Environmental Regulation, Technological Innovation and Development of Marine Fisheries—Evidence from Ten Coastal Regions in China

This study aims to examine the relationship between environmental regulation, technological innovation and the development of China’s marine fisheries. We make a theoretical overview of the relationship between environmental regulation, technological innovation and the development of marine fisheries. Using data from 10 coastal regions of China, we calculate the comprehensive development level of China’s marine fisheries in each region from 2009 to 2018 through the entropy method. Then, we use a double logit model to analyze the effects of environmental regulation and technological innovation on the development level of China’s marine fisheries, and further test the mediating effect of technological innovation. The results show that environmental regulations have a “U-shaped” effect on the development of China’s marine fisheries. Moreover, technological innovation is crucial in promoting the development of China’s marine fisheries. Further, we identify the mediating role of technological innovation, that is, environmental regulation affects the development of China’s marine fisheries by influencing technological innovation. These findings offer theoretical support for the development of China’s marine fisheries.

A framework to evaluate and elucidate the driving mechanisms of coastal sea surface <i>p</i>CO₂ seasonality using an ocean general circulation model (MOM6-COBALT)

The temporal variability of the sea surface partial pressure of CO2 (pCO2) and the underlying processes driving this variability are poorly understood in the coastal ocean. In this study, we tailor an existing method that quantifies the effects of thermal changes, biological activity, ocean circulation and freshwater fluxes to examine seasonal pCO2 changes in highly variable coastal environments. We first use the Modular Ocean Model version 6 (MOM6) and biogeochemical module Carbon Ocean Biogeochemistry And Lower Trophics version 2 (COBALTv2) at a half-degree resolution to simulate coastal CO2 dynamics and evaluate them against pCO2 from the Surface Ocean CO2 Atlas database (SOCAT) and from the continuous coastal pCO2 product generated from SOCAT by a two-step neuronal network interpolation method (coastal Self-Organizing Map Feed-Forward neural Network SOM-FFN, Laruelle et al., 2017). The MOM6-COBALT model reproduces the observed spatiotemporal variability not only in pCO2 but also in sea surface temperature, salinity and nutrients in most coastal environments, except in a few specific regions such as marginal seas. Based on this evaluation, we identify coastal regions of “high” and “medium” agreement between model and coastal SOM-FFN where the drivers of coastal pCO2 seasonal changes can be examined with reasonable confidence. Second, we apply our decomposition method in three contrasted coastal regions: an eastern (US East Coast) and a western (the Californian Current) boundary current and a polar coastal region (the Norwegian Basin). Results show that differences in pCO2 seasonality in the three regions are controlled by the balance between ocean circulation and biological and thermal changes. Circulation controls the pCO2 seasonality in the Californian Current; biological activity controls pCO2 in the Norwegian Basin; and the interplay between biological processes and thermal and circulation changes is key on the US East Coast. The refined approach presented here allows the attribution of pCO2 changes with small residual biases in the coastal ocean, allowing for future work on the mechanisms controlling coastal air–sea CO2 exchanges and how they are likely to be affected by future changes in sea surface temperature, hydrodynamics and biological dynamics.

MARINE HARDBOTTOM ENVIRONMENTS IN THE BEACHES OF CEARÁ STATE, EQUATORIAL COAST OF BRAZIL

This paper is a literature review on marine hardbottom environments (MHE) that emerge in coastal regions in the Brazilian state of Ceará. This stretch of the Brazilian coast houses several rock formations, which are widely distributed in the intertidal zone. These formations have various origins and composition, ranging from crystalline rocks to biogenic structures, but most are composed by sandstones. These substrates support biodiverse ecosystems that produce valuable environmental goods and services, which have historical and socioeconomic relevance for the state. Despite their importance, they are currently threatened by various types of local and global stressors, and a consistent government effort to protect them is still lacking. There are many knowledge gaps regarding these formations and new studies are needed to support conservation actions involving these ecosystems. Keywords: reef, beachrock, sandstone, intertidal zone, benthos

Comparison of modern and fossil diatom assemblages and their implication on sea-ice conditions in coastal Antarctic region

Antarctic Coastal regions are thought to be characterized by high productivity usually dominated by diatoms. Considering their prime importance in global carbon biological pump, diatom distribution and abundance studies are sparse especially in coastal regions of Antarctica. Biogenic silica is considered to be severely affected by dissolution in the undersaturated ocean water, therefore, combined study of diatom assemblages from water column and those found in the sediments is important. Therefore, we conducted a combined study of sediment diatoms along with surface water diatoms collected from Coastal Antarctica. When the modern assemblages are compared to the fossil record, it is clear the most of the important diatoms from the summer assemblages are not preserved in the underlying sediments. The studies reveal that only F. kerguelensis is common abundant species in both water and sediment which suggests that coastal Antarctic region could be having more open ocean influence. In contrast, the presence of sea ice related diatom species from surface sediment indicate for expansion of sea ice or ice edge adjacent to the water column, however such species were not found in the overlying water samples which could be due to less sea-ice extent.

On the issue of the impact of adverse and dangerous natural processes on the use of coastal recreational areas of the Russian Federation

Adverse and dangerous natural processes are a deterrent factor in the economic, in particular, recreational use of the coastal territories of Russia. They significantly reduce their tourist potential. At the same time, a decrease in the recreational value of territories is one of the consequences of human impact on the natural landscapes of the coastal zone. It seems important to consider the impact of adverse and dangerous natural processes specifically for coastal recreational areas due to their exceptional importance for domestic tourism. It, in turn, plays a huge role both for the economy of Russia and certain regions of our country, and for Russians themselves: tourists and local residents. As a result of the research, for each of the seaside recreational areas available in Russia, the study revealed the most characteristic adverse and dangerous natural processes. Some of them are more or less manifested everywhere, for example, abrasion processes or storms. Others, in particular, seismic threat, are characteristic only for certain coastal territories. Measures to counteract dangerous natural processes are also somewhat similar for all the regions considered. However, when developing measures to counteract adverse and dangerous natural processes, the peculiarities of coastal regions should also be taken into account. Such features include climatic and relief characteristics, the landscapes of the region, the existing structure of human activity and the intensity of economic development of the region, the types of tourism that are characteristic of it, and the level of popularity of the region among recreants, as well as its recreational potential.

Bayesian analyses question the role of climate in Chulmun demography

We investigate the relationship between climatic and demographic events in Korea during the Chulmun period (10,000–3,500 cal. BP) by analyzing paleoenvironmental proxies and 14C dates. We focus on testing whether a cooling climate, and its potential negative impact on millet productivity around the mid 5th-millennium cal. BP, triggered the population decline suggested by the archaeological record. We employ a Bayesian approach that estimates the temporal relationship between climatic events and change-points in the rate of growth in human population as inferred from radiocarbon time frequency data. Our results do not support the climate-induced population decline hypothesis for three reasons. First, our Bayesian analyses suggest that the cooling event occurred after the start of the population decline inferred from the radiocarbon time–frequency record. Second, we did not find evidence showing a significant reduction of millet-associated dates occurring during the cooling climate. Third, we detected different magnitudes of decline in the radiocarbon time–frequency data in the inland and coastal regions, indicating that the even if cooling episodes were ultimately responsible of these population ‘busts’, their impact was most likely distinct between these regions. We discuss our results highlighting the long tradition of mobility-based subsistence strategy in coastal regions as a potential factor contributing to the regional differences we were able to detect.