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Humans will always have oxygen to breathe, but we can’t say the same for ocean life

There is nothing more fundamental to humans than the availability of oxygen. We give little thought to the oxygen we need, we just breathe, but where does it come from?

To shed light on this, statements such as “the ocean provides 50% of the oxygen we breathe”, or its equivalent, “every second breath we breathe comes from the ocean”, have become common mantras to highlight human dependence on the ocean and the risk of lower oxygen supply due to climate change and environmental degradation.

These mantras are repeated by high-profile politicians, including US climate envoy John Kerry and French president Emmanuel Macron, international organisations such as Unesco and the European Commission, and even prominent reports from the IPCC and other reputable scientific institutions.

While they may be good fodder for speeches, these claims misrepresent where the oxygen we breathe actually comes from, and in doing so, mislead the public as to why we should step up our role as ocean custodians.

Where do we get our oxygen?

The Earth’s atmosphere has not always been as rich in oxygen as it is today. The atmosphere is now made up of 21% oxygen, but it accounted for just 0.001% of today’s levels during the first 2 billion years of Earth’s history.

It is the advent of microscopic ocean bacteria and plants (phytoplankton) and, later, larger plants on land which caused the staggering increase of oxygen in our atmosphere. This oxygen is derived from photosynthesis – the process by which plants turn carbon dioxide and water into organic matter and oxygen.

Oxygen has been relatively stable at a high level for the past 500 million years. Today, roughly half of photosynthesis takes place in the ocean and half on land.

So yes, the ocean is responsible for about 50% of the oxygen produced on the planet. But it’s not responsible for 50% of the air we humans breathe. Most of the oxygen produced by the ocean is directly consumed by the microbes and animals that live there, or as plant and animal products fall to the seafloor. In fact, the net production of oxygen in the ocean is close to 0.

Figure legend. Oxygen budget for the period 1960-2014 (redrawn from Grégoire et al., 2019)
Oxygen produced by photosynthesis (i.e. net primary production) in the upper ocean is roughly consumed by respiration within the water column, except for a small excess production of 0.002 Pmol O2 per year which corresponds to burial in the ocean floor. Redrawn from Grégoire et al., 2019, Fourni par l’auteur

A tiny fraction of the primary production, roughly 0.1%, escapes degradation and is stored as organic carbon in marine sediments – a process referred to as the biological carbon pump. This organic carbon may eventually turn into fossil fuels such as coal, oil and gas. The tiny amount of oxygen which had been generated to produce this carbon store can later be released to the atmosphere. A similar process occurs on land too, with some carbon stored in soils.

Therefore, the oxygen we currently breathe comes from the slow accumulation of O2 in the atmosphere supported by the burial of organic matter over very long time-scales – hundreds of millions of years – and not from the contemporary production by either the land or ocean biosphere.

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‘You can’t have a healthy planet without a healthy ocean’: interview with UN Special Envoy for the Ocean

The United Nations’ Special Envoy for the Ocean said we need to take more drastic measures to improve the health of our ocean.
Image: Unsplash/Naja Bertolt Jensen
  • The UN’s IPCC report said climate change is widespread, rapid and intensifying.
  • Detailed plans to cut greenhouse gas emissions and concrete commitments to invest in a sustainable blue economy are what’s needed, United Nations’ Special Envoy for the Ocean Peter Thomson said in an interview.
  • “You can’t have a healthy planet without a healthy ocean,” he said.
  • Ongoing changes to the ocean include warming, marine heatwaves, acidification and reduced oxygen levels.
  • Officials attending the COP26 climate summit need to increase their ambition, he said.

“Ramp it up” and “deliver us from this nightmare.”

That’s the message Peter Thomson, the United Nations’ Special Envoy for the Ocean and and Co-Chair of Friends of Ocean Action, is sending to global leaders as they head to a crucial climate summit in November.

Detailed plans to cut greenhouse gas emissions and concrete commitments to invest in a sustainable blue economy are what’s needed to slow the decline in ocean health and put a brake on human damage to the planet, he said.

“You can’t have a healthy planet without a healthy ocean,” Thomson said. “The big emitters have to face up to the fact that they are poisoning us all. They are the ones who have to take the lead on drastically cutting their emissions.”

Climate code red

His comments came after a major report from the UN’s Intergovernmental Panel on Climate Change confirmed ongoing changes to the ocean, including warming, more frequent marine heatwaves, acidification and reduced oxygen levels. The wide-ranging assessment of human impact on the planet said climate change is widespread, rapid and intensifying. UN Secretary General António Guterres called it a “code red for humanity.”

“The report is a huge alarm call for us all,” Thomson said. “From the ocean’s perspective, everything is connected. Think of it as one bathtub. So, what’s flowing off the Greenland ice sheet is causing a rising sea level in an atoll republic. If you’re burning coal to get your electricity, you’re contributing to the drowning of an age-old island culture.”

Once a support for the planet as a key absorber of carbon, the ocean is now at grave risk.

Warming, acidification, deoxygenation, changing circulation patterns and rising sea levels threaten marine life and ecosystems and put at risk the future ability of the seas to indirectly support life on Earth, Thomson said.

“We can see there are going to be increasing marine heatwaves and this, along with acidification, really puts the survival of tropical coral reefs in particular into jeopardy,” he said.

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A surface ocean CO2 monitoring strategy

Catalyse and facilitate the development of an internationally-agreed strategy for monitoring surface ocean CO2 globally and build on existing observing programmes, data management structures, and coordination bodies to create a global surface monitoring CO2 network capable of responding to the needs of global and regional policy drivers including the UNFCCC Global Stocktake. This activity contributes to G7 FSOI Action Areas 1, 3, and 4.

The G7 FSOI Coordination Centre will provide support for the GOOS Biogeochemistry Panel and build on existing international groups SOCONET and SOCAT to:

  • Develop an internationally-agreed observing strategy required to determine net ocean- atmosphere fluxes to an accuracy of 10% or better regionally and globally, and to monitor global ocean acidification, building on existing infrastructures and making best use of the combination of in situ observing platforms, satellite data, and models to fill gaps.
  • Develop international agreements on the system components required to support the observing network, including data management and global coordination support.
  • Develop a roadmap, phased-implementation plan, and budget requirements by the end of 2022 for a sustained surface ocean COmonitoring system, with the goal of establishing a fully functional system for the 2nd Global Stocktake of the UNFCCC in 2028.
  • Work with international partners to reach agreements on coordinated contributions and investments to implement the full fit-for-purpose observing system, including coastal areas, regional seas, and regional hubs (e.g., GOA-ON) and coordination support, by 2028.
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Ocean acidification exacerbates copper toxicity in both juvenile and adult stages of the green tide alga Ulva linza

Highlights

  • Seawater acidification alleviated the toxicity of low Cu levels on Ulva linza.
  • Increased Cu concentration would exacerbate toxicity and inhibit the grown of thalli.
  • Two stages of U. linza have same responses to high CO2 and Cu concentration.

Abstract

The toxicity of heavy metals to coastal organisms can be modulated by changes in pH due to progressive ocean acidification (OA). We investigated the combined impacts of copper and OA on different stages of the green macroalga Ulva linza, which is widely distributed in coastal waters, by growing the alga under the addition of Cu (control, 0.125 (medium, MCu), and 0.25 (high) μM, HCu) and elevated pCO2 of 1,000 μatm, predicted in the context of global change. The relative growth rates decreased significantly in both juvenile and adult thalli at HCu under OA conditions. The net photosynthetic and respiration rates, as well as the relative electron transfer rates for the adult thalli, also decreased under the combined impacts of HCu and OA, although no significant changes in the contents of photosynthetic pigments were detected. Our results suggest that Cu and OA act synergistically to reduce the growth and photosynthetic performance of U. linza, potentially prolonging its life cycle.

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A method for studying acidification and eutrophication potentials of a residential neighbourhood

Acidification and eutrophication are two environmental impacts that have a significant effect on air pollution and human health. The quantitative analysis of these two impacts remains hitherto unknown at the scale of new neighbourhoods. The main purpose of this research is to evaluate, analysis and compare the acidification and eutrophication potentials of one neighbourhood initially located in Belgium. To perform this comparison, the same neighbourhood design is applied to in 150 countries, but four parameters are adapted to each country: energy mix, local climate, building materials, and occupants’ mobility. In addition, this research evaluates the induced environmental costs of the neighbourhood over 100 years and examines the impact of the photovoltaic panel on these environmental impacts. This research, extended to the scale of several nations, will enable new researchers, and especially policy-makers, to measure the effectiveness of sustainable neighbourhoods. Eutrophication and acidification potentials were assessed under different phases (construction, use, renovation, and demolition), with Pleiades ACV software. Among the four local parameters (energy mix, local materials, climate, and transport, the energy mix has the most significant effect on the two studied environmental impacts. The results show that 72 %, and 65% of acidification, and eutrophication potentials are produced during the operational phase of the neighbourhood. In the case of sustainable neighbourhoods, the acidification potential is 22.1% higher in the 10 top Low incomes countries than the 10 top High-income countries. At the neighbourhood scale the main eutrophication potential component is water (34.2%), while, the main source of acidification potential is electricity production (45.1%)

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Anthropogenic and climatic contributions to observed carbon system trends in the Northeast Pacific

Abstract

The ocean absorbs anthropogenic carbon, slowing atmospheric CO2 increase but driving ocean acidification. Long-term changes in the carbon system are typically assessed from single-point time series or from hydrographic sections spaced by decades. Using higher resolution observations (1–3 year−1) from the Line P time series, we investigate processes modulating trends in the carbon system of the northeast subarctic Pacific. Dissolved inorganic carbon (DIC) and apparent oxygen utilization (AOU) from 1990 to 2019 reveal substantial trends over most of the upper water column along the 1,500 km coastal to open ocean transect. At the surface, an increasing trend in salinity-normalized DIC (sDIC33) (+0.5 ± 0.4 μmol kg−1 yr−1) is associated with a decrease in pH (0.01–0.02 decade−1) and a decrease in aragonite saturation state (0.04–0.08 decade−1). These observed trends are driven by anthropogenic CO2 uptake, partially offset by trends in surface salinity or temperature. Stratification associated with recent marine heat waves appears to have caused anomalously low surface pCO2. sDIC33 trends of similar magnitude were found below the seasonal thermocline on the 26.7–26.8 isopycnals (150–300 m), which are ventilated in the western Pacific. Roughly, a third (20%–50%) of the subsurface sDIC33 trend is driven by increased remineralization, likely caused by long-term decreases in ventilation in the western Pacific. Bidecadal oscillations in the ventilation of the 26.7–26.8 isopycnals arising from the Lunar Nodal Cycle cause oscillations in sDIC33 and AOU at the offshore end of our transect. We trace the oscillations to alternating periods of higher anthropogenic carbon uptake or higher carbon remineralization.

Plain Language Summary

The ocean takes up anthropogenic carbon and slows the rate at which atmospheric carbon dioxide is increasing. Using 30 years of data from the NE Pacific, we show that the surface ocean is indeed absorbing anthropogenic carbon and undergoing ocean acidification in this region. We find that carbon is also increasing in the subsurface waters. This excess carbon was absorbed in the western Pacific, where dense waters sink from the surface to the subsurface and transport anthropogenic carbon and oxygen eastward. This western Pacific breathing process appears to be weakening in time. If this trend continues, less anthropogenic carbon will be taken up and stored in subsurface waters in the future. Despite this reduction, some carbon will still naturally accumulate as the available oxygen is consumed and natural carbon dioxide is produced. Using data from three decades, we demonstrate the impact of climatic events and natural variability on the carbon system. At the surface, recent marine heat waves have reduced the amount of carbon absorbed by the ocean. In the subsurface waters, we observed that anthropogenic carbon increased in decades with stronger ventilation, while natural carbon generated by respiration of organic matter increased during periods of weaker ventilation.

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Climate and communities social scientist (21-1137): Alaska

Agency: Pacific States Marine Fisheries Commission

Location: Juneau, Alaska

Job category: Full time Positions

Salary: $28.73-$33.04/hour, DOE

Start date: 11/08/2021

Last date to apply: 08/18/2021

Website: https://www.psmfc.org/psmfc-info/careers_2018

Description:

Title: Climate and Communities Social Scientist (21-1137)

Anticipated Start Date: November 8, 2021

Position Type: Full Year (12 months or more), Hourly/Non-Exempt

Benefits Eligible: Yes | www.psmfc.org/benefits

Job Number: 21-1137

How to Apply: Online at www.psmfc.org/careers

Closing Date: August 18, 2021 at midnight (PT)

Group Definition: Data Management Specialists (Social Sciences) use a background in the social sciences as they assist in the population, maintenance, enhancement and distribution of databases. They locate, obtain, standardize, enter, verify, and correct various data sets related to project goals and work plans.

Position/Project Specifics: This position will assist on a project that will develop network models for south-central and southeast Alaska to improve communities’ and resource managers’ knowledge of socioecological system dynamics in response to ocean acidification (OA) and to enable these stakeholders to assess potential vulnerabilities and adaptation strategies. Participatory workshops with stakeholders will gather information on drivers and barriers that shape adaptive capacity and synthesize this information in socioecological network models that will enable stakeholders to better evaluate points of vulnerability and identify key adaptive strategies. The project will develop decision-support tools that are responsive to stakeholder concerns; reflect local community priorities and their ecological, social, economic, and management context; and synthesize the best available science. The position will work on all phases of the project, assisting with scoping meetings with principal investigators and key informants; conducting focus groups and semi-structured interviews; developing network models; analyzing and reporting the results as well as working with economic and ecological modelers to incorporate social system variables into integrated models. ** This position requires a valid driver’s license and all offers of employment will be contingent upon passing a driving record check. ** Essential Functions: (The functions listed below are characteristic of the type and level of work associated with this group and pay band. They are not all-inclusive. Individual positions may perform some or all, as well as other similar work.)

At the lower end of the range, employees:

• Conduct outreach to key stakeholders and development of protocols for participatory workshops including individualized exercises and group discussions.

• Work with local member of each study community to ensure broad, representative participation.

• Assist with conducting participatory workshops and analyzing results.

• Compile project data using social science data techniques and software.

• Develop qualitative network models and fuzzy cognitive maps during participatory workshops and afterwards with principal investigators.

• Assist in running perturbations on network models and analyzing results.

• Develop protocols for ground truthing results from network model perturbations with stakeholders.

• Examine adaptive strategies and capacities within the communities to ocean acidification perturbations.

• Extract relevant data which may be presented in many different text and numeric formats, reports, tables, graphics, or figures.

….

Agriculture & Life Sciences, Texas A & M University, 11 August 2021. More information.

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Effects on ocean among primary climate concerns for Iceland

Waves crashing over Reykjavík lighthouse
Photo: Golli. Waves crash over lighthouse in Reykjavík winter storm.

Ocean acidification, increased frequency of landslides, and possible changes to ocean currents are some of the impacts of climate change that could most affect Iceland, according to the country’s experts. Responding to the newly released report from the UN’s Intergovernmental Panel on Climate Change (IPCC), Iceland’s Environment Minister Guðmundur Ingi Guðbrandsson says government around the world need to step up their response to the climate crisis.

The PICC’s newest climate change report, intended as a resource for policymakers, compiles the latest data on climate change. Compared to the panel’s earlier reports, its findings are categorical about climate change being caused by humans and about the severity of the consequences it has in store.

Ocean acidification as concerning as warming

Tómas Jóhannesson is Director of Glaciology and an expert on the avalanche team at the Icelandic Met Office. He says the impact on the ocean surrounding Iceland is one of the biggest concerns regarding the local impact of climate change. The earth’s ocean’s have absorbed around 90% of the heat that has accumulated due to the increased greenhouse effect.

Considering Iceland’s dependence on the ocean, its acidification as a result of the carbon it absorbs from the atmosphere could be a long-term issue for the country. Acidification can affect the survival of smaller ocean organisms, in turn affecting the survival of fish and sea birds. “The acidification of the sea is unequivocal and is just as much a reason to stop emissions as warming,” Tómas stated.

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Call for registration: ARCUS Arctic Research seminar with Jens Terhaar, University of Bern

The Arctic Research Consortium of the U.S. (ARCUS) invites registration for the next Arctic Research Seminar featuring Jens Tehaar, a postdoctoral fellow in the division of Climate and Environmental Physics at the Physics Institute of the University of Bern. Dr. Tehaar’s presentation, titled Stressors of the Arctic Ocean Ecosystems: Improved Understanding of Primary Production and Ocean Acidification, will be held via Zoom on Tuesday, 17 August 2021 at 9:00 a.m. AKDT (1:00 p.m. EDT/5:00 p.m. GMT).

Seminar Abstract:

The Arctic Ocean is changing faster than any other ocean region in the world. Uptake of anthropogenic carbon, amplified warming, sea ice reduction, coastal erosion, and enhanced riverine runoff are driving important changes in the Arctic Ocean ecosystems through changes in primary production and ocean acidification. However, the current understanding of primary production and ocean acidification in the Arctic remains highly uncertain. Furthermore, projections of both processes by Earth-System Models diverge strongly in this region.

During this webinar, Dr. Terhaar will present: (1) a modelling study that quantifies the impact of terrigenous nutrients from rivers and coastal erosions on Arctic Ocean primary production, a process that was (wrongly?) neglected so far, and (2) results from two studies on emergent constraint on ocean acidification in the Arctic Ocean that suggests that projections of Earth-System Models collectively underestimated the extent of future ocean acidification in the Arctic Ocean.

Registration is required for this event. Instructions for accessing the webinar will be sent to registrants prior to the event.

To register for the event, go to:
ARCUS Arctic Research Seminar Series webpage

For questions, contact:
Stacey Stoudt
Email: stacey@arcus.org
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Zobol ocean acidification – white coral wastelands (audio)

Zobol – Ocean Acidification EP Nocta Numerica Records ‎– NN020 Vinyl 12′ 2021, Paris, France

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Surface pH record (1990–2013) of the Arabian Sea from boron isotopes of Lakshadweep corals—trend, variability, and control

Abstract

Atmospheric CO2 rise in post-industrial era has resulted in decline in surface ocean pH, commonly known as “ocean acidification (OA),” which has become a threat to marine calcifiers. Instrumental records of ocean pH and its reconstruction utilizing boron isotope (δ11B) composition of corals demonstrate a long-term OA trend characterized by large spatio-temporal variability in both Pacific and Atlantic oceans. However, no such record exists to elucidate long-term OA trend of the Indian Ocean. We report the first sub-annually resolved pH record (1990–2013) from the Arabian Sea based on δ11B measurements on Porites coral from Lakshadweep coral reefs. This pH record is characterized by large variability ranging from 7.93 to 8.65 with no long-term discernable trend. The long-term declining trend expected from the ∼50 ppm increase in atmospheric CO2 during the coral growth interval appears to be obscured by large surface pH variability in the Arabian Sea. Our investigation reveals that physical oceanographic processes for example, upwelling, downwelling and convective mixing modulated by El Niño-Southern Oscillation (ENSO) largely control surface pH variability and masked expected long-term OA trend resulting from anthropogenic CO2 rise. Combining the model-based predictions of increase in frequency and amplitude of ENSO events in a future warming scenario and the observed ENSO dependency of surface water pH, we predict more frequent and large pH variability (“pH extremes”) in this region. Such pH extremes and their occurrences might be critical for the resilience and adaptability of corals and other calcifiers in Arabian Sea and other similar oceanic settings elsewhere.

Plain Language Summary

Increase in the atmospheric CO2 concentration since the industrial revolution (∼1850) has resulted in decrease in ocean pH, known as ocean acidification (OA). Only limited number of pH records are avalable to assess the impacts of OA on marine ecosystems. The available pH records from the Pacific and Atlantic oceans, based on both instrumental observations and coral boron isotope records, demonstrate a long-term declining trend with significant internal variability. However, no such records are available from the Indian Ocean. Here, we provide the first seasonally resolved record of Indian Ocean pH for a 23 year period (1990–2013) based on boron isotope study of corals collected from the Lakshadweep, Arabian Sea. pH variability in the Arabian Sea is domiantly controlled by ENSO modulated oceanographic processes such as upwelling and mixing. We did not observe any long-term declining trend corresponding to the ∼50 ppm rise in atmospheric CO2 during the studied interval. The OA trend is possibly obscured by large surface pH variability in the Arabian Sea. Based on our observation and model based simulation showing an increase in ENSO frequency and amplitude for future scenarios, we expect that pH extremes are likely to increase, which is critical for resilience and adaptability of calcifying marine organisms.

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Dwarf eelgrass (Zostera noltii) fatty acid remodelling induced by climate change

Highlights

  • Seagrasses are marine founding species threatened by climate change.
  • These plants are sources of essential fatty acids (FAs) for the marine heterotrophic life.
  • Leaf saturated and polyunsaturated FAs in response to warming and acidification.
  • Changes in FAs suggest a membrane composition rearrangement to maintain membrane fluidity.
  • Linolenic acid decrease appears to be connected to reactive oxygen species quenching.
  • Seagrass FAs profile appear as good candidate biomarkers for climate change related stress.

Abstract

Dwarf eelgrass Zostera noltii meadows are found in estuarine coastal areas across the north-eastern Atlantic, where they provide key ecosystem services, including nursery grounds, sediment stabilization, nutrient cycling and carbon sequestration. These blue carbon ecosystems are being subjected to several anthropogenic pressures, including climate change-related effects. In the present study, we investigated the biochemical changes (fatty acid profiling) under different climate change scenarios (present-day conditions, ocean acidification, ocean warming and combined warming and acidification), following IPCC RCP scenario 8.5. Significant modifications in the percentage of saturated (SFA) and polyunsaturated fatty acids (PUFAs) in response to warming and low pH levels were detected. The changes suggest a rearrangement of membrane composition to maintain membrane fluidity, especially under warming conditions. Individuals under warming treatment showed higher plastidial pathway activity, while acidification induced a shift in the fatty acid synthesis pathway towards the extra-plastidial pathway, indicating a need to readjust the chloroplastidial monogalactosyldiacylglycerol (MGDG) and digalactosyldiacylglycerol (DGDG) lipids under thermal stress to counteract excessive membrane fluidity. Regarding PUFA fatty acids, α-linolenic acid (ALA, C18:3, n-3) showed a pronounced decrease under the combined treatment, a tendency that can be connected to reactive oxygen species (ROS) quenching and membrane remodelling. Thus, and observing the changes in the fatty acid profile, these essential molecules appear as good candidate biomarkers to detect changes in seagrass ecophysiology under acute climate change-related events. Our findings suggest that future global warming will pose a serious threat to these already endangered blue ecosystems.

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Consider the following: a pilot study of the effects of an educational television program on viewer perceptions of anthropogenic climate change and ocean acidification

Climate change portends significant harms to humans and biodiversity but public knowledge of relevant scientific information remains limited. As societal changes and investment are essential to addressing anthropogenic climate change, efforts to better promote both civic science literacy and public awareness of climate change impacts are urgently required. Popular scientific television programming provides one avenue for broad climate change communication efforts.

Our pilot study seeks to evaluate the effects viewing a popular scientific television program, “Bill Nye Saves the World: The Earth is a hot mess” on both fact recall and personal perceptions. We surveyed undergraduate students enrolled in non-majors courses at two institutions of higher education, one large selective private university, and one community college with open enrollment before and after viewing this program. The survey contained both open-response questions and Likert-like ordinal responses intended to evaluate both fact recall and beliefs related to climate change.

After viewing the program, student awareness of climate change impacts was improved, especially for topics emphasized by the program such as sea level rise. Student awareness of ocean acidification was extremely low prior to viewing the program, and improved dramatically, with most respondents aware that ocean acidification is already impacting marine life after viewing. Our pilot study suggests that scientific television programs may successfully promote awareness of climate change impacts and increase perceived personal relevance of climate change, but additional data from a larger and demographically broad population is required to test whether this result is more broadly applicable.

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Elevated CO2 accelerated the bloom of three Ulva species after one life cycle culture

Human activities and the resulting global climate change have profound effects on ecosystems, and economic and social systems, including those dependent on the ocean. Increasing concentrations of atmospheric CO2 have led to gradual changes in the marine carbonate system. It is well known that environmental changes determine the composition and abundance of algal populations. In the present study, we evaluated the growth, photosynthesis, nutrient uptake rates, tissue C and N content, nitrate reductase activity, and nitrate transporter gene expression of Ulva proliferaUlva linza, and Ulva compressa exposed to 400, 1000, and 2000 ppm CO2 levels after one life cycle culture. Elevated CO2 promoted the rapid propagation of three Ulva species, which can result in the formation of a green tide. This was due to enhanced photosynthetic and respiration efficiency, reductions in energy requirements for biosynthesis and metabolism for maintaining external pH, and promotion of NO3 uptake by increased NO3 gene expression level and NO3 reductase activity.

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IPCC author Tamsin Edwards: ‘still possible to limit warming to 1.5°C’

Tamsin Edwards
Tamsin Edwards is a lead author of the new IPCC report

The landmark report released yesterday by the Intergovernmental Panel on Climate Change (IPCC) has left many people reeling about the current and future state of our planet. But Tamsin Edwards at King’s College London, a lead author on the report, says it is understandable that it takes time for the gravity of the situation to sink in. “I think many people aren’t that aware that we have already committed ourselves to changes that are irreversible. That is a profound thing to take on board,” she says.

Those changes include warmer ocean temperatures, ocean acidification and a decline in oxygen levels in our seas. All are now irreversible on centennial to millennial time scales because of humanity’s fossil fuel burning and other activities. “We are changing the planet. It will continue to change no matter what we do in terms of our emissions, for hundreds of thousands of years. That is beyond our comprehension in many ways,” says Edwards.

Her involvement in reviewing the global environmental crisis is intimately connected to her own personal health crisis. Edwards was appointed a lead author on the report in 2018, around the same time she was diagnosed with bowel cancer. Three years ago, she delayed chemotherapy to attend a vital meeting in China with some of the 234 other authors of the report. The covid-19 pandemic pushed those meetings online, culminating in the past fortnight where the final text was approved by 195 governments, a process that adds to the report’s gravitas.

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Fighting ocean acidification: Smith Cove blue carbon project (text & video)

Oyster beds, kelp, and eel grass in Smith Cove to enhance efforts against ocean acidification. The Port of Seattle is leading many efforts to reduce greenhouse gas emissions (GHG emissions), the most important step towards combatting ocean acidification. The Port has been very active in enhancing shoreline habitat, reducing pollution, and engagement with communities. At Smith Cove in Elliott Bay, the Port of Seattle and its partners are conducting scientific research that will contribute to building resiliency in local ecosystems related to ocean acidification. As part of the Port of Seattle’s commitment to the International Alliance to Combat Ocean Acidification (OA Alliance), the Port prepared its first ever Ocean Acidification Action Plan to detail steps we are taking to address ocean acidification. “Last year, the Port of Seattle was the first port in the world to join the International Alliance to Combat Ocean Acidification (OA Alliance), recognizing the many ways in which ocean acidification impacts the maritime sector and acknowledging the important role ports can play in leading environmental action,” said Stephanie Bowman, Port of Seattle Commissioner. “We encourage other ports to join in on these efforts.” The Smith Cove Blue Carbon Pilot Project is located on Port and City-owned aquatic lands near Terminal 91. The goal of the project is to evaluate the potential benefits of marine habitat enhancement of kelp, eelgrass, and oysters on carbon sequestration, water quality (amelioration of seawater acidification), and habitat productivity. The Port of Seattle, along with partners at the Washington State Department of Natural Resources (DNR) and the Department of Ecology (Ecology), and the Puget Sound Restoration Fund (PSRF) is monitoring the site over three years for potential benefits in and around the site and includes a community-based science initiative.

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Effects of climate change induced ocean acidification and hypoxia on larval rockfish

Date: 20 August 2021

Time: 10:00 pm

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AR6 Climate change 2021: the physical science basis

The Working Group I contribution to the Sixth Assessment Report addresses the most up-to-date physical understanding of the climate system and climate change, bringing together the latest advances in climate science, and combining multiple lines of evidence from paleoclimate, observations, process understanding, and global and regional climate simulations.

Disclaimer: The Summary for Policymakers (SPM) is the approved version from the 14th session of Working Group I and 54th Session of the Intergovernmental Panel on Climate Change and remains subject to final copy-editing and layout.

The Technical Summary (TS), the full Report Chapters, the Annexes and the Supplementary Materials are the Final Government Distribution versions, and remain subject to revisions following the SPM approval, corrigenda, copy-editing, and layout.

Full report

CHANGING by Alisa Singer
Changing by the artist Alisa Singer
“As we witness our planet transforming around us we watch, listen, measure … respond.”

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Opportunities for U.S. State Governments and in-region partners to address ocean acidification through management and policy frameworks

Increasing OA, combined with other stressors like warming and loss of oxygen, threatens marine species and ecosystems, including those that sustain jobs and support coastal economies. For the last 10 years, U.S. coastal states have played a key role in responding to OA specifically. In 2019, OA practitioners from the U.S. east and west coasts assembled for a multi-day conference focused on sharing and documenting advances in OA collaborations, governance and management strategies. Since that time, conference attendees, supported by conference organizer the International Alliance to Combat Ocean Acidification, have worked to distill the lessons learned and to synthesize collective experiences. To assist governments, agencies, and organizations in addressing OA, this paper describes state-level efforts to develop and implement OA actions within policy and management frameworks. We outline pathways to action and illustrate approaches that link OA with climate policy and environmental management.

Continue reading ‘Opportunities for U.S. State Governments and in-region partners to address ocean acidification through management and policy frameworks’

Estuarine acidification: exploring the situation of mangrove dominated Indian sundarban estuaries

  • Provides insights into ecosystem services of the coastal zone and estuaries which have direct impact on national GDPs
  • Offers insights from one of the most fragile ecosystems in the world, Indian Sundarbans, a World Heritage Site
  • Presents in-depth case studies which highlight challenges of increasing acidification of coastal and estuarine waters

This book provides a cross-sectoral, multi-disciplinary assessment of different problems associated with estuarine acidification with special thrust on mangrove dominated Indian Sundarban estuaries. The arms of ocean acidification have extended to coastal and estuarine waters, where a wide spectrum of biodiversity thrives with unique adaptation extending several ecosystem services. Impact of acidification in these areas is a matter of concern as acidification potentially has more immediate effects on the health of estuaries and inshore regions as well as regional economies. Ground zero data collected for more than three decades have made the book stand on a strong base.

Continue reading ‘Estuarine acidification: exploring the situation of mangrove dominated Indian sundarban estuaries’

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