Earth's Biosphere Research Articles

Research on Collaborative Innovation Path and Strategy of China's Marine Industry Chain

Ding, D.; Gao, Q., and Wang, Z.C., 2020. Research on collaborative innovation path and strategy of China's marine industry chain. In: Bai, X. and Zhou, H. (eds.), Advances in Water Resources, Environmental Protection, and Sustainable Development. Journal of Coastal Research, Special Issue No. 115, pp. 229-231. Coconut Creek (Florida), ISSN 0749-0208.With the continuous development of economic globalization and the continuous progress of science and technology, industrial competition and market competition are becoming more and more fierce. Technological innovation has become an important force to promote national industrial development and economic progress. Faced with the rapid population growth and the increasing shortage of various land resources, making full use of marine resources has become an inevitable choice for China's economic development. The ocean is one of the most important ecosystems in the earth's biosphere and the birthplace of human civilization. In order to ensure the smooth implementation of the established industrial chain development mechanism, we must take corresponding countermeasures to solve various problems that may occur in the implementation process. The eco-environmental cost of marine development activities cannot be effectively compensated, which leads to a series of marine eco-environmental problems. Under the contradiction between economic development and the shortage of energy, space and other resources, human beings gradually turn the focus of economic development strategy to the ocean, which puts forward higher requirements for the development and utilization of marine industry chain.

Seismic response of canisters embedded in a repository analyzed through centrifuge modeling

High-level waste (HLW), one of the most poisonous materials known to science, includes spent fuel from nuclear power plants. Therefore, nuclear engineers seek to isolate HLW from the Earth's biosphere by using multibarrier systems, including engineered and natural barriers deep below the surface of the earth. Typically, disposal holes are drilled into intact rocks. Canisters and buffer materials are then placed in the drilled holes. These highly stable canisters should not be easily affected by the natural environment, human activities, and tectonic movement. However, Taiwan is located in the Ring of Fire of the Pacific Ocean; thus, earthquakes threaten Taiwan frequently. Consequently, scholarly investigations must expand knowledge regarding the effects of earthquake-induced vibration on the canisters and buffer materials placed in the drilled holes and on the disposal system. This study assumes that the relevant disposal holes are created in granite deposit layers and have no deformations and cracks. The methods and geometry of the KBS-3 V system were examined; in this study a physical apparatus one-tenth the size of the KBS-3 V system was designed. The one-tenth-scale physical apparatus was subjected to an artificial acceleration field of 10 g as a simulation of the in-situ stress between the canisters and buffer material. The physical model was positioned on a shaking table and subjected to simulated seismic events. During shaking, sensors measured the acceleration, pore water pressure, and total pressure values to determine the interactive behavior between canisters and buffer materials during seismic activity. Six models were developed with different initial water content and hydration conditions; these models simulated the state of the buffer material after construction, after underground water invasion of the disposal hole, and after saturation of the buffer material. After centrifuge modeling had been conducted, the container was disassembled to check for crack development in the surrounding buffer material. The results can be used to distinguish the difference between each stage of buffer blocks and to determine the behavior of canisters during shaking; thus, these results can be employed to design HLW repositories in seismically active zones.

Widespread energy limitation to life in global subseafloor sediments.

Microbial cells buried in subseafloor sediments comprise a substantial portion of Earth's biosphere and control global biogeochemical cycles; however, the rate at which they use energy (i.e., power) is virtually unknown. Here, we quantify organic matter degradation and calculate the power utilization of microbial cells throughout Earth's Quaternary-age subseafloor sediments. Aerobic respiration, sulfate reduction, and methanogenesis mediate 6.9, 64.5, and 28.6% of global subseafloor organic matter degradation, respectively. The total power utilization of the subseafloor sediment biosphere is 37.3 gigawatts, less than 0.1% of the power produced in the marine photic zone. Aerobic heterotrophs use the largest share of global power (54.5%) with a median power utilization of 2.23 × 10-18 watts per cell, while sulfate reducers and methanogens use 1.08 × 10-19 and 1.50 × 10-20 watts per cell, respectively. Most subseafloor cells subsist at energy fluxes lower than have previously been shown to support life, calling into question the power limit to life.

Assessment of the water facilities’ impact types on the basin geosystems’ geosphere during construction and operation

Water resources use as a renewable natural resource on all hierarchical basin geosystems levels of within the Earth biosphere, in almost all types of economic and other activities carried out by intra-basin or inter-basin water flow regulation and redistribution (surface, underground), quantitative and qualitative indicators, formed within the spatial limits of the basin system under consideration. For the water flow regulation within the considered river hydrographic seasonal or multi-year regulation network, the reservoirs are built, including the necessary complex hydrotechnical and related facilities, providing the selection of the estimated water flow (Q m3 / s) from water body with a subsequent transportation to specific water users and water consumers. For water resources use in various sectors of economic and other activities within about 10 of the basin geosystems in the Kuban, Terek and Lower Don rivers water facilities were built last century. According to the current regulatory environmental requirements at the design stage, construction and subsequent operation an urgent need to carry out the environmental impact assessment of water facilities arose. The construction objects referred to as “Facilities” and related to the water use with a systematic approach as a way to describe the processes of interconnection, interaction and the relationship between the natural, man-made components and the population developed the methodology foundations for creating and developing a class of natural-technical systems “Environment - Facility – Population” on the water resources use in the economic activity industries. The developed methodology basis for this class of natural-technical systems found practical application at the design, construction and operation stages water objects of activity, referred to as “Facilities”, with the implementation of the existing regulatory environmental requirements. In the methodology foundations development for the creation and development of this class the natural-technical systems, the concept of the dominant role of the whole was formulated, which defines the dominant effect of natural processes in the water flow formation (surface, underground) in the zones of “Facility” influence within the considered basin geosystem. For the considered class of systems according to the study results, such basic system concepts as structure, component, element, the dominant role of the whole, including the concept of natural and technogenic components as well as the environmental acceptability are defined.

Astrochronology of the Ediacaran Shuram carbon isotope excursion, Oman

The Ediacaran is a highly dynamic period in terms of large perturbations in Earth's atmosphere, biosphere, and climate. Among these perturbations, a pronounced negative carbon isotope excursion, known as the Shuram excursion (SE), is characterized by the most depleted δ13C values (-12‰) that have ever been observed in the geological record. A poorly determined chronostratigraphic framework makes the SE difficult to correlate and compare globally. Therefore, it is hard to study the potential connection between the SE and coeval climate and biological variations. Here, we present a high-resolution astrochronological study of the Ediacaran Shuram and Buah Formations, Nafun Group, Oman, in which the SE is reported for the first time. Power spectral analysis of the 600-m long gamma ray log of the Miqrat-1 Well shows that a hierarchy of astronomically-forced climate cycles (eccentricity, obliquity, and precession) is accurately-preserved. Using multiple statistical tests, we constructed a sedimentation rate variation profile that covers the entire SE, which is characterized by low rates in shale-dominated layers and high rates in shale-carbonate interbedded layers. The duration of the SE in Oman is suggested to be 7.7 ± 0.2 Myr, which agrees with estimates from South Australia, South China, and the United States. An identical duration of the SE supports its global synchroneity and indicates a primary origin of the depleted δ13C values. Combined with the newly proposed termination age (562.5 ± 1.1 Ma) of the SE, our astrochronological results suggest that the onset age of the excursion is 570.2 ± 1.1 Ma. The astrochronology of the SE delineates the tempo of the excursion, with a rapid decrease (∼ 1 Myr) from the onset to its isotopic nadir followed by a more gradual recovery (∼ 6–7 Myr) towards the termination. The new chronostratigraphic framework permits further investigations of the potential causal links between the global carbon cycle and the widespread glaciation, the oceanic oxygenation, and the biological diversification in Ediacaran time.

Galactic Factors, the Young Sun, the Earth, and the Biophysics of Living Systems

The effects of radiation from the young Sun and galactic cosmic rays on the physical conditions on the early Earth are significantly underestimated in studies of the problems related to the origin and evolution of the biosphere. This review considers the dynamics of solar and galactic processes over the 4.56 billion years of the existence of the Solar System. These factors substantially affected the development of adaptive technologies in ancient and modern living systems. The features of biosphere development are considered for the early Earth under the young Sun, which was fainter, but more flare active. The radiation spectrum of the young Sun is discussed together with the paradoxical mismatch between the solar radiation spectrum and the chlorophyll adsorption spectrum. Ways of solving the paradox are proposed. The role of solar radiation is important when studying models of the early biosphere of the Earth and hypothetical biospheres of giant planet satellites and exoplanets.

Seismic Soundoff

The following is an excerpt from SEG's podcast, Seismic Soundoff. In episode 79, host Andrew Geary highlights Estella Atekwana's upcoming virtual course, “Biogeophysics: Exploring earth's subsurface biosphere using geophysical approaches.” Atekwana explains how geophysical tools helped develop biogeophysics, why microorganisms play an important role on earth, how her research applies to the search for life on other planets, and why flexibility is the key to a successful career. Listen to the full episode at https://seg.org/podcast/post/9011 .

Primary Forests Are Undervalued in the Climate Emergency

Scientists are increasingly alarmed by the accelerating climate and biodiversity crises, as, for example, Ripple and colleagues (2020), recently published in BioScience and signed by three of us (DAD, BM, BR) during the initiating letter. However, decision-makers rarely recognize the inextricable link between biodiversity and climate change. We cannot solve one without the other. Earth's biosphere contains enormous carbon stocks that have the potential to fundamentally alter the trajectory of climate change. Biodiversity is crucial for stabilizing these carbon stocks and keeping them out of the atmosphere.

Sicilian serpentinite xenoliths containing abiotic organics with nanodiamond clusters as key model for prebiotic processes

Rock fragments from the deepest parts of a buried hydrothermal system belonging to the Mesozoic Tethys Ocean entered as xenoliths in a Miocenic diatreme, hence brought to the surface, in the Hyblean Plateau (Sicily). Some xenoliths consist of strongly serpentinized ultramafic rocks bearing blebs of abiotic organic matter, where clusters of amorphous carbon nanoparticles, including nanodiamonds, are immersed. Such an occurrence conjures up established hypotheses that diamond surfaces are suitable catalytic platforms stimulating the assemblage of complex bio-organic molecules relevant to the emergence of life on Earth. The appearance of bio-organic molecules under primitive Earth conditions is one of the major unsolved questions on the origin of life. Here we report new micro-Raman spectra on blebs of abiotic organic matter from a selected xenolith. Diamond bands were related to hydrogenated nanocrystalline diamonds, with size of nearly 1–1.6 ​nm, formed from organics at low pressures and temperatures. In particular, diamond surfaces can give rise to crystalline interfacial water layers that may have played a fundamental role in the early biosphere evolution as a good medium for rapidly transporting positive charges in the form of hydrated protons. Nowadays, proton gradients in alkaline hydrothermal vents along oceanic ridges are generally viewed as key pre-biotic factors. In general, serpentinites span the entire geological record, including prebiotic times. These hydrous ultramafic rocks often display evidence of abiotic carbon species, both organic and inorganic, including nanodiamonds, being also capable to give rise to chemiosmotic processes and proton gradients necessary to the organisms, such as the “Last Universal Common Ancestor” (LUCA), in the prebiotic Earth.

Characterization and comparison of groundwater quality and redox conditions in the Arakawa Lowland and Musashino Upland, southern Kanto Plain of the Tokyo Metropolitan area, Japan

Groundwater is essential for the Earth biosphere but is often contaminated by harmful chemical compounds due to both anthropogenic and natural causes. A key factor controlling the fate of harmful chemicals in groundwater is the reduction/oxidation (redox) conditions. The formation factors for the groundwater redox conditions are insufficiently understood. In this study, long-term groundwater quality beneath one of the world megacities was monitored and evaluated. We measured and compared hydrogeochemical conditions including groundwater quality (35 chemical parameters) and redox conditions of five aquifers in the Arakawa Lowland and Musashino Upland, southern Kanto Plain of the Tokyo Metropolitan area, Japan. Monitoring results suggested the following: The main origin of groundwater is precipitation in both the Lowland and Upland areas. The three aquifers in the Arakawa Lowland are likely fully separated, with one unconfined and two confined aquifers under iron reducing and methanogenic conditions, respectively. Oppositely, in the Musashino Upland, the water masses in the two aquifers are likely partly connected, under aerobic conditions, and undergoing the same groundwater recharge and flow processes under similar hydrogeological conditions. The different groundwater redox conditions observed are likely caused by the very different groundwater residence times for the Arakawa Lowland and Musashino Upland.

The impact of marine nutrient abundance on early eukaryotic ecosystems.

The rise of eukaryotes to ecological prominence represents one of the most dramatic shifts in the history of Earth's biosphere. However, there is an enigmatic temporal lag between the emergence of eukaryotic organisms in the fossil record and their much later ecological expansion. In parallel, there is evidence for a secular increase in the availability of the key macronutrient phosphorus (P) in Earth's oceans. Here, we use an Earth system model equipped with a size-structured marine ecosystem to explore relationships between plankton size, trophic complexity, and the availability of marine nutrients. We find a strong dependence of planktonic ecosystem structure on ocean nutrient abundance, with a larger ocean nutrient inventory leading to greater overall biomass, broader size spectra, and increasing abundance of large Zooplankton. If existing estimates of Proterozoic marine nutrient levels are correct, our results suggest that increases in the ecological impact of eukaryotic algae and trophic complexity in eukaryotic ecosystems were directly linked to restructuring of the global P cycle associated with the protracted rise of surface oxygen levels. Our results thus suggest an indirect but potentially important mechanism by which ocean oxygenation may have acted to shape marine ecological function during late Proterozoic time.

Microbial chemolithotrophy mediates oxidative weathering of granitic bedrock

The flux of solutes from the chemical weathering of the continental crust supplies a steady supply of essential nutrients necessary for the maintenance of Earth's biosphere. Promotion of weathering by microorganisms is a well-documented phenomenon and is most often attributed to heterotrophic microbial metabolism for the purposes of nutrient acquisition. Here, we demonstrate the role of chemolithotrophic ferrous iron [Fe(II)]-oxidizing bacteria in biogeochemical weathering of subsurface Fe(II)-silicate minerals at the Luquillo Critical Zone Observatory in Puerto Rico. Under chemolithotrophic growth conditions, mineral-derived Fe(II) in the Rio Blanco Quartz Diorite served as the primary energy source for microbial growth. An enrichment in homologs to gene clusters involved in extracellular electron transfer was associated with dramatically accelerated rates of mineral oxidation and adenosine triphosphate generation relative to sterile diorite suspensions. Transmission electron microscopy and energy-dispersive spectroscopy revealed the accumulation of nanoparticulate Fe-oxyhydroxides on mineral surfaces only under biotic conditions. Microbially oxidized quartz diorite showed greater susceptibility to proton-promoted dissolution, which has important implications for weathering reactions in situ. Collectively, our results suggest that chemolithotrophic Fe(II)-oxidizing bacteria are likely contributors in the transformation of rock to regolith.

The liquid synergetic decontamination on the atmospheric electricity principles

The article is devoted to the liquid substances’ disinfection nature-like technology synergistic aspects on the atmospheric electricity impact principles on the Earth's biosphere. In the thesis form, a method, technological aspects, the disinfected liquid interaction synergistic moments with the proposed device reproducible blocks effects are suggested. It is proved that on the synergistic interactions’ basis, the greening production processes in developing new areas efficiency increases dramatically.

Viruses as a survival strategy in the armory of life.

Viruses have generally been thought of as infectious agents. New data on mimivirus, however, suggests a reinterpretation of this thought. Earth's biosphere seems to contain many more viruses than previously thought and they are relevant in the maintenance of ecosystems and biodiversity. Viruses are not considered to be alive because they are not free-living entities and do not have cellular units. Current hypotheses indicate that some viruses may have been the result of genomic reduction of cellular life forms. However, new studies relating to the origins of biological systems suggest that viruses could also have originated during the transition from First to the Last Universal Common Ancestor (from FUCA to LUCA). Within this setting, life has been established as chemical informational system and could be interpreted as a macrocode of multiple layers. The first entity to acquire these features was the First Universal Common Ancestor (FUCA) that evolved to an intermediate ancestral that could be named T-LUCA (Transitional-LUCA) and be equated to Woese's concept of progenotes. T-LUCA may have remained as undifferentiated subsystems with viruses-like structures. The net result is that both cellular life forms and viruses shared protein synthesis apparatuses. In short, virus is a strategy of life reached by two paths: T-LUCAs like entities and the reduction of cellular life forms.

When Did Life Likely Emerge on Earth in an RNA‐First Process?

AbstractThe widespread presence of ribonucleic acid (RNA) catalysts and cofactors in the Earth′s biosphere today suggests that RNA was the first biopolymer to support Darwinian evolution. However, most “path‐hypotheses” to generate building blocks for RNA require reduced nitrogen‐containing compounds not made in useful amounts in the CO2−N2−H2O atmospheres of the Hadean. We review models for Earth′s impact history that invoke a single ∼1023 kg impactor (Moneta) to account for measured amounts of platinum, gold, and other siderophilic (“iron‐loving”) elements on the Earth and Moon. If it were the last sterilizing impactor, by reducing the atmosphere but not the mantle Moneta, would have opened a “window of opportunity” for RNA synthesis, a period when RNA precursors rained from the atmosphere onto land holding oxidized minerals that stabilize advanced RNA precursors and RNA. Surprisingly, this combination of physics, geology, and chemistry suggests a time when RNA formation was most probable, ∼120±100 million years after Moneta′s impact, or ∼4.36±0.1 billion years ago. Uncertainties in this time are driven by uncertainties in rates of productive atmosphere loss and amounts of sub‐aerial land.

A round Earth for climate models

Sunlight drives the Earth's weather, climate, chemistry, and biosphere. Recent efforts to improve solar heating codes in climate models focused on more accurate treatment of the absorption spectrum or fractional clouds. A mostly forgotten assumption in climate models is that of a flat Earth atmosphere. Spherical atmospheres intercept 2.5 W⋅m-2 more sunlight and heat the climate by an additional 1.5 W⋅m-2 globally. Such a systematic shift, being comparable to the radiative forcing change from preindustrial to present, is likely to produce a discernible climate shift that would alter a model's skill in simulating current climate. Regional heating errors, particularly at high latitudes, are several times larger. Unlike flat atmospheres, constituents in a spherical atmosphere, such as clouds and aerosols, alter the total amount of energy received by the Earth. To calculate the net cooling of aerosols in a spherical framework, one must count the increases in both incident and reflected sunlight, thus reducing the aerosol effect by 10 to 14% relative to using just the increase in reflected. Simple fixes to the current flat Earth climate models can correct much of this oversight, although some inconsistencies will remain.

Productivity and Community Composition of Low Biomass/High Silica Precipitation Hot Springs: A Possible Window to Earth's Early Biosphere?

Terrestrial hot springs have provided a niche space for microbial communities throughout much of Earth’s history, and evidence for hydrothermal deposits on the Martian surface suggest this could have also been the case for the red planet. Prior to the evolution of photosynthesis, life in hot springs on early Earth would have been supported though chemoautotrophy. Today, hot spring geochemical and physical parameters can preclude the occurrence of oxygenic phototrophs, providing an opportunity to characterize the geochemical and microbial components. In the absence of the photo-oxidation of water, chemoautotrophy in these hot springs (and throughout Earth’s history) relies on the delivery of exogenous electron acceptors and donors such as H2, H2S, and Fe2+. Thus, systems fueled by chemoautotrophy are likely energy substrate-limited and support low biomass communities compared to those where oxygenic phototrophs are prevalent. Low biomass silica-precipitating systems have implications for preservation, especially over geologic time. Here, we examine and compare the productivity and composition of low biomass chemoautotrophic versus photoautotrophic communities in silica-saturated hot springs. Our results indicate low biomass chemoautotrophic microbial communities in Yellowstone National Park are supported primarily by sulfur redox reactions and, while similar in total biomass, show higher diversity in anoxygenic phototrophic communities compared to chemoautotrophs. Our data suggest productivity in Archean terrestrial hot springs may be directly linked to redox substrate availability, and there may be high potential for geochemical and physical biosignature preservation from these communities.

Direct Cell Mass Measurements Expand the Role of Small Microorganisms in Nature.

Microbial biomass is a key parameter needed for the quantification of microbial turnover rates and their contribution to the biogeochemical element cycles. However, estimates of microbial biomass rely on empirically derived mass-to-volume relationships, and large discrepancies exist between the available empirical conversion factors. Here we report a significant nonlinear relationship between carbon mass and cell volume ([Formula: see text]; [Formula: see text]) based on direct cell mass, volume, and elemental composition measurements of 12 prokaryotic species with average volumes between 0.011 and 0.705 μm3 The carbon mass density of our measured cells ranged from 250 to 1,800 fg of C μm-3 for the measured cell volumes. Compared to other currently used models, our relationship yielded up to 300% higher carbon mass values. A compilation of our and previously published data showed that cells with larger volumes (>0.5 μm3) display a constant (carbon) mass-to-volume ratio, whereas cells with volumes below 0.5 μm3 exhibit a nonlinear increase in (carbon) mass density with decreasing volume. Small microorganisms dominate marine and freshwater bacterioplankton as well as soils and marine and terrestrial subsurface. The application of our experimentally determined conversion factors will help to quantify the true contribution of these microorganisms to ecosystem functions and global microbial biomass.IMPORTANCE Microorganisms are a major component of Earth's biosphere, and their activity significantly affects the biogeochemical cycling of bioavailable elements. To correctly determine the flux of carbon and energy in the environment, reliable estimates of microbial abundances and cellular carbon content are necessary. However, accurate assessments of cellular carbon content and dry weight are not trivial to obtain. Here we report direct measurements of cell dry and carbon mass of environmentally relevant prokaryotic microorganisms using a microfluidic mass sensor. We show a significant nonlinear relationship between carbon mass and cell volume and discuss this relationship in the light of currently used cellular mass models.

A New Frontier for Palaeobiology: Earth's Vast Deep Biosphere

Diverse micro-organisms populate a global deep biosphere hosted by rocks and sediments beneath land and sea, containing more biomass than any other biome except forests. This paper reviews an emerging palaeobiological archive of these dark habitats: microfossils preserved in ancient pores and fractures in the crust. This archive, seemingly dominated by mineralized filaments (although rods and coccoids are also reported), is presently far too sparsely sampled and poorly understood to reveal trends in the abundance, distribution, or diversity of deep life through time. New research is called for to establish the nature and extent of the fossil record of Earth's deep biosphere by combining systematic exploration, rigorous microanalysis, and experimental studies of both microbial preservation and the formation of abiotic pseudofossils within the crust. It is concluded that the fossil record of Earth's largest microbial habitat may still have much to tell us about the history of life, the evolution of biogeochemical cycles, and the search for life on Mars.

Mainstreaming Molecular Biodiversity: A call for a unified and interoperable framework

Over the past 20 years, immense progress has been made in enhancing the effectiveness, affordability, and deployability of molecular methods for biodiversity assessment and monitoring. From the micro- to macroscopic scale, methods such as amplicon sequencing of phylogenetic marker genes, metagenomics, and metatranscriptomics have greatly impacted biology and ecology, and are steadily being integrated into national and international biodiversity policy. Over the next decade, technologies such as miniaturised and autonomous DNA sequencing platforms will amplify this momentum, ushering in an unprecedented volume of deeply minable biodiversity information. While production-grade resources exist to standardise, archive, and exchange raw molecular data (e.g. the resources of the International Nucleotide Sequence Database Collaboration (INSDC) for DNA and RNA sequences), there are still no equivalent frameworks for biodiversity information derived from molecular methods. Research infrastructures in both the biodiversity and molecular biology domains must fill this gap with great urgency to channel molecular advances into efforts to understand and sustain Earth's imperilled biosphere. This session seeks to accelerate the implementation of global standards to link molecular biodiversity data to taxonomy-based systems. Only with these in place can we realise a robust, distributed, yet fully interoperating, network of infrastructures, projects, and researchers addressing molecular biodiversity. This introductory series of flash talks will present the rationale and goals of the session, alongside a joint vision from representatives of several convening stakeholders. A contribution from ELIXIR, an intergovernmental organisation of distributed infrastructures for biological data, will demonstrate the high readiness of biological data resources such as the European Nucleotide Archive (ENA) to mobilise molecular data along new standards. An intervention from the SILVA rRNA database project - itself an ELIXIR Core Data Resource - will note the actionability of interfacing molecular-based phylogenies with Linnaean systems hosted by partners such as the Global Biodiversity Information Facility (GBIF). Two more contributions will emphasise the essential role (and thus critical need) of molecular biodiversity standards in bridging research and operations. The first will focus on the nation-scale Metagenomics-Based Ecosystem Biomonitoring (EcoBiomics) project in Canada, which is using 'omic approaches to better assess, monitor, and remediate microbial and invertebrate biodiversity in soil and aquatic ecosystems, thus sustaining ecosystem resilience and service provision upon which society and economies depend. The second will underscore the need for international and stable standards to advance the long-term mission of the Global Omics Observatory Network (GLOMICON), and its contribution to the Global Ocean Observing System's Essential Ocean Variables (GOOS EOVs) under the Intergovernmental Oceanographic Commission of the United Nations Educational, Scientific, and Cultural Organization (IOC-UNESCO). Collectively, these contributions will make the case for a concerted effort to expedite the principled creation of operational information standards in molecular biodiversity. We invite all stakeholders to join us in implementing these standards in the coming years.