2019
DOI: 10.1016/j.ejar.2019.06.003
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Morphometric length-weight relationships of wild penaeid shrimps in Malindi-Ungwana Bay: Implications to aquaculture development in Kenya

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Cited by 10 publications
(7 citation statements)
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“…Moreover, the Indian Ocean has a complex current system with the South Equatorial Current flowing westward across the Indian Ocean and splitting into the Southeast and Northeast Madagascar Current, which can facilitate long-distance larval dispersal as well as generate migration barriers ( Schott et al 2009 ; Otwoma and Kochzius 2016 ; Huyghe and Kochzius 2018 ). Considering the offshore planktonic larval phase (approximately 20 days) of P. monodon ( Motoh 1985 ), a stepping-stone model could explain larval dispersal throughout the entire Indian Ocean over several generations because the period of seasonal monsoons (northeast winds in December/January and southwest winds in July/August) corresponds with the peak P. monodon spawning seasons in the Indian Ocean ( Sk et al 2015 ; Kaka et al 2019 ). Although we do not know the exact divergence time between the ancestral (WIO populations) and the Indo-Polynesian lineage (Sri Lanka, Southeast Asia, Australia, and Fiji), it could have occurred during the late Pleistocene given the lineage divergence timing of other species in this region ( Vogler et al 2012 ; Hui et al 2016 ; Farhadi et al 2017 ; Huyghe and Kochzius 2017 ).…”
Section: Discussionmentioning
confidence: 99%
“…Moreover, the Indian Ocean has a complex current system with the South Equatorial Current flowing westward across the Indian Ocean and splitting into the Southeast and Northeast Madagascar Current, which can facilitate long-distance larval dispersal as well as generate migration barriers ( Schott et al 2009 ; Otwoma and Kochzius 2016 ; Huyghe and Kochzius 2018 ). Considering the offshore planktonic larval phase (approximately 20 days) of P. monodon ( Motoh 1985 ), a stepping-stone model could explain larval dispersal throughout the entire Indian Ocean over several generations because the period of seasonal monsoons (northeast winds in December/January and southwest winds in July/August) corresponds with the peak P. monodon spawning seasons in the Indian Ocean ( Sk et al 2015 ; Kaka et al 2019 ). Although we do not know the exact divergence time between the ancestral (WIO populations) and the Indo-Polynesian lineage (Sri Lanka, Southeast Asia, Australia, and Fiji), it could have occurred during the late Pleistocene given the lineage divergence timing of other species in this region ( Vogler et al 2012 ; Hui et al 2016 ; Farhadi et al 2017 ; Huyghe and Kochzius 2017 ).…”
Section: Discussionmentioning
confidence: 99%
“…Despite extensive knowledge about its life cycle (Carvalho et al, 2015;Boos et al, 2016), there is still a lack of information regarding its estuarine phase (Alfaro-Montoya, 2010). We highlight the studies of Chu et al (1995) in a Chinese estuary, Pérez-Castañeda and Defeo (2002) in a Mexican coastal lagoon and Kaka et al (2019) that approached both estuarine and marine areas from Kenya. The lack of fisheries data regarding its abundance, especially regarding small-scale fisheries, is one of the reasons that made the species be considered as data deficient in Brazil according to the IUCN (International Union for Conservation of Nature) criteria (Boos et al, 2016).…”
Section: Introductionmentioning
confidence: 94%
“…The spines on the rostrum section are commonly used to assess the meristic characteristics of Macrobrachium species and are the main taxonomic characteristics used to identify freshwater prawn species (Wowor and Ng 2007;Adite et al 2013;Chen et al 2015;Kaka et al 2019). The number of serrations under the rostrum (ventral) in almost all male and female specimens was the same.…”
Section: Morphometric and Meristic Characteristicsmentioning
confidence: 99%