Biometric Relationship of Tegillarca granosa (Bivalvia: Arcidae) from the Northern Region of the Strait of Malacca

Khalil, Munawar; Ezraneti, Riri; Rusydi, Rachmawati; Yasin, Zulfigar; Tan, Shau Hwai

doi:10.1007/s12601-021-00019-x

Cited by 4 publications

(3 citation statements)

References 36 publications

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…Two rudist spheres have also been observed in the Sarvak Formation (Figures 3-E and 4-A). The shell of most bivalves is composed of aragonite, and some have mixed mineralogy [18,34]. Gastropods are one of the many components of limestone [21,22].…”

Section: Skeletal Carbonate Components (Foraminifera)mentioning

confidence: 99%

Sedimentological Studies of Marine Oil Fields in Order to Reduce Drilling Risk and Environmental Pollution: A Case Study of South of Iran

Abbasi¹,

Pourmorad²,

Mohanty³

et al. 2023

BIJCEES

View full text Add to dashboard Cite

Detailed studies of sedimentology and petrology of oil ﬁelds, especially oil ﬁelds located in the seas, play a very important role in reducing the risk of danger, increasing harvest, and reducing the amount of environmental pollution. The South Pars gas ﬁeld in the waters of the Persian Gulf on the joint border line of Iran and Qatar and on the south coast of Iran has been used as a comprehensive model for this type of study. In these studies, the sedimentary environment and sequential stratigraphy of the Scorpion and Sarvak Formations in the South Pars gas ﬁeld in wells 1 and 3 have been investigated. Microscopic studies and analysis of gamma-ray and acoustic diagrams of these formations have led to the identiﬁcation of 9 facies in three facies belts related to wetland, dam, and open sea. Dam facies have been identiﬁed only in Sarvak formation. This study shows that the facies belts of the abovementioned formations in a ramp platform are also sloping. Sequence stratigraphy of Kazhdomi and Sarvak Formations in the study wells shows that Kazhdomi Formation has one sedimentary sequence (third category cycle) and Sarvak Formation has two sedimentary sequences. The lower boundaries of sequences 1 and 2 and the upper boundary of sequence 3 have type 1 (SB1) discontinuities, and the boundary between sequences 2 and 3 has type 2 (SB2) discontinuities.

show abstract

Section: Skeletal Carbonate Components (Foraminifera)mentioning

confidence: 99%

Sedimentological Studies of Marine Oil Fields in Order to Reduce Drilling Risk and Environmental Pollution: A Case Study of South of Iran

Abbasi¹,

Pourmorad²,

Mohanty³

et al. 2023

BIJCEES

View full text Add to dashboard Cite

show abstract

“…Two rudist spheres have also been observed in the Sarvak Formation (Figures 3E, 4A). The shell of most bivalves is composed of aragonite, and some have mixed mineralogy (18,19).…”

Section: Skeletal Carbonate Components (Foraminifera)mentioning

confidence: 99%

Sedimentological studies of marine oil ﬁelds in order to reduce drilling risk and environmental pollution: a case study of South of Iran

Abbasi,

Pourmorad,

Mohanty

et al. 2023

BIJCEES

View full text Add to dashboard Cite

Detailed studies of sedimentology and petrology of oil fields, especially oil fields located in the seas, play avery important role in reducing the risk of danger, increasing harvest, and reducing the amount of environmentalpollution. The South Pars gas field in the waters of the Persian Gulf on the joint border line of Iran and Qatar andon the south coast of Iran has been used as a comprehensive model for this type of study. In these studies, thesedimentary environment and sequential stratigraphy of the Scorpion and Sarvak Formations in the South Parsgas field in wells 1 and 3 have been investigated. Microscopic studies and analysis of gamma-ray and acousticdiagrams of these formations have led to the identification of 9 facies in three facies belts related to wetland,dam, and open sea. Dam facies have been identified only in Sarvak formation. This study shows that the faciesbelts of the abovementioned formations in a ramp platform are also sloping. Sequence stratigraphy of Kazhdomiand Sarvak Formations in the study wells shows that Kazhdomi Formation has one sedimentary sequence (thirdcategory cycle) and Sarvak Formation has two sedimentary sequences. The lower boundaries of sequences 1 and2 and the upper boundary of sequence 3 have type 1 (SB1) discontinuities, and the boundary between sequences2 and 3 has type 2 (SB2) discontinuities.

show abstract

“…Berdasarkan nilai b diketahui bahwa kerang darah dari ketiga stasiun penelitian memiliki pertumbuhan allometrik negatif. Hal ini identik dengan beberapa hasil penelitian dari beberapa lokasi lainnya, seperti Perairan Bagan Siapi-Api (Dewi et al 2019), Teluk Lada, Selat Sunda (Komala et al 2011), dan Pesisir Selat Malaka (Khalil et al 2021). Variasi dalam nilai koefisien b dan faktor kondisi kerang darah antarlokasi dapat dipengaruhi oleh berbagai faktor, seperti kondisi lingkungan, adaptasi, dan pola makan (Khalil et al 2021).…”

Section: Hubungan Panjang Bobot Dan Faktor Kondisiunclassified

Kondisi Biometrik Kerang Darah, Tegillarca granosa, di Pesisir Pantai Utara Kota Banda Aceh

Zulfahmi

Helmi

Rahmah

et al. 2021

J. Ilmu. Pertan. Indones.

View full text Add to dashboard Cite

The blood clam, Tegillarca granosa (Linnaeus, 1758) is one of the economically important aquatic organisms. Therefore, information related to biometric conditions is crucial as preventive and responsive efforts to manage blood clams. This study aims to analyze the biometric condition of blood clams collected from the northern coast of Banda Aceh City. Blood-clam samples were collected from three locations, namely Alue Naga, Tibang, and Deah Raya. A total of 300 blood clams were observed. The biometric parameters included the distribution of length and weight classes, the relationship between length and weight, condition factors, ratios, and correlations between total weight, meat weight, and shell weight were measured. The results showed that the majority of blood clams found in Deah Raya were in the smaller length and weight classes (30-32 mm and 12,25-17,24 g) compared to those found in Alue Naga (33-35 mm and 17,25-22,24 g) and Tibang (42-44 mm and 22,25-27,24 g). Despite having identical growth patterns (negative allometric) and condition-factor values, the blood clams collected from Alue Naga had higher meat weight ratios than those collected from the other two locations. The correlation values between the weight of the meat and the total weight of the blood clams collected from Deah Raya tends to be lower than those of blood clams obtained from Alue Naga and Tibang, which are 0,55; 0,81; and 0,78, respectively. Keywords: biometric, environmental factor, Deah Raya

show abstract

Biometric Relationship of Tegillarca granosa (Bivalvia: Arcidae) from the Northern Region of the Strait of Malacca

Cited by 4 publications

References 36 publications

Sedimentological Studies of Marine Oil Fields in Order to Reduce Drilling Risk and Environmental Pollution: A Case Study of South of Iran

Sedimentological Studies of Marine Oil Fields in Order to Reduce Drilling Risk and Environmental Pollution: A Case Study of South of Iran

Sedimentological studies of marine oil ﬁelds in order to reduce drilling risk and environmental pollution: a case study of South of Iran

Kondisi Biometrik Kerang Darah, Tegillarca granosa, di Pesisir Pantai Utara Kota Banda Aceh

Contact Info

Product

Resources

About