Publications by authors named "Akira Tsujimoto"

Chlorinated paraffins (CPs) readily deposit in sediments upon entering estuaries and adjacent seas. Time-series investigations are indispensable for the long-term monitoring of historical releases and identifying CPs of emerging concerns in the marine environment. In this study, short-, medium-, and long-chain CPs (SCCPs, MCCPs, and LCCPs) were investigated using time-of-flight high-resolution mass spectrometry (ToF-HRMS) in sediment cores, dated between the 1920s and the 2010s sampled from Hong Kong waters and Lingdingyang of the Pearl River Estuary (PRE), South China.

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Citizen science can play an important role in addressing the issue of marine debris. However, citizen science data are often composed of inconsistent methods compared to data collected by experts. In this study, we applied beach cleanup data, collected in different survey years at different survey sites, to a hierarchical Bayesian model to elucidate the factors affecting the distribution of beach litter.

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Article Synopsis
  • Plastic pollution is a major environmental issue in the Anthropocene, causing visual and physical harm along with releasing harmful chemicals.
  • Despite the importance of benthic foraminifera in ecosystems, only a tiny fraction (0.4%) of studies have looked into the effects of micro- and nano-plastics on them.
  • The authors recommend including benthic foraminifera in future plastic pollution research to better understand their responses and to use them as indicators of pollution levels for effective coastal ecosystem management.
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A large-scale sluice gate, which was built in southwest Japan as a national project to reclaim and desalinate lagoon water in 1974, was removed between 2005 and 2009. To examine the impact of this removal on both Nakaumi Lagoon and the nearby coastal waters, we analyzed the foraminiferal assemblages of a coastal sediment core and of samples obtained during 10 years of lagoon monitoring (2001-2010). Detailed Pb dating of the sediment core revealed an increased sediment accumulation rate in the coastal waters, implying that discharge of fine-grained materials, including organic matter, was facilitated by removal of the sluice gate.

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We gathered total organic carbon (%) and relative abundances of benthic foraminifera in intertidal areas and transitional waters from the English Channel/European Atlantic Coast (587 samples) and the Mediterranean Sea (301 samples) regions from published and unpublished datasets. This database allowed to calculate total organic carbon optimum and tolerance range of benthic foraminifera in order to assign them to ecological groups of sensitivity. Optima and tolerance range were obtained by mean of the weighted-averaging method.

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This work contributes to the ongoing work aiming at confirming benthic foraminifera as a biological quality element. In this study, benthic foraminifera from intertidal and transitional waters from the English Channel/European Atlantic coast and the Mediterranean Sea were assigned to five ecological groups using the weighted-averaging optimum with respect to TOC of each species. It was however not possible to assign typical salt marsh species due to the presence of labile and refractory organic matter that hampers TOC characterization.

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Controlling the characteristics of photon emission represents a significant challenge for both fundamental science and device technologies. Research on microcavities, photonic crystals, and plasmonic nanocavities has focused on controlling spontaneous emission by way of designing a resonant structure around the emitter to modify the local density of photonic states. In this work, we demonstrate resonantly enhanced emission using luminescent nanostructured waveguide resonance (LUNAR).

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Article Synopsis
  • An analysis of microfossil records from 150 studies reveals that human-induced marine ecosystem degradation began earlier in Europe and North America (around the 1800s) compared to Asia (after 1900), largely due to earlier industrialization.
  • The results indicate that this degradation accelerated globally post-World War II, driven by economic growth, with recovery efforts showing limited success in some areas.
  • Nutrient enrichment, leading to eutrophication and hypoxia, was identified as the primary cause of degradation, along with other significant factors such as metal pollution, water acidification, and alterations in salinity from construction activities.
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  • Atmospheric carbon dioxide levels and climate changes over geological times are influenced by volcanic outgassing and weathering processes, specifically the breakdown of silicate and organic-carbon rocks.
  • A study presented a 53-million-year record of carbonate accumulation from the equatorial Pacific Ocean, showing that the calcium carbonate compensation depth has increased from approximately 3.0-3.5 km to 4.6 km over time, indicating long-term ocean cooling and increased weathering.
  • The research identified significant fluctuations in the carbonate compensation depth during the middle and late Eocene, attributing these changes to variations in weathering and how organic carbon was delivered to the oceans.
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8-oxoguanosine, which is derived from the oxidation of guanosine (dG), is known to induce transversion mutations (G:C-->T:A) in DNA. The compounds with a small molecular weight for recognizing 8-oxoG were designed on the basis of the structure of the G-clamp, which is reported to have selective affinity toward guanosine. The G-clamp derivatives with the additional binding units toward 8-oxoG were effectively synthesized and named "8-oxoG-clamps.

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8-Oxoguanosine (8-oxoG) is derived from the oxidation of guanosine (dG) and is known to induce transversion mutations (G:C to T:A) in DNA. We have already reported the fluorescent probe "8-oxoG-clamp", which shows a selective fluorescence quenching phenomenon toward 8-oxoG. In this study, attachment of an additional fluorophore to 8-oxoG-clamp was investigated as a strategy for the detection of 8-oxoG by a fluorescence color change attributed to the 8-oxoG-clamp.

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8-Oxoguanosine, which is derived by the oxidation of guanosine (dG), is known to induce transversion mutations (G:C-->T:A) in DNA. The compounds with small molecular weight for recognizing 8-oxoG were designed on the basis of the structure of the G-clamp, which is reported to have selective affinity toward guanosine. The G-clamp derivatives with the additional binding units toward 8-oxoG were effectively synthesized and named "8-oxoG-clamps".

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