Abstract

Simple SummaryThis study’s data suggest that under the projected scenarios of ocean acidification by 2100 and beyond, significant negative impacts on growth, health, and meat quality are expected, particularly on black sea bream, and will be susceptible to the scientifically approved fish having a weaker resistance to diseases and environmental changes if CO2 emissions in the atmosphere are not curbed. Knowing the expected consequences, mitigation measures are urgently needed.Acidification (OA), a global threat to the world’s oceans, is projected to significantly grow if CO2 continues to be emitted into the atmosphere at high levels. This will result in a slight decrease in pH. Since the latter is a logarithmic scale of acidity, the higher acidic seawater is expected to have a tremendous impact on marine living resources in the long-term. An 8-week laboratory experiment was designed to assess the impact of the projected pH in 2100 and beyond on fish survival, health, growth, and fish meat quality. Two projected scenarios were simulated with the control treatment, in triplicates. The control treatment had a pH of 8.10, corresponding to a pCO2 of 321.37 ± 11.48 µatm. The two projected scenarios, named Predict_A and Predict_B, had pH values of 7.80-pCO2 = 749.12 ± 27.03 and 7.40-pCO2 = 321.37 ± 11.48 µatm, respectively. The experiment was preceded by 2 weeks of acclimation. After the acclimation, 20 juvenile black sea breams (Acanthopagrus schlegelii) of 2.72 ± 0.01 g were used per tank. This species has been selected mainly due to its very high resistance to diseases and environmental changes, assuming that a weaker fish resistance will also be susceptibly affected. In all tanks, the fish were fed with the same commercial diet. The seawater’s physicochemical parameters were measured daily. Fish samples were subjected to physiological, histological, and biochemical analyses. Fish growth, feeding efficiency, protein efficiency ratio, and crude protein content were significantly decreased with a lower pH. Scanning electron microscopy revealed multiple atrophies of microvilli throughout the small intestine’s brush border in samples from Predict_A and Predict_B. This significantly reduced nutrient absorption, resulting in significantly lower feed efficiency, lower fish growth, and lower meat quality. As a result of an elevated pCO2 in seawater, the fish eat more than normal but grow less than normal. Liver observation showed blood congestion, hemorrhage, necrosis, vacuolation of hepatocytes, and an increased number of Kupffer cells, which characterize liver damage. Transmission electron microscopy revealed an elongated and angular shape of the mitochondrion in the liver cell, with an abundance of peroxisomes, symptomatic of metabolic acidosis.

Highlights

  • The full report of the Intergovernmental Panel on Climate Change (IPCC) published in 2019 [1] informed that from the pre-industrial period (1850–1900) until the present time, 2021, the Industrial Revolution involving the anthropogenic emission of CO2 into the atmosphere has led to climate change, causing ocean warming and acidification [2,3,4,5,6,7,8,9,10]

  • This research found that pH values of 7.80 at the end of the 21st century and 7.40 in the 23rd century would significantly decrease the crude protein content of black sea bream and the protein efficiency ratio

  • Under the projected Ocean Acidification (OA) pH, the growth performance data revealed that black sea bream eat more than normal but grow less than normal

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Summary

Introduction

The full report of the Intergovernmental Panel on Climate Change (IPCC) published in 2019 [1] informed that from the pre-industrial period (1850–1900) until the present time, 2021, the Industrial Revolution involving the anthropogenic emission of CO2 into the atmosphere has led to climate change, causing ocean warming and acidification [2,3,4,5,6,7,8,9,10]. From 1750 to 2011, CO2 emissions from fossil fuel combustion have released a mean value estimated as 375 (345–405) GtC to the atmosphere, while deforestation and other land-use changes have released an estimated mean value of 180 (100–260) GtC. Of these cumulative anthropogenic CO2 emissions, a mean of 240 (230–250) GtC have accumulated in the atmosphere, 155 (125–185) GtC have been taken up by the ocean, and a mean value of 160 (70–250) GtC have accumulated in terrestrial ecosystems [1,11]. The projected Ocean Acidification (OA) in the coming century is assumed to negatively impact aquatic ecosystems, with increased risks of environmental pollution and a significant threat to its living resources [12,13,14,15,16,17,18]

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