scholarly journals MEIOFAUNA (FORAMINIFERA) IN SEDIMENTS AND ITS RELATION TO WHITE SANDY BEACH OF SENGGIGI AND WATER CONDITION OFF WEST LOMBOK

2012 ◽  
Vol 4 (1) ◽  
Author(s):  
Kresna T. Dewi ◽  
L. Arifin ◽  
A. Yuningsih ◽  
Y. Permanawati

A development of meiofaunal data (foraminifera) from offshore area of West Lombok was conducted on 20 marine sediment samples. The samples were taken out using a grab sampler in 1997. The purpose of this study was to apply the formula of Foraminiferal Index by Hallock et al. (2003). Another purpose of this study was to recognize its relation of white sands of Senggigi beach that was dominated by Shlumbergerella floresiana. The result of analysis showed that the value of Foraminiferal Index (FI) was varies between 1.22 and 9.81. The low value of FI (<2) was found at sites that were close to the coastal area. The values FI >2 and <4 occur at five stations that gave indication of limited environment for coral growth. Value of FI >4 that showed good water condition was found in an area surrounding small islands of Gili Trawangan, Gili Meno, Gili Air and southern part of the study area. Based on the identification of foraminiferal specimens, the occurrence of Shlumbergerella floresiana was not abundant as it was accumulated in Senggigi beach. This result showed that this species did not come from samples studied but might come from marine sediment adjacent to the Senggigi beachKeywords: Benthic foraminifera, FORAM Index, west Lombok

2012 ◽  
Vol 4 (1) ◽  
Author(s):  
Kresna T. Dewi ◽  
L. Arifin ◽  
A. Yuningsih ◽  
Y. Permanawati

<p>A development of meiofaunal data (foraminifera) from offshore area of West Lombok was conducted on 20 marine sediment samples. The samples were taken out using a grab sampler in 1997. The purpose of this study was to apply the formula of Foraminiferal Index by Hallock et al. (2003). Another purpose of this study was to recognize its relation of white sands of Senggigi beach that was dominated by Shlumbergerella floresiana. The result of analysis showed that the value of Foraminiferal Index (FI) was varies between 1.22 and 9.81. The low value of FI (&lt;2) was found at sites that were close to the coastal area. The values FI &gt;2 and &lt;4 occur at five stations that gave indication of limited environment for coral growth. Value of FI &gt;4 that showed good water condition was found in an area surrounding small islands of Gili Trawangan, Gili Meno, Gili Air and southern part of the study area. Based on the identification of foraminiferal specimens, the occurrence of Shlumbergerella floresiana was not abundant as it was accumulated in Senggigi beach. This result showed that this species did not come from samples studied but might come from marine sediment adjacent to the Senggigi beach</p><p>Keywords: Benthic foraminifera, FORAM Index, west Lombok</p>


2020 ◽  
Vol 17 (2) ◽  
Author(s):  
Eko Saputro ◽  
Lili Fauzielly ◽  
Imelda Rosalina Silalahi ◽  
Winatris Winatris

Sebanyak 20 sampel sedimen dari perairan Teluk Cenderawasih telah digunakan sebagai bahan studi foraminifera, yang bertujuan untuk mengetahui bagaimana sebaran spasial dan struktur komunitas foraminifera di perairan Teluk Cenderawasih. Hasil penelitian menunjukkan komposisi foraminifera planktonik yang terdiri dari 7 Genus dan 13 Spesies sedangkan foraminifera bentonik terdiri dari 57 Genus dan 87 Spesies. Foraminifera planktonik yang paling umum ditemukan karena muncul di seluruh sampel adalah genus Globigerinoides, terutama G. trilobus dan G. ruber. Sedangkan foraminifera bentonik didominasi oleh subordo Rotaliina, dan yang paling banyak ditemukan adalah genus Cibicidiodes dan Lenticulina. Keanekaragaman foraminifera planktonik dan bentonik termasuk dalam kategori tinggi dengan kisaran antara 0.82 – 0.90 (planktonik) dan 0.79 – 0.95 (bentonik). Kemerataan foraminifera planktonik dan bentonik juga termasuk dalam kategori tinggi dengan kisaran antara 0.83 – 0.99 (planktonik) dan 0.82–0.99 (bentonik). Sedangkan untuk dominasi foraminifera planktonik dan bentonik berada dalam kategori rendah dengan kisaran 0.10 – 0.18 (planktonik) dan 0.05 – 0.21 (bentonik). Hal ini menunjukkan bahwa Teluk Cendrawasih meskipun merupakan perairan yang semi tertutup, namun kondisinya masih sangat bagus bagi perkembangan foraminiferaKata Kunci : foraminifera, distribusi spasial, struktur komunitas, dan Teluk Cenderawasih A total of 20 marine sediment samples from Cenderawasih Bay waters have been used for foraminiferal study, . The purpose to describe the spatial distribution and structure of the foraminifera community in the waters of Cenderawasih Bay. The results indicate that marine sediments are composed of 7 genera and 13 species of planktonic foraminifera, and 57 genera and 87 species belong to benthic foraminifera. The most common planktonic foraminifera is Globigerinoides which is found in all location, particularly G. trilobus and G. ruber. Furthermore, benthonic foraminifera is dominated by subordo Rotaliina, particularly genera Cibicidoides and Lenticulina as the most common genera. Diversity of both Planktonic and benthonic foraminifera are categorized as high, the values are between 0.82 and 0.90, and between 0.79 and 0.95 respectively. Planktonic and benthonic foraminiferal evenness are also high with range value between 0.83 and 0.99 (planktonic), and between 0.82 and 0.99 (benthonic). In contrast, dominance of both foraminiferal type are low, between 0.10 and 0.18 for planktonic, and between 0.05 and 0.21 (benthonic).This indicates that despite a semi–enclosed bay, Cendrawasih Bay is still considered as a good environment for foraminiferal community. Keywords: foraminifera, spatial distribution, community structure, and Cenderawasih Bay.


Química Nova ◽  
2009 ◽  
Vol 32 (4) ◽  
pp. 855-860 ◽  
Author(s):  
Eloy Yordad Companioni Damas ◽  
Miriam Odette Cora Medina ◽  
Ana Catalina Núñez Clemente ◽  
Miguel Ángel Díaz Díaz ◽  
Luis González Bravo ◽  
...  

2021 ◽  
Author(s):  
Ellie Pryor ◽  
Ian Hall ◽  
Morten Andersen ◽  
Daniel Babin ◽  
Yue (Merry) Cai ◽  
...  

&lt;div&gt; &lt;p&gt;Sediment provenance is of key importance for understanding transport history and characterising sediment source regions in the marine and terrestrial environment. Radiogenic isotopes are widely used to identify inland and coastal sediment origins. They document changes in detrital terrigenous sediment fluxes which can be related to continental hydrological variability. Understanding sediment sources to the ocean is a pre-requisite before interpreting past climate archives in marine sediment cores.&lt;/p&gt; &lt;/div&gt;&lt;div&gt; &lt;p&gt;&lt;span&gt;South African coastal drainage basins are composed of various geological units, each reflected by different radiogenic isotope signals in the sediment. In addition to the age and nature of their source rocks, the sediment type influences this radiogenic signature.&lt;/span&gt;&lt;/p&gt; &lt;/div&gt;&lt;div&gt; &lt;p&gt;&lt;span&gt;Here, we present a review of the present-day radiogenic isotopic fingerprints of South African river catchments signals from new river sediment samples with the aim to gain a broad spatial coverage of the source rocks in the region and their relative contributions of terrigenous sediment delivered to the ocean. This information will be applied to marine sediment core MD20-3591 (36&amp;#176; 43.707 S; 22&amp;#176; 9.151 E, water depth 2464m), located offshore South Africa which has the potential to record both Agulhas Current and terrestrial variability. The core site receives a significant amount of terrigenous material from the African continents via riverine input. During the last glacial period, these rivers flowed across the continental shelf within a subdued incised valley. The Gourritz River catchment drains the Cape Supergroup and Karoo Supergroup, typical of these southern drainage basins, whereas the eastern Cape rivers drain the Karoo Supergroup geological unit which is capped by the Drakensberg basalts.&lt;/span&gt;&lt;/p&gt; &lt;/div&gt;&lt;div&gt; &lt;p&gt;&lt;span&gt;We are using the knowledge gained from these new South African terrestrial river sediment samples to identify the sources and transport pathways of the terrigenous sediments in MD20-3591. Of particular interest is the sensitivity of the radiogenic isotopic signatures to grain size variabilities and how this relationship can help to define local or distal sediments. These records will allow us to explore variability in regional hydroclimate in relation to the abundant archaeological evidence of cultural and technological innovations of Middle Stone Age humans in southern Africa.&lt;/span&gt;&lt;/p&gt; &lt;/div&gt;


2019 ◽  
Vol 49 (4) ◽  
pp. 434-455
Author(s):  
Mary McGann ◽  
Gregory M. Ruiz ◽  
Anson H. Hines ◽  
George Smith

Abstract We investigated the potential role of ballast sediment from coastal and transoceanic oil tankers arriving and de-ballasting in Port Valdez as a vector for the introduction of invasive benthic foraminifera in Prince William Sound, Alaska. Forty-one ballast sediment samples were obtained during 1998–1999 from 11 oil tankers that routinely discharged their ballast in Prince William Sound after sailing from other West Coast (Los Angeles/Long Beach Harbor, San Francisco Bay, and Puget Sound) or foreign ports (Japan, Korea, and China) where they originally ballasted. Forty of these samples contained benthic foraminifera, including 27 (66%) with the introduced species Trochammina hadai Uchio from nine (81%) of the ships. In all, 59 species were recovered and foraminiferal abundance peaked at 27,000 specimens per gram dry sediment. Of the 41 samples, three were stained and living benthic foraminifera were recovered in all three of them. The entrained foraminifera reflected the number of times ballasting occurred (single or multiple sources), the location of ballasting (estuarine or offshore), and post-acquisition alteration of the sediment (i.e., growth of gypsum crystals at the possible expense of calcareous tests). In temperate regions, sediment samples resulting from single-source ballasting in estuaries (SSBE), multiple-source ballasting in estuaries (MSBE), single-source ballasting offshore (SSBO), and a combination of SSBO and SSBE or MSBE, typically contained increasingly higher species richness, respectively. The potential for foreign species invasion is dependent on the presence of viable candidates and their survivability, their abundance in the ballasting location, and the number of times ballasting occurs, most of which are evident from the ship's ballasting history. We estimate that 442.1 billion to 8.84 trillion living foraminifera were introduced into Port Valdez in a single year, suggesting it is quite likely that an invasive species could be successfully established there. Trochammina hadai is a good example of a successful invasive in Prince William Sound for the following reasons: 1) the species is abundant enough in U.S. West Coast and foreign ports where ballasting occurs that sufficient individuals needed for reproduction may be transported to the receiving waters; 2) Port Valdez, in particular, receives repeated and frequent inoculations from the same source ports where T. hadai is present; 3) large quantities of sediment are taken up by commercial vessels during ballasting and benthic foraminifera occur in abundance in ballast sediment; 4) ballast sediment provides a suitable environment in which benthic foraminifera can survive for extended periods of time during transport; 5) T. hadai flourishes in a wide range of temperatures and environmental conditions that characterize both the ports where ballasting takes place as well as in Port Valdez where de-ballasting occurs; and 6) the species is capable of asexual reproduction and possibly the ability to form a dormant resting stage, both of which have the potential to lower the threshold for colonization. Clearly, ballast sediment is a viable vector for the introduction of T. hadai and other invasives into Alaskan ports and elsewhere worldwide.


2014 ◽  
Vol 896 ◽  
pp. 521-524 ◽  
Author(s):  
Muhammad Farid ◽  
Kirbani Sri Brotopuspito ◽  
Wahyudi ◽  
Sunarto ◽  
Wiwit Suryanto

North Bengkulu district has an area prone to earthquakes, because this area is very closed to the Sumatra subduction zone to the Eurasian tectonic plate. Coastal area in this region is experiencing with the very fast erosion. This is thought to have relation with earthquake-prone zones. This study aims to find the relationship between Ground Shear Strain (GSS) and rate of erosion in the coastal area of North Bengkulu. The data of coastal erosion rate was obtained by overlaying shoreline in 1947 and 2012. The GSS can be obtained by multiplying Seismic Vulnerability Index (SVI) and Peak Ground Acceleration (PGA) values around the shoreline. Seismic Vulnerability Index was obtained by processing microseismic data acquired using three component in short period of seismometers. The PGA was obtained from the historical earthquake and calculated by using Fukushima-Tanaka equation. The results show that the value of GSS varies between 0.0001 to 0.0055, and the SVI values is ranging from 1.2 to 16.1. In addition, we estimated that PGA value is 92 to 120 and the rate of erosion between 3.6 up to 5.8 m/yr. GSS value for each type of coastal is 0.00046 for the fine sandy beach flat, 0.0043 for flat coastal muddy, 0.0001 for flat rocky beaches, 0.0006 for sandy beaches to rugged, 0.0003 for steep rocky lava beach, 0.0014 for steep rocky coast of for clay, 0.0011 for bertufa steep sandy beach stones, and 0.0014 for the steep rocky shore tuffaceous clay. It is found that the GSS value depends on the type of coastal. In this case, flat coastal muddy show highest effect on the GSS. Both SVI and GSS can be estimated to be a quadratic relation to the erosion rate.


1997 ◽  
Vol 30 (5) ◽  
pp. 1037-1050 ◽  
Author(s):  
S. Kartikeyan ◽  
B. Vijayalekshmy ◽  
S. Chandramouleeswaran ◽  
T. P. Rao ◽  
C. S. P. Iyer

2016 ◽  
Vol 22 (1) ◽  
pp. 35
Author(s):  
Hananto Kurnio

Mineable iron sand deposits in Cilacap – southern coastal area of Central Java have certain coastal characteristics that need to be studied in order to understand its depositional environment. With the knowledge of such environment, it can be applied to look for other places prospective of iron sand deposits that have the same characteristics especially recently when Cilacap’s deposits were almost depleted. Coastal characteristics of iron sand deposit in Cilacap is shown by successive sandy beach ridges separated by marshy valleys typical of prograded coasts and by dunes of sand elongated parallel to the shore line with elevation varies from 0 m to 15 m above sea level. The iron sand deposit was derived from denudation of andesite and “Old Andesite Formation” enriched in magnetite and ilmenite minerals in the steep elevated and deeply weathered rock hinterlands of Cilacap. High sediment loads of Serayu Basin in the hinterland (3,500-4,500 ton/km2/year; Citarum River basin only 800-1,200 ton/km2/year) was causing extensive deposition of iron sand in the coastal zone. Key words: coast, characteristic, iron sand, Cilacap Endapan pasir besi yang dapat ditambang di Cilacap – pesisir selatan Jawa Tengah memiliki karakteristik pantai tertentu yang perlu dikaji agar dapat dipahami lingkungan pengendapannya. Dengan pengetahuan tentang lingkungan pengendapan tersebut, dapat diterapkan untuk mencari daerah-daerah lain prospek endapan pasir besi yang memiliki karakteristik yang sama terutama pada akhir-akhir ini ketika endapan Cilacap akan habis. Karakteristik pantai endapan pasir besi di Cilacap dicirikan oleh urutan pematang pantai berpasir yang dipisahkan oleh lembah-lembah berawa khas pantai maju dan oleh gumuk-gumuk pasir memanjang sejajar dengan garis pantai dengan ketinggian bervariasi dari 0 m hingga 15 m dari muka laut. Endapan pasir besi di daerah ini berasal dari proses denudasi andesit dan “Formasi Andesit Tua” yang kaya akan mineral magnetit dan ilmenit pada pedalaman Cilacap dengan kondisi elevasi curam dan batuan sangat terlapukkan. Muatan sedimen yang tinggi dari Cekungan Serayu di pedalaman tersebut (3.500-4.500 ton/km2/tahun; cekungan Sungai Citarum hanya 800-1.200 ton/km2/tahun) menyebabkan pengendapan yang sangat luas pasir besi di wilayah pantai. Kata kunci: pantai, karakteristik, pasir besi, Cilacap


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