Spatial and Short-Term Temporal Patterns of Octocoral Assemblages in the West Philippine Sea

Octocorals are relatively understudied than other coral reef organisms despite their ecological and economic values. The Philippines is known to have high marine biodiversity, but information on octocorals is lacking. This study investigated spatial and temporal variations in the assemblage of octocorals in selected reef sites in the West Philippine Sea (WPS)- the Kalayaan Island Group (i.e., Pag-asa, Sabina, Lawak, and Northeast Investigator) and Ulugan in 2017 and 2019. Results showed high octocoral taxonomic richness (at least 10 families) in the study sites. Mean percent octocoral cover in WPS was 5.35% SE ± 0.55, with Sabina having the highest octocoral cover in both years. Significant differences in octocoral cover were observed among sites in both years, but among-station differences were only observed in 2017. Octocoral assemblage also differed among sites in both years (ANOSIM: R > 0.5, p < 0.05), wherein different octocoral taxa dominated in different sites. In particular, variations were driven by high cover of holaxonians, nephtheids, and coelogorgiids in Sabina, and clavulariids, tubiporiids, and xeniids in Northeast Investigator in 2017. In 2019, significant variations were driven by high cover of helioporiids in Pag-asa, while Sabina had higher abundance of holaxonians, nephtheids, alcyoniids, and xeniids. Short-term temporal variation on octocoral cover in monitoring stations in Pag-asa was not observed (Kruskal-Wallis, p > 0.05), although the overall mean octocoral cover increased from 1.23% ± SE 0.47 in 2017 to 2.09% SE ± 0.37 in 2019. Further, there was no significant change in the octocoral assemblage in Pag-asa between years (ANOSIM, R = 0.11, p = 0.07). This study highlights high octocoral taxonomic richness in the WPS relative to other sites in the Indo-Pacific Region and provides baseline information on the octocoral assemblages, which can be useful for future ecological studies and marine biodiversity conservation efforts.

Tintinnids (Ciliophora, Oligotrichea) within power plant discharge and marine protected areas in Masinloc-Oyon Bay

There are only five studies on tintinnids of the Philippines. We present a checklist of tintinnids (Ciliophora, Oligotrichea) from Masinloc-Oyon Bay, Province of Zambales, West Philippine Sea. Masinloc-Oyon Bay is a unique in having both marine protected areas and a coal-fired thermal power plant within the same bay. Field sampling was performed in July 2017, which recorded 10 species belonging to one order, six families, and seven genera. Station 1 inside the power plant’s outfall had the lowest diversity, whereas the stations within marine protected areas had a relatively higher species diversity index. Our new data are the first records of tintinnid species in Masinloc-Oyon Bay. These records add to the regional checklist of the Philippine Sea.

Infodemics and Deadly Racist Viruses: covid-19 Response in the Chinese-Filipino Community

In the last decade, the Philippines has experienced an escalation of anti-Chinese sentiment due to many factors, founded and unfounded. The growing presence of illegal immigrants and crimes associated with them; an increase in the number of Chinese workers, who are perceived as competing with Filipino workers; an increase in Chinese businesses, especially in retail, some operating without permits; the continuing dispute between China and the Philippines over the islands in the West Philippine Sea; President Rodrigo Duterte’s China pivot policy and what has been deemed as favoring China to the detriment of the Philippines. This confluence of events has served to worsen the image of China. The covid-19 pandemic and the way the government responded to it worsened the sinophobia directed at anyone considered “Chinese,” including Filipinos of Chinese ancestry. This paper explores the racism vented against the Chinese and how the local Chinese-Filipino community has responded with positive action to help mitigate the anti-Chinese wave.

The Imperial Japanese Navy and the battle of the Philippine Sea: An analysis of the main causes of defeat

This article aims to demonstrate through mathematical analysis that the primary reason for the defeat of the Imperial Japanese Navy (IJN) in the battle of the Philippine Sea during World War II (WWII) was quantitative, and that the defeat is particularly attributable to the lack of force concentration. Scholars have placed much emphasis on the qualitative aspects of the forces involved, such as the skill of IJN pilots or the air defence capabilities of the United States Navy (USN), in seeking to explain the Japanese defeat. We, however, assert that in this naval battle, quantitative factors played a more important role than qualitative ones. Accordingly, we offer an improved version of the mathematical model of Armstrong and Powell, which was previously used to analyse battles between aircraft carriers (CVs). The coefficients in our mathematical model will then be estimated and verified using historical data from the main battles between CVs of the IJN and USN during WWII. Finally, we will analyse the factors underlying the IJN’s defeat in the Battle of the Philippine Sea using the model. This study proposes a useful technique for evaluating quantitative and qualitative aspects of naval forces.

Active Carbon Flux of Mesozooplankton in South China Sea and Western Philippine Sea

The active carbon flux mediated by diel vertical migration (DVM) of zooplankton is an important component of the downward carbon flux in the ocean. However, active fluxes transported by zooplankton DVM are poorly known in the South China Sea (SCS) and the Western Philippine Sea (WPS). In this study, active carbon fluxes in the SCS and WPS were evaluated on the basis of the data of mesozooplankton community and DVM at two stations of these areas. The mesozooplankton community in the SCS was obviously different from that in the WPS, and higher species number and abundance in the SCS were observed, which may be related to the higher chlorophyll a (Chl a) concentration and the wide gradients of temperature and salinity in this sea. Moreover, shallow depth Chl a maximum and strong thermocline were detected in the SCS, causing lower migration amplitudes of mesozooplankton in the SCS than those in the WPS. However, the migrant biomass of mesozooplankton in the SCS was 98.40 mg C m–2, higher than that in the WPS at 25.12 mg C m–2. The mesozooplankton active carbon flux in the SCS (4.64 mg C m–2⋅d–1) was also higher than that in the WPS (1.80 mg C m–2⋅d–1). The mesozooplankton active fluxes were equivalent to 8.3 and 8.1% of the total flux (active flux plus passive flux) of the SCS and WPS, respectively, and they play an important role in the biological pump functioning in the two regions.