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"Laut Flores memiliki dinamika oseanografi secara historis yang disebabkan oleh pergerakan massa air di dalamnya. Pergerakan massa air laut ini dikenal sebagai fenomena upwelling, dimana air bersuhu dingin dan kaya nutrisi dari kedalaman lautan bergerak menuju permukaan laut. Air laut yang bergerak ke permukaan ini membawa nutrien, yang terukur melalui kadar klorofil-a yang dihasilkan oleh fitoplankton di permukaan laut. Upwelling disebabkan oleh transpor Ekman, yakni transpor arus laut yang terbentuk oleh angin yang bertiup di atas permukaan air laut. Dalam penelitian ini, digunakan data anomali suhu permukaan laut (SSTa) dari NOAA AVHRR Pathfinder Version 5.3 Collated Global, data vektor angin permukaan laut (u dan v) dari ERA5 Copernicus, serta data konsentrasi klorofil (chlor-a) dari Ocean Color SMI dengan rentang tahun 1998 Р2023. Analisis spasial dilakukan dengan melihat variasi spasiotemporal klorofil-a, SSTa dan indeks upwelling. Analisis temporal dilakukan secara time series, dekomposisi dan rerata bulanan tiap variabel. Hasil penelitian menunjukkan fenomena upwelling di Laut Flores utamanya disebabkan oleh pergerakan angin arah barat laut pada musim angin muson timur (April-Oktober), ditandai dengan indeks upwelling positif. Pada periode tersebut, upwelling terjadi di Laut Flores bagian utara dekat Sulawesi Selatan. Upwelling kuat tercatat terjadi pada tahun 2004, 2014, 2015, 2019 dan 2020, dimana perisitwa ini dipengaruhi oleh El Ni̱o.

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The historical of Flores Sea was driven by oceanographic dynamics caused by the movement of water masses within it. This movement of seawater masses is known as the upwelling phenomenon, where cold-temperature, nutrient-rich water from the ocean depths moves towards the sea surface. This surface-moving seawater carries nutrients, which are measured through chlorophyll-a levels produced by phytoplankton at the ocean surface. Upwelling is caused by Ekman transport, which is the transport of water mass formed by wind blowing over the sea surface. This study use the data of sea surface temperature (SSTa) anomaly data from NOAA AVHRR Pathfinder Version 5.3 Collated Global, sea surface wind vector data (u and v) from ERA5 Copernicus, and chlorophyll concentration data (chlor-a) from Ocean Color SMI with time range in 1998 Р2023. Spatial analysis was conducted by analyzing spatiotemporal variations in chlorophyll-a, SSTa and upwelling index. Temporal analysis was done by time series analysis, decomposition and monthly average of each variable. The results showed that the upwelling phenomenon in the Flores Sea is mainly caused by northwest wind movements during the east monsoon season (April РOctober), characterized by a positive upwelling index. During this period, upwelling occurs in the northern Flores Sea near South Sulawesi. Strong upwelling was recorded in 2004, 2014, 2015, 2019 and 2020, where this event was influenced by El Ni̱o."

"Upwelling adalah proses penting yang mengangkut nutrisi ke sistem biologis yang terkait dengan jaring makanan di kolom air. Penelitian ini bermaksud untuk menyelidiki karakteristik fenomena upwelling dengan menganalisis kesuburan historis perairan Banggai melalui dua indikator utama, yaitu suhu permukaan laut (SST), dan klorofil-a, menggunakan data citra satelit, serta melihat hubungan antara fenomena upwelling dan produksi perikanan tangkap di perairan Banggai. Analisis dilakukan dengan data resolusi spasial 4 kilometer menggunakan SST (NOAA AVHRR Pathfinder Version 5.3 Collated Global), data konsentrasi klorofil (Ocean Color SMI), dan analisis regresi polinemal untuk menguji hubungan fenomena upwelling dengan produksi perikanan tangkap. Hasil pola dispersi klorofil-a dari tahun 1998 hingga 2022 dikumpulkan pada bulan Agustus 2004, 2006 dan 2015, dengan konsentrasi klorofil rata-rata 0,49 mg/m3 dan kisaran suhu permukaan laut 23–24°C. Hasil trend dekomposisi dari sebaran klorofil-a konsentrasi tinggi di perairan Banggai, pola upwelling terjadi setahun sekali pada setiap bulan Agustus. Sementara itu, dekomposisi suhu permukaan laut pada grafik tren musiman menunjukkan nilai yang rendah, dan suhu tersebut dapat meningkat tiga kali lipat dalam satu tahun. Hal ini terkait dengan periode El-Nino. Berdasarkan penelitian ini, persebaran klorofil-a di Banggai paling besar terjadi pada periode El Nino. Pengaruh hubungan antara fenomena upwelling dengan jumlah ikan yang ditangkap melalui grafik fluktuasi tidak menunjukkan pengaruh yang signifikan.

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Upwelling is an important process that transports nutrients to biological systems linked to food webs in the water column. This study intends to investigate the characteristics of the upwelling phenomena by analyzing the historical fertility of Banggai waters via two key indicators, namely sea surface temperature (SST), and chlorophyll-a, using satellite imagery data, as well as looking at the relationship between the phenomenon of upwelling and capture fisheries production in Banggai waters. The analysis was conducted with a data spatial resolution of 4 kilometers using SST (NOAA AVHRR Pathfinder Version 5.3 Collated Global), chlorophyll concentration (Ocean Color SMI) data, and polynemal regression analysis to examine the relationship of the upwelling phenomenon with capture fisheries production. Results of chlorophyll-a dispersion patterns from 1998 to 2022 were collected in August 2004, 2006 and 2015, with an average chlorophyll concentration of 0.49 mg/m3 and a sea surface temperature range of 23–24°C. The result of trend decomposition from the distribution of high concentrations of chlorophyll-a in Banggai waters, the pattern of upwelling occurs once a year in every August. Meanwhile, the decomposition of sea surface temperature on the seasonal trend chart shows a low value, and the temperature can increase three times in one year. This is related to the El-Nino period. Based on this study, the chlorophyll-a distribution in Banggai was greatest during the El Nino period. The effect of the relationship between the upwelling phenomenon and the amount of fish caught through the fluctuation graph does not show a significant effect."

"Synaptidae was one of holothuroidea member, unique because they has no podia or tube feet in their surface of body wall and has no respiratory trees in their internal organ. They has anchor shape spicules in their body wall that supporting locomotory function. Synaptidae were frequently found in the sea grass area, but no publication was specifically observed their existence. This study proposed to observed the species of synaptidae in Sanur Beach-Bali, included their length distribution and their vegetation preference to live with. The observation was conducted twice time using swept survey time based method (one hour) on low tide. The results shows 46 individual of synaptidae consist of two species (Synapta maculata and Opheodesoma grisea) found in the intertidal zone of Sanur Beach-Bali. In the first observation, most of synaptidae had shorter body length then in the second observation. Almost all of synaptidae observed was associated with Enhalus acoroides. Synaptidae in the study area adapt to a very extrem environment. Their adaptation were: 1) osmoregulation to the fluctuation of salinity; 2) wide tolerance of temperature fluctuation; defense mechanism to the wave motion by 3) having sticky skin and 4) autotomy mechanism. "

"Green tides are usually induced by water eutrophication. An acceleration of chemical inputs that influence algal population, especially Ulva. The increase of nitrogen and phosphorus is the main factor in green tides. Ulva is very efficient to proliferate by fragmentaion and creates such blooms, some species were documented on green tide occurrences in several regions, namely: Ulva lactuca, U. rigida, U. olivascens, U. gigantea, U. curvata, U. rotundata, U. scandinavica, U. pseudocurvata, U. armoricana, U. prolifera, U. reticulata. Generally, green tides have negative impact on marine ecosystem, human health and economic. Green tides also impact the fishing and aquaculture activities, dead alga can produce hydrogen sulfide which can cause animals and humans death"

"Penilia avirostris, Kladosera laut kosmopolitan. Penilia avirorostris adalah salah satu jenis dari delapan jenis Kladosera yang hidup di laut sebagai zooplankton. Walaupun keanekaragaman kladosera sangat rendah di perairan marin, namun distribusi jenis-jenisnya sangat luas mulai dari perairan hangat sampai perairan beriklim sedang (temperate). Penilia avirostris memiliki kemampuan reproduksi secara partenogenesis dan gametogenesis. Ketika kondisi lingkungan mendukung kehidupan (favorable) maka reproduksi dilakukan secara partenogenesis, sebaliknya ketika lingkungan kurang mendukung maka akan bereproduksi secara gametogenesis. Kemampuan beradaptasi yang tinggi terhadap kondisi lingkungan ekstrim dengan cara dormansi atau hibernasi, diduga sangat berpengaruh terhadap semakin luasnya daerah persebaran. "