A Chack List of Penaeid Prawn Found in Indian Water with Their Distribution

Burkenroad created two subgenera of the genus Trachypenaeus viz., Trachypenaeus (Trachypenaeus) and Trachypenaeus (Trachysalambria) in 1934. These two subgenera were raised to the status of genus by Pérez Farfante and Kensley and simultaneously created two new genera for the group namely Megokris and Rimapenaeus. As such the trachypenaeid group of penaeid prawns consists of four valid genera namely Trachypenaeus, Trachysalambria, Megokris and Rimapenaeus. During the present study genus Megokris is being synonymised under its original genus Trachypenaeus. Therefore, the main objective of the present study is to propose a revision to the trachypenaeid group of penaeid prawn and to prepare a comprehensive document for the group recorded from Indian water. The study area represents genus Trachysalambria and Megokris with three species under each genus.

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Changes in the pituitary FSH and LH levels during the oestrous cycle in the Indian water buffalo

Reproduction ◽

10.1530/jrf.0.0270300 ◽

1971 ◽

Vol 27 (2) ◽

pp. 300-301 ◽

Cited By ~ 1

Author(s):

S. Agrarwal ◽

N. Buch

Keyword(s):

Water Buffalo ◽

Oestrous Cycle ◽

Indian Water

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Infrastructures as colonial beachheads: The Central Arizona Project and the taking of Navajo resources

Environment and Planning D Society and Space ◽

10.1177/0263775821991537 ◽

2021 ◽

pp. 026377582199153

Author(s):

Andrew Curley

Keyword(s):

Colorado River ◽

Water Network ◽

Navajo Nation ◽

Political Factors ◽

Indian Water ◽

Central Arizona Project ◽

Indigenous Lands ◽

Archival Documents ◽

Central Arizona ◽

Colorado River Water

Colonial difference is a story of national infrastructures. To understand how colonialism works across Indigenous lands, we need to appreciate the physical, legal, and political factors involved in the building and expanding of national infrastructures in different historical contexts; infrastructures that arrive in some places while denied in others. Using archival documents, this article accounts for the colonial politics necessary to bring Colorado River water into Phoenix and Tucson. It highlights how the following moments worked to enlarge Arizona’s population and power while denying Diné water claims: the 1922 Colorado Compact, Arizona’s 1960s campaign for the Central Arizona Project, and recent Indian water settlements between Arizona and Navajo Nation. The infrastructures that emerged from these events formed a coal–energy–water nexus reliant on Navajo coal while constructing Arizona’s water network. In sum, these projects served as colonial beachheads—temporal encroachments on Indigenous lands and livelihoods that augment material and political difference over time and exacerbate inequalities.

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W chromosome in the Indian water snake (checkered keel back)Natrix piscator (colubridae)

Cellular and Molecular Life Sciences ◽

10.1007/bf02136807 ◽

1968 ◽

Vol 24 (1) ◽

pp. 79-80 ◽

Cited By ~ 6

Author(s):

L. Singh ◽

T. Sharma ◽

S. P. Ray-Chaudhuri

Keyword(s):

W Chromosome ◽

Indian Water ◽

Water Snake

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Modelling Penaeid Prawn Larval Advection in Albatross Bay, Australia: Defining the Effective Spawning Population

Marine and Freshwater Research ◽

10.1071/mf9960157 ◽

1996 ◽

Vol 47 (2) ◽

pp. 157 ◽

Cited By ~ 19

Author(s):

PC Rothlisberg ◽

PD Craig ◽

JR Andrewartha

Keyword(s):

Activity Pattern ◽

Activity Patterns ◽

Circulation Model ◽

Flood Tide ◽

Spatial Extent ◽

3 Dimensional ◽

Penaeid Prawn ◽

Transition Depth

A 3-dimensional numerical circulation model was linked to four larval-postlarval behaviour patterns to establish the origins of postlarvae recruiting into the estuaries adjacent to Albatross Bay, Gulf of Carpentaria, Australia. The area from which these postlarvae originate is called the 'advective envelope' and it delimits the spatial extent of the effective spawning population. The different behaviour scenarios vary the amount of time the postlarvae are active during the flood tide and the depth at which they change between their diel and tidal activity patterns (transition depth). The envelope with a behaviour scenario that incorporated a 20 m transition depth and a 3 h tidal activity pattern was 1000 km2. Incorporation of seasonal winds changed the shape but not the extent of the advective envelopes.

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Environmentally Driven Changes in Fatty Acid Profiles of a Commercially Important Penaeid Prawn

Estuaries and Coasts ◽

10.1007/s12237-018-0461-0 ◽

2018 ◽

Vol 42 (2) ◽

pp. 528-536 ◽

Cited By ~ 5

Author(s):

Matthew D. Taylor ◽

Natalie A. Moltschaniwskyj ◽

Marcus J. Crompton ◽

R. Hugh Dunstan

Keyword(s):

Fatty Acid ◽

Fatty Acid Profiles ◽

Penaeid Prawn ◽

Commercially Important

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Assessment of reliability of extreme wave height prediction models

Natural Hazards and Earth System Science ◽

10.5194/nhess-17-409-2017 ◽

2017 ◽

Vol 17 (3) ◽

pp. 409-421 ◽

Cited By ~ 18

Author(s):

Satish Samayam ◽

Valentina Laface ◽

Sannasiraj Sannasi Annamalaisamy ◽

Felice Arena ◽

Sundar Vallam ◽

...

Keyword(s):

North America ◽

Mediterranean Sea ◽

Wave Height ◽

Prediction Models ◽

North Pacific Ocean ◽

Coastal Hazards ◽

Extreme Wave ◽

Indian Water ◽

Wave Hindcast ◽

Buoy Data

Abstract. Extreme waves influence coastal engineering activities and have an immense geophysical implication. Therefore, their study, observation and extreme wave prediction are decisive for planning of mitigation measures against natural coastal hazards, ship routing, design of coastal and offshore structures. In this study, the estimates of design wave heights associated with return period of 30 and 100 years are dealt with in detail. The design wave height is estimated based on four different models to obtain a general and reliable model. Different locations are considered to perform the analysis: four sites in Indian waters (two each in Bay of Bengal and the Arabian Sea), one in the Mediterranean Sea and two in North America (one each in North Pacific Ocean and the Gulf of Maine). For the Indian water domain, European Centre for Medium-Range Weather Forecasts (ECMWF) global atmospheric reanalysis ERA-Interim wave hindcast data covering a period of 36 years have been utilized for this purpose. For the locations in Mediterranean Sea and North America, both ERA-Interim wave hindcast and buoy data are considered. The reasons for the variation in return value estimates of the ERA-Interim data and the buoy data using different estimation models are assessed in detail.

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