GLORIA

GEOMAR Library Ocean Research Information Access

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Frontiers Media SA  (2)
  • Joo, HuiTae  (2)
  • 1
    Online Resource
    Online Resource
    Frontiers Media SA ; 2022
    In:  Frontiers in Marine Science Vol. 9 ( 2022-9-29)
    In: Frontiers in Marine Science, Frontiers Media SA, Vol. 9 ( 2022-9-29)
    Abstract: The biochemical compositions of marine particulate organic matter (POM) can provide significant information to understanding the physiological conditions of phytoplankton and food quality for their potential consumers. We investigated the seasonal variations in biomolecular and amino acid (AA) compositions of the bulk POM in the southwestern East/Japan Sea from four different sampling months (February, April, August, and October) in 2018. In terms of the biomolecular composition of the POM, overall carbohydrates (CHO) were predominant among three biomolecules accounting for 48.6% followed by lipids (LIP; 35.5%) and proteins (PRT; 15.9%) in the East/Japan Sea. However, markedly seasonal differences in the biomolecular composition of POM were found from February to October, which could be due to seasonally different conditions favorable to phytoplankton growth. Dominant AA constituents to trace POM lability were glycine (GLY), alanine (ALA), and glutamic acid (GLU), suggesting that our POM was the mixtures of decomposing and fresher materials. Furthermore, the significantly negative correlation between the proportion of total essential amino acids (EAAs) and PRT composition (r = -0.627, p & lt; 0.01) was probably reflected by nutrient availability to phytoplankton partitioning EAAs or non-essential AAs (NEAAs). The different biomolecular compounds under un- or favorable growth conditions for phytoplankton could determine the nutritional quality of POM as potential prey as well as degradation status of POM. Therefore, the biochemical compositions of phytoplankton-originated POM hold important ecological implications in various marine ecosystems under ongoing climate changes.
    Type of Medium: Online Resource
    ISSN: 2296-7745
    Language: Unknown
    Publisher: Frontiers Media SA
    Publication Date: 2022
    detail.hit.zdb_id: 2757748-X
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Online Resource
    Online Resource
    Frontiers Media SA ; 2022
    In:  Frontiers in Marine Science Vol. 9 ( 2022-6-15)
    In: Frontiers in Marine Science, Frontiers Media SA, Vol. 9 ( 2022-6-15)
    Abstract: Nitrous oxide (N 2 O) is an important greenhouse gas emitted in significant volumes by the Pacific Ocean. However, the relationship between N 2 O dynamics and environmental drivers in the subtropical western North Pacific Ocean (STWNPO) remains poorly understood. We investigated the distribution of N 2 O and its production as well as the related mechanisms at the surface (0–200 m), intermediate (200–1500 m), and deep (1500–5774 m) layers of the STWNPO, which were divided according to the distribution of water masses. We applied the transit time distribution (TTD) method to determine the ventilation times, and to estimate the N 2 O equilibrium concentration of water parcels last in contact with the atmosphere prior to being ventilated. In the surface layer, biologically derived N 2 O (ΔN 2 O) was positively correlated with the apparent oxygen utilization (AOU) (R 2 = 0.48), suggesting that surface N 2 O may be produced by nitrification. In the intermediate layer, ΔN 2 O was positively correlated with AOU and NO 3 − (R 2 = 0.92 and R 2 = 0.91, respectively) and negatively correlated with nitrogen sinks (N * ) (R 2 = 0.60). Hence, the highest ΔN 2 O value in the oxygen minimum layer suggested N 2 O production through nitrification and potential denitrification (up to 51% and 25% of measured N 2 O, respectively). In contrast, the deep layer exhibited a positive correlation between ΔN 2 O and AOU (R 2 = 0.92), suggesting that the N 2 O accumulation in this layer may be caused by nitrification. Our results demonstrate that the STWNPO serves as an apparent source of atmospheric N 2 O (mean air−sea flux 2.0 ± 0.3 μmol m -2 d -1 ), and that nitrification and potential denitrification may be the primary mechanisms of N 2 O production in the STWNPO. We predict that ongoing ocean warming, deoxygenation, acidification, and anthropogenic nitrogen deposition in the STWNPO may elevate N 2 O emissions in the future. Therefore, the results obtained here are important for elucidating the relationships between N 2 O dynamics and environmental changes in the STWNPO and the global ocean.
    Type of Medium: Online Resource
    ISSN: 2296-7745
    Language: Unknown
    Publisher: Frontiers Media SA
    Publication Date: 2022
    detail.hit.zdb_id: 2757748-X
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...