Category Ranking

98%

Total Visits

921

Avg Visit Duration

2 minutes

Citations

20

Article Abstract

The energetically costly transition from free-swimming larvae to a benthic life stage and maintenance of a calcareous structure can make calcifying marine invertebrates vulnerable to ocean acidification. The first goal of this study was to evaluate the impact of ocean acidification on calcified tube growth for two Serpulidae polychaete worms. sp. and were collected at 11 m depth from the northwest Mediterranean Sea and maintained for 30 and 90 days at three mean pH levels (total scale): 8.1 (ambient), 7.7 and 7.4. Moderately decreased tube elongation rates were observed in both species at pH 7.7 while severe reductions occurred at pH 7.4. There was visual evidence of dissolution and tubes were more fragile at lower pH but fragility was not attributed to changes in fracture toughness. Instead, it appeared to be due to the presence of larger alveoli covered in a thinner calcareous layer. The second objective of this study was to test for effects on offspring development. Spawning was induced, and offspring were reared in the same pH conditions that the parents experienced. Trochophore size was reduced at the lowest pH level but settlement success was similar across pH conditions. Post-settlement tube growth was most affected. At 38 days post-settlement, juvenile tubes at pH 7.7 and 7.4 were half the size of those at pH 8.1. The results suggest future carbonate chemistry will negatively affect the initiation and persistence of both biofouling and epiphytic polychaete tube worms.

Download full-text PDF

Source
http://dx.doi.org/10.1242/jeb.196543DOI Listing

Publication Analysis

Top Keywords

ocean acidification
12
tube growth
12
tube
5
acidification calcareous
4
calcareous tube
4
growth adults
4
adults reared
4
reared offspring
4
offspring serpulid
4
serpulid polychaetes
4

Similar Publications

Ocean acidification (OA) due to anthropogenic CO2 emissions has significantly altered ocean chemistry since the industrial era. Ocean alkalinity enhancement (OAE) is an innovative strategy to mitigate excess CO, with ocean liming (OL) serving as a potential carbon dioxide removal (CDR) method, through the spreading of Ca(OH) (slaked lime) at the ocean surface. This study examined the ecological effects of OL on a natural zooplankton community from the ultraoligotrophic Eastern Mediterranean Sea during a 14-day mesocosm experiment conducted in spring-summer.

View Article and Find Full Text PDF

Oyster farming acts as a marine carbon dioxide removal (mCDR) hotspot for climate change mitigation.

Proc Natl Acad Sci U S A

September 2025

Key Laboratory of Mariculture of Ministry of Education, Fisheries College, Ocean University of China, Qingdao 266003, China.

Bivalve farming, a vital component of global aquaculture, has been proposed as a potential marine carbon dioxide removal (mCDR) strategy, yet its role remains contentious. Using field mesocosms, we demonstrate that oyster filter-feeding enhances mCDR by accelerating the formation of particulate and dissolved organic carbon in the water column and promoting organic carbon deposition in sediments. This process shifts the water column toward a more autotrophic and alkaline state, effectively sequestering CO from the atmosphere.

View Article and Find Full Text PDF

Multidecadal decoupling between coral calcifying fluid and seawater saturation states.

Sci Adv

August 2025

Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA 70118, USA.

Ocean acidification poses a threat to coral skeleton formation via reductions in the saturation state of aragonite (Ω) in seawater. Given that corals precipitate their skeletons from a calcifying fluid supplied by seawater, reductions in seawater Ω should, in theory, confound calcification. Here, we reconstruct up to 200 years of coral calcifying fluid Ω, using Raman spectroscopy techniques, at approximately monthly resolution in two sp.

View Article and Find Full Text PDF

The influence of cross-generational warming on the juvenile development of a coral reef fish under ocean warming and acidification.

Mar Environ Res

August 2025

ARC Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, QLD, 4811, Australia; College of Science and Engineering, James Cook University, Townsville, QLD, 4811, Australia.

Marine ecosystems are facing escalating chronic and acute environmental stressors, yet our understanding of how multiple stressors influence individuals is limited. Here, we investigated how projected ocean warming (+1.5 °C) during grandparental (F) and parental (F) generations of the spiny chromis damselfish (Acanthochromis polyacanthus), influences the sensitivity of F juveniles to ocean warming (present-day vs +1.

View Article and Find Full Text PDF

In the perspective of a future ocean, climate change can alter upwelling systems globally. Along the Chilean coast, upwelling becomes intensified, leading to cool temperatures and low pH, which can affect common and widespread calcifying seaweed species such as Corallina officinalis. We measured physiological, biomineralogical, and palatability responses in two distinct populations originating from contrasting upwelling regimes, one from an upwelling area and the other from an upwelling shadow, by exposing them to current and future upwelling conditions.

View Article and Find Full Text PDF