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"ABSTRACTThe genus Ulva (Phyllum Chlorophyta, Family Ulvaceae) is a kind of green seaweed which has been exploited for many purposes is very rich in bioactive compounds that are important for medical purposes, such as anti coagulan, anti cancer; anti oxidant, anti microbial and anti influenza. Ulva has been used for a long time but still lack of cultivation techniques lnformation about the characteristics and biological aspects of Ulva is important for basis technology of Ulva cultivation, including reproductive biology, habitat, distribution and commercial uses of Ulva. The technology of Ulva cultivation is expected to reduce exploitation of Ulva in the wild."

"ABSTRACTThe algal blooms or red tide that resulting mass mortality of fish and other biota are frequently occurred in coastal water: where human activities and population increase in significant. The impacts not only to marine life and environmental quality, but also impact on the fishery economic, food security and health consumer; and also psychology of the surrounding community. In some countries the impact of aquatic disaster has resulted in human fatalities after consuming fishery products. The incidence of red tide phenomenon is characterized by the appearance of other colors in the surface water such as red, red-brown or greenish depending on the causative speciean fact, the incidence of algal bloom has a connection with the amount of nutrients concentration in the waters, which sourced from human activities in the upland, domestic waste, agricultural, industrial waste, etc, which run into the water via rivers or run off 0n the other hand, the increasing eutrophication may lead to alteration of nutrients composition in the waters and can trigger the bloom of toxic species in the waters (toxic algal bloom)."

"ABSTRACTThere is a long history of marine research in Indonesia, starting from mid December 1905 when Dr. J. C. Koningsbergena terrestrial zoologist,established the Visscherii Laboratorium te Batavia (Jakarta F ishery Laboratory) at Jalan Akuarium Pasar Ikan, Jakarta. During its development this institution, which was the forerunner of the Research Center for Oceanography LIPI, underwent a series of name changes, the development of its tasks and fimctions, and improvements in its institutional status font branch to national level. There were also changes in how the institution was administered, and it finally came under the auspices of the Indonesian Institute of Sciences, which was established under the Decree of the President of Republic of Indonesia Number 128/1967, 23 August 1967. To support research activities, this marine research institution has had several research vessels since it first began and, to cover Indonesian waters more widely, it also established Marine Research Stations or Technical Implementation Units in several other parts of Indonesia. Historical events happen only once and are never repeated exactly the same again, yet they can determine people Is lives, and still be remembered for all time. As the oldest institution for marine research in Indonesia, at 110 years (mid December 1905 mid December 2015), it is valuable to have an archive of facts and information about significant historical milestones, about its founder; its development, and the history of marine research in Indonesia. In addition, this is essential information for leaders and employees of the Research Center for Oceanography LIPI, both now and in the future, and may also benefit the academic community in general."

"Karang Unarang adalah perairan perbatasan Indonesia dan Malaysia yang selama masih disengketakan sehingga perlu dilaksanakan patroli guna terciptanya keamanan. Pemilihan jenis Kapal Patroli untuk melaksanakan operasi di perbatasan ini sangant perlu disesuaikandengan keadaan hidro-oseonografi dan potensi ancaman yang dihadapi. Penelitian terkait pemilihan jenis kapal patroli yang ditugaskan untuk melaksanakan operasi di perairan Karang Unarang sangat diperlukan. Pengambilan keputusan tentang jenis kapal patroli tidak menempatkan kriteria sebagai suatu hierarki karena ada hubungan saling memengaruhi antarkriteria yang ditentukan. Keterkaitan ini bisa terjadi antar subkriteria yang terdapat di dalam kriteria (Innerdependece) dan keterkaitan antarelemen yang berbeda (outerdependence). Hasil penelitian menggunakan ANP ini didapatkan sesuai dengan apayang tertera dalam bobot nilai pada data yang menggunakan tools superdecisions sebagai alternatif terbaik terkait jenis kapal patroli yang harus melaksanakan operasi."

"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."

"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."

"ABSTRACTFishing activities currently require good management, in order to meet the protein needs of the community. Knowledge on the distribution pattern of fishes related to the condition of marine waters is one way of good management efforts. Several oceanographic parameters that can affect the distribution of fishes are SST (Sea Surface Temperature), chlorophyll a, salinity, and others. Each type offish has different optimal level of particular oceanographic parameters. The distribution of oceanographic parameters are effected by West monsoon, East monsoon and the season inbetween. Therefore, by studying oceanographic parameters on a regular basis, we can determine the fishing areas."

"ABSTRACTMECHANISM OF GENETIC DISORDER AND MUTATION ON BIVALVES INFLUENCED BY LEAD. Bivalves have a feeding mechanism of suspension-feeder or deposit-feeder or both, making bivalves consume the material contained in either beneficial or toxic water. Bivalve can survive even with the condition of polluted waters, including the concentration of heavy metals that exceed a specified threshold. Lead is one type of harmful pollutants originating from anthropogenic activities and contaminated marine waters. The purpose of this paper is to provide knowledge about the process or mechanism of bivalves to defend itself against lead, which can be found in their environment, especially genetic disorders and mutations that may be experienced by marine bivalves as a result of exposure to lead."