Two decades of seagrass area change: Organic carbon sources and stock.

Although seagrass ecosystems provide various ecosystem services, the implications in correspondence with temporal changes of the meadows is lacking. In this study, we analyzed two-decade changes of the seagrass area with the organic carbon storage and the sources at Libong island in Thailand. The seagrass area covered 841 ha in 2019, after two decades of decline (3.2 and 0.6% yr-1 between 2004 and 2009 and 2009-2019, respectively). Although δ13C was not significant between depth layers (p > 0.05), the general trend suggested that the terrestrial source of carbon is dominating bottom depth layer (31.7-37.2%), mixture of terrestrial (19.7-30.3%), seagrass (22.9-29.6%), mangrove (16.8-43.0%) and CPOM (11.2-25.4%) in the middle, and mangroves and seagrasses are dominating surface layer (28.3-66.2 and 29.3-36.5%, respectively). These trends approximately correspond to the areal changes of the meadows, as well as changes of urban area and water quality, providing detailed information on the meadow changes and possible causes.

Nitrification and its influence on biogeochemical cycles from the equatorial Pacific to the Arctic Ocean.

We examined nitrification in the euphotic zone, its impact on the nitrogen cycles, and the controlling factors along a 7500 km transect from the equatorial Pacific Ocean to the Arctic Ocean. Ammonia oxidation occurred in the euphotic zone at most of the stations. The gene and transcript abundances for ammonia oxidation indicated that the shallow clade archaea were the major ammonia oxidizers throughout the study regions. Ammonia oxidation accounted for up to 87.4% (average 55.6%) of the rate of nitrate assimilation in the subtropical oligotrophic region. However, in the shallow Bering and Chukchi sea shelves (bottom ⩽67 m), the percentage was small (0-4.74%) because ammonia oxidation and the abundance of ammonia oxidizers were low, the light environment being one possible explanation for the low activity. With the exception of the shallow bottom stations, depth-integrated ammonia oxidation was positively correlated with depth-integrated primary production. Ammonia oxidation was low in the high-nutrient low-chlorophyll subarctic region and high in the Bering Sea Green Belt, and primary production in both was influenced by micronutrient supply. An ammonium kinetics experiment demonstrated that ammonia oxidation did not increase significantly with the addition of 31-1560 nm ammonium at most stations except in the Bering Sea Green Belt. Thus, the relationship between ammonia oxidation and primary production does not simply indicate that ammonia oxidation increased with ammonium supply through decomposition of organic matter produced by primary production but that ammonia oxidation might also be controlled by micronutrient availability as with primary production.

Nonsynonymous site heteroplasmy in fish mitochondrial DNA.

Heteroplasmic nucleotide polymorphisms are rarely observed in wild animal mitochondrial DNA. The occurrence of such site heteroplasmy is expected to be extremely rare at nonsynonymous sites where the number of nucleotide substitutions per site is low due to functional constraints. This report deals with nonsynonymous mitochondrial heteroplasmy from two wild fish species, chum salmon and Japanese flounder. We detected an A/C nonsynonymous heteroplasmic site corresponding to putative amino acids, Ile or Met, in NADH dehydrogenase subunit-5 (ND5) region of chum salmon. The heteroplasmic site was at the 3rd position of 58th codon. As for Japanese flounder we detected a C/T nonsynonymous heteroplasmic site corresponding to putative amino acids, Leu or Pro, in ND4 region. The heteroplasmic site was at the 2nd position of 450th codon. We also verified heteroplasmy at these sites by sequencing cloned fragments.

SHORT-TERM MEASUREMENT OF CARBON STABLE ISOTOPE DISCRIMINATION IN PHOTOSYNTHESIS AND RESPIRATION BY AQUATIC MACROPHYTES, WITH MARINE MACROALGAL EXAMPLES(1).

Progress in the study of stable isotope discrimination in carbon assimilation by aquatic macrophytes has been slower than for other groups of primary producers, such as phytoplankton and terrestrial plants. A probable reason has been the methodologies employed for such a study: field collections or long-term incubations, both relying on the observation of changes in carbon isotope composition of plant tissue. Here, we present a short-term incubation method based on the change in carbon stable isotope composition in water. Its fundamental advantage over the other approaches is that the change in stable isotope composition in water in a closed system is much faster than in the plant tissue. We applied the method to investigate the relationship between carbon assimilation intensity and isotope discrimination. The results included a relatively small discrimination in respiration, a significant influence of carbon assimilation rate on discrimination, and the suggestion of HCO3 (-) or CO2 uptake in photosynthesis. The information gathered using this method would be difficult to obtain in other ways, and so we believe that it should contribute to a better understanding of the physiology and ecology of aquatic macrophytes.