Alongshore variation in barnacle populations is determined by surf zone hydrodynamics

Influence of a changing wave climate on the quality and morphometry of the stalked barnacle Pollicipes pollicipes (Gmelin, 1789), along the coasts of NW Iberia

Wave climate is shifting over the last decades along the Atlantic coasts of Europe ultimately driven by large-scale patterns of atmospheric variability forced by anthropogenic global warming. Changes in wave height and surf zone orbital currents are hypothesized to drive marked shifts in the shape of intertidal organisms such as the stalked barnacle Pollicipes pollicipes, whose quality and market price are known to decrease non linearly with the peduncle length: width ratio S. This study evaluates wave trends in NW Iberian Peninsula, using the Spanish Port System 2006-2020 SIMAR wave hindcast. On the other hand, trends in stalked barnacle morphology and quality are estimated from 26 sites at the management regions of Baiona and A Guarda between 2011 and 2020. Results show evidence of temporal changes in barnacle quality and, especially, morphometry caused by simultaneous shifts in winter wave induced orbital currents. Because of the non linear relationship between S and the high quality threshold, large increases in S are usually translated to small reductions in quality. However, we identified a tipping point around S = 2.4 that if surpassed can lead to great drops in barnacle quality. In addition, changes in wave forcing will have different effects at each extraction site, as trends in wave climate are decoupled from barnacle morphometry at steeper sites sheltered from the predominant wave direction. In conclusion, this knowledge could be applied to develop site specific barnacle harvesting strategies based on annual wave climate forecasts.

Graphical abstract

Supplementary Information

The online version contains supplementary material available at 10.1007/s11160-024-09838-2.

Ontogeny of osmoregulation of the Asian shore crab Hemigrapsus sanguineus at an invaded site of Europe

We studied the ontogeny of osmoregulation of the Asian shore crab Hemigrapsus sanguineus at an invaded area in the North Sea. H. sanguineus is native to Japan and China but has successfully invaded the Atlantic coast of North America and Europe. In the invaded areas, H. sanguineus is becoming a keystone species as driver of community structure and the adults compete with the shore crab Carcinus maenas. Strong osmoregulatory abilities may confer the potential to use and invade coastal areas already earlier in the life cycle. We reared larvae and first juveniles at 24°C in seawater from hatching to intermoult of each developmental stage (zoea I-V, megalopa, crab I). We exposed each stage to a range of salinities (0-39 ppt) for 24 h, and then we quantified haemolymph osmolality, using nano-osmometry. In addition, we quantified osmolality in field-collected adults after acclimation to the test salinities for 6 days. Larvae of H. sanguineus were able to hyper-osmoregulate at low salinities (15 and 20 ppt) over the complete larval development, although the capacity was reduced at the zoeal stage V; at higher salinities (25-39 ppt), all larval stages were osmoconformers. The capacity to slightly hypo-regulate at high salinity appeared in the first juvenile. Adults were able to hyper-osmoregulate at low salinities and hypo-regulate at concentrated seawater (39 ppt). H. sanguineus showed a strong capacity to osmoregulate as compared to its native competitor C. maenas, which only hyper-regulates at the first and last larval stages and does not hypo-regulate at the juvenile-adult stages. The capacity of H. sanguineus to osmoregulate over most of the life cycle should underpin the potential to invade empty niches in the coastal zone (characterized by low salinity and high temperatures). Osmoregulation abilities over the whole life cycle also constitute a strong competitive advantage over C. maenas.

Surf-zone hydrodynamics alter phytoplankton subsidies affecting reproductive output and growth of tidal filter feeders

Surf zones, classified from reflective to dissipative, separate the ocean from shore and subsidies from the coastal ocean must pass through surf zones to reach the shore. We have observed that variations in phytoplankton concentrations in the water over the intertidal zone varied with surf-zone hydrodynamics and we hypothesized that this variation would alter growth rates, population structure, and reproductive output of Mytilus californianus and Balanus glandula. From May 2016 to April 2017, along 7 km of Cape Arago, Oregon, USA surf-zone phytoplankton concentrations were determined weekly at nine sites with varying surf-zone hydrodynamics as indicated by surf-zone widths. Throughout the year, concentrations of phytoplankton in wider, more dissipative surf zones were, on average, 16× higher than in narrow, more reflective surf zones. Similar to previous observations, surf-zone width explained >90% of the variability in phytoplankton concentrations in the surf-zone. On average, ~83% of B. glandula had egg lamellae at more dissipative shores compared to only 8% at more reflective. An index of potential reproductive output by barnacle populations as measured by ash free dry mass (AFDM) of egg lamellae was ~243× larger at more dissipative than at reflective shores and surf-zone phytoplankton concentrations and surf-zone width explained ~96 and 92% of the variability in this index. On average, density of M. californianus was ~2× higher at more reflective shores, but 60% of these individuals were smaller and non-reproductive compared to only 24% at the more dissipative sites. The gonad tissue mass/m² of medium sized mussels was ~5× greater at more dissipative than reflective shores. Surf-zone phytoplankton concentrations and surf-zone width explained ~80% and 65% of the variability in individual mussel gonad mass and ~69% and 56% of the variability in mussel population gonad mass, respectively. M. californianus were out-planted to assess growth rates and, after 5 months, average body mass was ~3× greater at more dissipative than reflective shores. Surf-zone phytoplankton concentrations and width explained ~85% and 92% of the mass increase, respectively. Phytoplankton subsidies varied with surf-zone hydrodynamics altering the growth and reproductive output of two ecologically important intertidal filter feeders.

Planktonic Subsidies to Surf-Zone and Intertidal Communities

Plankton are transported onshore, providing subsidies of food and new recruits to surf-zone and intertidal communities. The transport of plankton to the surf zone is influenced by wind, wave, and tidal forcing, and whether they enter the surf zone depends on alongshore variation in surf-zone hydrodynamics caused by the interaction of breaking waves with coastal morphology. Areas with gently sloping shores and wide surf zones typically have orders-of-magnitude-higher concentrations of plankton in the surf zone and dense larval settlement in intertidal communities because of the presence of bathymetric rip currents, which are absent in areas with steep shores and narrow surf zones. These striking differences in subsidies have profound consequences; areas with greater subsidies support more productive surf-zone communities and possibly more productive rocky intertidal communities. Recognition of the importance of spatial subsidies for rocky community dynamics has recently advanced ecological theory, and incorporating surf-zone hydrodynamics would be an especially fruitful line of investigation.