Archive for January, 2021



Ocean acidification is transforming California mussel shells

The large mollusk known as the California mussel makes its home in the rocky shoreline along the Pacific Coast from Mexico to Alaska. Considered a “foundational” animal, Mytilus californianus provides homes for hundreds of other species and offers a rich food source for species ranging from spiny lobsters to humans.

As the waters off our coasts change due to human influences, scientists at the University of California San Diego are finding that the composition of California mussel shells is weakening as it becomes more tolerant of acidic conditions.

Scientists have known that rising levels of human-produced carbon dioxide that are increasingly absorbed into the world’s oceans will have an impact on sea life. But as ocean waters increasingly acidify, tracking impacts on specific species has been difficult to gauge over time. Most of what we know about species’ responses to acidifying waters comes from short-term experiments that suggest these increases in ocean acidity—causing a lowering of seawater pH and less availability of carbonate ions to make shells—can lead to less fortified shells and more vulnerable animals.

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Ocean acidification commission

Event Details

Status: Upcoming

Event Date: Thursday, January 14, 2021

Start Time: 11:00 AM

Location: Virtual Hearing
https://us02web.zoom.us/j/85762774455?pwd=M0FuL1ZiTUtyWjJjRklsZkhkaTZRZz09

Event Description

Ocean Acidification Commission

Discuss OA report release

Meeting ID: 857 6277 4455

Passcode: 258991

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MACAN to host webinar on the biological responses of ocean acidification in early life-stages of fishes of inshore waters of the Mid-Atlantic

The Mid-Atlantic Coastal Acidification Network (MACAN) will host a webinar entitled Examining the Biological Responses of Ocean Acidification in Early Life-Stages of Fishes of Inshore Waters of the Mid-Atlantic, USA on Jan 26, 2021 at 11:00 AM EST. 

To register: https://attendee.gotowebinar.com/register/4753238655917450512    

Speaker Information: Chris Chambers is a Research Fishery Biologist at the Northeast Fisheries Science Center’s Howard Marine Sciences Laboratory at Sandy Hook, New Jersey. He and his Life History and Recruitment team study how the environment, including climate change and ocean acidification, affect the likelihood of survival and general health of the earliest and most sensitive life-stages of a variety of marine finfish species.  His research uses first principles of ecology, life history, and inference to anticipate how fishes might respond to future environments.

Continue reading ‘MACAN to host webinar on the biological responses of ocean acidification in early life-stages of fishes of inshore waters of the Mid-Atlantic’

Ocean acidification- a new threat to marine ecosystem discussed in Monrovia

Human-made carbon dioxide (CO2) emissions have taken residence in the ocean at significant proportion and causing unprecedented changes to ocean chemistry by reducing the water’s pH level, leading to a collection of chemical changes dubbed ocean acidification.

Some of the participants pose for group photos

With continuous CO2 emissions, scientists predict that the menace will intensify to the detriment of marine ecosystems and the services they provide to society, particularly coastal communities. This is a risk, scientists from across Europe, Africa and the United States are working to avert by holding a side event in Monrovia virtually and in-person on the weekend of January 8, 2021, to promote awareness and remedy research gaps in Africa- a continent proven to lack technical resources that would enable it to face this fastest-growing threat.

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Effects of ocean acidification on coral endolithic bacterial communities in Isopora palifera and Porites lobata

Endolithic microbes in coral reefs may act as a nutrient source for their coral hosts. Increasing atmospheric CO2 concentrations are causing ocean acidification (OA), which may affect marine organisms and ecosystems, especially calcifying organisms such as reef-building corals. However, knowledge of how OA affects marine microbes remains limited, and little research has been done on how coral endolithic communities respond to shifting environmental baselines. In this study, the endolithic communities of two common shallow water coral species, Isopora palifera and Porites lobata, were examined to investigate the microbial community dynamics under OA treatments. The colonies were placed in an environment with a partial pressure of carbon dioxide (pCO2) of 1,000 or 400 ppm (control) for 2 months. Several I. palifera colonies bleached and died at 1,000 ppm pCO2, but the P. lobata colonies remained unaffected. Inversely, the endolithic community in P. lobata skeletons showed significant changes after OA treatment, whereas no significant dynamics were observed among the I. palifera endoliths. Our findings suggest that the skeletal structures of different coral species may play a key role in corals host and endoliths under future high-OA scenarios.

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CO2 emissions increase ocean acidity (video and text)

IAEA Video

The 8th of January (08.01) was chosen to be the Ocean Acidification Day of Action because 8.1 is the current pH of the ocean. Global ocean acidification is a clear illustration of one of the profound effects of sustained climate change. This phenomenon is changing the chemistry of our oceans and affecting the health of many marine animals, some of which people rely on for their livelihood and for food.

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Sustaining leadership for climate and ocean action in 2021

The 3rd annual International Ocean Acidification Day of Action is being hosted by OA Alliance member, The Ocean Foundation on January 8th,  representing 8.1 the current pH level of our ocean.

To celebrate, the OA Alliance has issued the following article calling for increased international collaboration and leadership that will help build resilience to the social, economic and cultural vulnerabilities caused by climate and ocean change.

Please visit the “OA Day of Action” website to learn more.

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Gene expression patterns of red sea urchins (Mesocentrotus franciscanus) exposed to different combinations of temperature and pCO2 during early development

Background

The red sea urchin Mesocentrotus franciscanus is an ecologically important kelp forest herbivore and an economically valuable wild fishery species. To examine how M. franciscanus responds to its environment on a molecular level, differences in gene expression patterns were observed in embryos raised under combinations of two temperatures (13 °C or 17 °C) and two pCO2 levels (475 μatm or 1050 μatm). These combinations mimic various present-day conditions measured during and between upwelling events in the highly dynamic California Current System with the exception of the 17 °C and 1050 μatm combination, which does not currently occur. However, as ocean warming and acidification continues, warmer temperatures and higher pCO2 conditions are expected to increase in frequency and to occur simultaneously. The transcriptomic responses of the embryos were assessed at two developmental stages (gastrula and prism) in light of previously described plasticity in body size and thermotolerance under these temperature and pCO2 treatments.

Continue reading ‘Gene expression patterns of red sea urchins (Mesocentrotus franciscanus) exposed to different combinations of temperature and pCO2 during early development’

Tracking ocean acidification in Puerto Rico: a video journey

January 19 @ 2:00 pm – 3:00 pm

NOAA Ocean Acidification Program

Presented by: Melissa Melendez, University of Hawai’i Manoa and Lisa-Marie Carrubba, NOAA/NMFS Office of Protected Resources

Register: https://register.gotowebinar.com/register/7216082030659424272


Puerto Rico is home to vibrant coral reef ecosystems that support a diversity of marine life and livelihoods. Join us as we share our journey in creating Spanish-language videos (with English subtitles) about ocean acidification, its causes, consequences, research and possible solutions for the Puerto Rican public and island visitors. The video invites viewers to get involved in community actions that reduce other stressors to marine organisms and increase their resilience to the effects of ocean acidification. A full length and short video (highlighting key messages) were created in collaboration with a number of NOAA and non-NOAA partners, including the University of Puerto Rico and Paradise SCUBA and Snorkeling Center, and produced by a local videographer, Efra Visuals. You’re welcome to view the full video on the producer’s YouTube channel prior to the live webinar.

We hope to ‘see’ you there!

Continue reading ‘Tracking ocean acidification in Puerto Rico: a video journey’

Thermal stress reduces pocilloporid coral resilience to ocean acidification by impairing control over calcifying fluid chemistry

The combination of thermal stress and ocean acidification (OA) can more negatively affect coral calcification than an individual stressors, but the mechanism behind this interaction is unknown. We used two independent methods (microelectrode and boron geochemistry) to measure calcifying fluid pH (pHcf) and carbonate chemistry of the corals Pocillopora damicornis and Stylophora pistillata grown under various temperature and pCO2 conditions. Although these approaches demonstrate that they record pHcf over different time scales, they reveal that both species can cope with OA under optimal temperatures (28°C) by elevating pHcf and aragonite saturation state (Ωcf) in support of calcification. At 31°C, neither species elevated these parameters as they did at 28°C and, likewise, could not maintain substantially positive calcification rates under any pH treatment. These results reveal a previously uncharacterized influence of temperature on coral pHcf regulation—the apparent mechanism behind the negative interaction between thermal stress and OA on coral calcification.

Continue reading ‘Thermal stress reduces pocilloporid coral resilience to ocean acidification by impairing control over calcifying fluid chemistry’

Acidification stress effect on umbonate veliger larval development in Panopea globosa

Highlights

  • The pH significantly influenced the biometric variables in Panopea globosa larvae.
  • Larvae exposed to lower pH showed shell dissolution at the umbo level.
  • The metabolic rate was higher in larvae exposed to acidification compared to the control.
  • Nicotinamide adenine dinucleotide dehydrogenase expression levels to pH 7.5 suggest a higher energy requirement.

Abstract


Ocean acidification generates a decrease in calcium carbonate availability essential for biomineralization in organisms such as mollusks. This effect was evaluated on Panopea globosa exposing for 7 days umbonate veliger larvae to two pH treatments: experimental (pH 7.5) and control (pH 8.0). Exposure to pH 7.5 affected growth, reducing larval shell length from 5.15–13.34% compared to the control group. This size reduction was confirmed with electron microscopy, also showing shell damage. The physiological response showed an increase in oxygen consumption in larvae exposed to low pH with a maximum difference of 1.57 nmol O2 h−1 larvae−1 at day 7. The gene expression analyses reported high expression values for nicotinamide adenine dinucleotide (NADH) dehydrogenase and Perlucin in larvae at pH 7.5, suggesting a higher energetic cost in this larval group to maintain homeostasis. In conclusion, this study showed that acidification affected development of P. globosa umbonate veliger larvae.

Continue reading ‘Acidification stress effect on umbonate veliger larval development in Panopea globosa’

Corals bleached from heat become less resilient to ocean acidification

Cat’s Paw Coral (Stylophora pistillata)
blickwinkel/Alamy

Corals get a double-whammy negative from heat – those that are bleached as a result of heat stress also become less resilient to ocean acidification.

Robert Eagle at the University of California, Los Angeles and his colleagues have analysed the effect of elevated temperatures on the growth of two species of stony coral when the corals are also exposed to ocean acidification.

The acidification of oceans occurs as result of carbon dioxide in the atmosphere being absorbed by seawater. The results are a decrease in the pH of the water, a decrease in its concentration of carbonate ions and a drop in the saturation states of calcium carbonate minerals.

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Physiological adaptation of marine bivalves to global changes (M/F) in Argenton at IFREMER (in English)

Job title : Physiological adaptation of marine bivalves to global changes (M/F)

Reference:  PV-2020-096

Department/Office: Département des Ressources Biologiques et Environnement, Unité de recherche Physiologie Fonctionnelle des Organismes Marins, Laboratoire de Physiologie des Invertébrés

Duty station:  Landunvez, Bretagne, FR , France

Deadline for applications : 07/02/2021

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Seven countries in Gulf of Guinea to start monitoring ocean acidification

The BIOTTA (Building CapacIty in Ocean AcidificaTion MoniToring in the Gulf of GuineA) project will be the first coordinated effort in ocean acidification monitoring the Gulf of Guinea and other adjoining coasts in Africa.

With seed funding and equipment support from the Partnership for Observation of the Global Ocean (POGO) and The Ocean Foundation (TOF) respectively, BIOTTA will establish long-term Ocean Acidification monitoring stations in seven countries in West Africa (Liberia, Cote d’Ivoire, Ghana, Benin, Nigeria, Cameroon, and the Republic of Congo.

The leader of the BIOTTA working group Dr. Edem Mahu, from the Department of Marine and Fisheries Sciences of the University of Ghana, noted that “a lack of skillset and capacity in the measurement of ocean acidification in West Africa hinders our understanding of the phenomenon and threatens valuable economical and ecological resources in the Gulf of Guinea such as fisheries, aquaculture and tourism. This deficit in ocean acidification measurement skills forestalls our understanding of species vulnerability to changing pH and associated chemical reactions.  Ocean Acidification monitoring in this understudied area has come to stay and we will work assiduously to sustain this brilliant initiative.”

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The new face of the Antarctic

In the future, the Antarctic could become a greener place and be colonised by new species. At the same time, some species will likely disappear. 25 researchers recently presented these and many other findings in a major international project, in which they analysed hundreds of articles on the Antarctic published in the past ten years. By doing so, the team have provided an exceptionally comprehensive assessment of the status quo and future of Antarctica and the Southern Ocean that surrounds it.

Never before have researchers arrived at so many new findings on the biological and biochemical processes at work in the Antarctic than in the past ten years. Now 25 experts, led by the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (AWI), have analysed and compiled these findings in the project “AnT-ERA.” Having ultimately processed several hundred articles on the Antarctic, the team have now distilled the content into ten core messages addressing a broad range of aspects, e. g. ocean acidification, biodiversity, and the significance of sea ice for various organisms. “If you look at the timeframe from 1970 to the present, roughly 80 percent of all academic publications on biology and biochemistry in the Antarctic were released between 2010 and 2020. That’s what moved us to condense this enormous amount of knowledge into a single article,” says marine biologist and project coordinator Julian Gutt from the AWI. The project outcomes have just been published in the journal Biological Reviews.

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Raising ocean acidification awareness and research gaps in Africa: scientists meet to brainstorm

Many African countries rely heavily on their coasts and rivers for economic growth and well-being. Unfortunately, Africa’s marine and coastal ecosystems face severe environmental threats, such as untreated wastewater discharge, illegal fishing, and habitat degradation, all combined with human-induced climate change. The rapidly increasing atmospheric carbon dioxide (CO2) alters the climate and the chemistry of the ocean. Hence the ocean has absorbed one-fourth of anthropogenic CO2, thereby causing an increase in seawater acidity, a process referred to as ocean acidification.

The overwhelming evidence demonstrates that ocean acidification has the potential to negatively marine ecosystems and their associated services. While a global reduction of CO2 emissions (mitigation) is the ultimate solution, local adaptation strategies are needed to minimize ocean acidification’s negative effects. Currently, the lack of data on ocean acidification and its impacts for Africa is strongly limiting the potential to develop and implement such strategies. Ocean Acidification Africa (OA-Africa; https://www.oa-africa.net/) is a pan-African network working to coordinate and promote ocean acidification awareness and research in Africa.  The network is composed of more than 100 scientists interested in conducting ocean acidification research in Africa. OA- Africa is part of the wider Global Ocean Acidification Observing Network  (https://www.goa-on.org/)  as one of seven regional hubs.

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Ocean acidifcation may be increasing the intensity of lightning over the oceans

The anthropogenic increase in atmospheric CO2 is not only considered to drive global warming, but also ocean acidification. Previous studies have shown that acidification will affect many aspects of biogenic carbon uptake and release in the surface water of the oceans. In this report we present a potential novel impact of acidification on the flash intensity of lightning discharged into the oceans. Our experimental results show that a decrease in ocean pH corresponding to the predicted increase in atmospheric CO2 according to the IPCC RCP 8.5 worst case emission scenario, may increase the intensity of lightning discharged into seawater by approximately 30 ± 7% by the end of the twenty-first century relative to 2000.

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Seasonal variability of net sea-air CO2 fluxes in a coastal region of the northern Antarctic Peninsula

We show an annual overview of the sea-air CO2 exchanges and primary drivers in the Gerlache Strait, a hotspot for climate change that is ecologically important in the northern Antarctic Peninsula. In autumn and winter, episodic upwelling events increase the remineralized carbon in the sea surface, leading the region to act as a moderate or strong CO2 source to the atmosphere of up to 40 mmol m–2 day–1. During summer and late spring, photosynthesis decreases the CO2 partial pressure in the surface seawater, enhancing ocean CO2 uptake, which reaches values higher than − 40 mmol m–2 day–1. Thus, autumn/winter CO2 outgassing is nearly balanced by an only 4-month period of intense ocean CO2 ingassing during summer/spring. Hence, the estimated annual net sea-air CO2 flux from 2002 to 2017 was 1.24 ± 4.33 mmol m–2 day–1, opposing the common CO2 sink behaviour observed in other coastal regions around Antarctica. The main drivers of changes in the surface CO2 system in this region were total dissolved inorganic carbon and total alkalinity, revealing dominant influences of both physical and biological processes. These findings demonstrate the importance of Antarctica coastal zones as summer carbon sinks and emphasize the need to better understand local/regional seasonal sensitivity to the net CO2 flux effect on the Southern Ocean carbon cycle, especially considering the impacts caused by climate change.

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Ocean acidification increases polyspermy of a broadcast spawning bivalve species by hampering membrane depolarization and cortical granule exocytosis

Highlights

  • Ocean acidification (OA) increases polyspermy risk in the blood clam
  • Population recruitment of broadcast spawning marine species might be threatened by OA
  • OA induces polyspermy via hampering membrane depolarization and cortical reaction
  • Disrupted polyspermy blocking may be due to alterations in intracellular Ca2+ and ATP

Abstract


Ensuring that oocytes are fertilized by a single sperm during broadcast spawning is crucial for the fertilization success of many marine invertebrates. Although the adverse impacts of ocean acidification (OA) on various marine species have been revealed in recent years, its impact on polyspermy and the underlying mechanisms involved remain largely unknown. Therefore, in the present study, the effect of OA on polyspermy risk was assessed in a broadcast spawning bivalve, Tegillarca granosa. In addition, the impacts of OA on the two polyspermy blocking processes, the fast block (membrane depolarization) and the permanent block (cortical reaction), were investigated. The results show that the exposure of oocytes to two future OA scenarios (pH 7.8 and pH 7.4) leads to significant increases in polyspermy risk, about 1.70 and 2.38 times higher than the control, respectively. The maximum change in the membrane potential during oocyte membrane depolarization markedly decreased to 15.79% (pH 7.8) and 34.06% (pH 7.4) of the control value. Moreover, the duration of oocyte membrane depolarization was significantly reduced to approximately 63.38% (pH 7.8) and 21.91% (pH 7.4) of the control. In addition, cortical granule exocytosis, as well as microfilament migration, were significantly arrested by OA treatment. Exposure to future OA scenarios also led to significant reductions in the ATP and Ca2+ content of the oocytes, which may explain the hampered polyspermy blocking. Overall, the present study suggests that OA may significantly increase polyspermy risk in T. granosa by inhibiting membrane depolarization and arresting cortical granule exocytosis.

Continue reading ‘Ocean acidification increases polyspermy of a broadcast spawning bivalve species by hampering membrane depolarization and cortical granule exocytosis’

Animal size and sea water temperature, but not pH, influence a repeatable startle response behavior in a wide-ranging marine mollusc

Highlights

  • We measured startle response (time to open) in mussels following a predator cue.
  • We tested effects of temperature, pH and size and measured repeatability.
  • Larger mussels opened faster; repeatable startle response; evidence of habituation.
  • High temperature increased time to open; no effect of pH.
  • Blue mussels are sensitive to temperature and vulnerable to climate change.

Abstracts

Startle response behaviours are important in predator avoidance and escape for a wide array of animals. For many marine invertebrates, however, startle response behaviours are understudied, and the effects of global change stressors on these responses are unknown. We exposed two size classes of blue mussels (Mytilus edulis × trossulus) to different combinations of temperature (15 and 19 °C) and pH (8.2 and 7.5 pHT) for 3 months and subsequently measured individual time to open following a tactile predator cue (i.e. startle response time) over a series of four consecutive trials. Time to open was highly repeatable in the short term and decreased linearly across the four trials. Individuals from the larger size class had a shorter time to open than their smaller-sized counterparts. High temperature increased time to open compared to low temperature, while pH had no effect. These results suggest that bivalve time to open is repeatable, related to relative vulnerability to predation and affected by temperature. Given that increased closure times impact feeding and respiration, the effect of temperature on closure duration may play a role in the sensitivity to ocean warming in this species and contribute to ecosystem level effects.

Continue reading ‘Animal size and sea water temperature, but not pH, influence a repeatable startle response behavior in a wide-ranging marine mollusc’

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