
Project
LifeWatch: Flemish contribution to LifeWatch.eu
WoRMS: World Register of Marine Species
Dataset status: In Progress
Data type: Data
Data origin: Literature research
Metadatarecord created: 2017-08-22
Information last updated: 2024-01-11