Chemosensory Ecology of Oyster Larvae: Benthic-Pelagic Coupling

2021 ◽  
pp. 37-50
Author(s):  
Richard K. Zimmer-Faust ◽  
Mario N. Tamburri ◽  
Alan W. Decho
Author(s):  
Toshiyuki TAKAO ◽  
Osamu SHIMOZAWA ◽  
Kazuo MURAKAMI ◽  
Ikuo ABE ◽  
Tomonari OKADA ◽  
...  

2021 ◽  
Vol 61 ◽  
pp. 101208
Author(s):  
Swagata Sinha ◽  
Arnab Banerjee ◽  
Nabyendu Rakshit ◽  
Akkur V. Raman ◽  
Punyasloke Bhadury ◽  
...  

Hydrobiologia ◽  
2009 ◽  
Vol 629 (1) ◽  
pp. 147-156 ◽  
Author(s):  
Robinson W. Fulweiler ◽  
Scott W. Nixon

PLoS ONE ◽  
2012 ◽  
Vol 7 (8) ◽  
pp. e44155 ◽  
Author(s):  
Martin Ubertini ◽  
Sébastien Lefebvre ◽  
Aline Gangnery ◽  
Karine Grangeré ◽  
Romain Le Gendre ◽  
...  

2015 ◽  
Vol 282 (1817) ◽  
pp. 20152025 ◽  
Author(s):  
Elias Broman ◽  
Martin Brüsin ◽  
Mark Dopson ◽  
Samuel Hylander

Many coastal marine systems have extensive areas with anoxic sediments and it is not well known how these conditions affect the benthic–pelagic coupling. Zooplankton lay their eggs in the pelagic zone, and some sink and lie dormant in the sediment, before hatched zooplankton return to the water column. In this study, we investigated how oxygenation of long-term anoxic sediments affects the hatching frequency of dormant zooplankton eggs. Anoxic sediments from the brackish Baltic Sea were sampled and incubated for 26 days with constant aeration whereby, the sediment surface and the overlying water were turned oxic. Newly hatched rotifers and copepod nauplii (juveniles) were observed after 5 and 8 days, respectively. Approximately 1.5 × 10 5 nauplii m −2 emerged from sediment turned oxic compared with 0.02 × 10 5 m −2 from controls maintained anoxic. This study demonstrated that re-oxygenation of anoxic sediments activated a large pool of buried zooplankton eggs, strengthening the benthic–pelagic coupling of the system. Modelling of the studied anoxic zone suggested that a substantial part of the pelagic copepod population can derive from hatching of dormant eggs. We suggest that this process should be included in future studies to understand population dynamics and carbon flows in marine pelagic systems.


1999 ◽  
Vol 56 (9) ◽  
pp. 1679-1686 ◽  
Author(s):  
Frank M Wilhelm ◽  
Jeff J Hudson ◽  
David W Schindler

We estimated the net P transport by Gammarus lacustris from the benthic to pelagic regions of a fishless alpine lake and compared it with P regeneration by the entire plankton community. Gammarus lacustris released between 5.2 and 18.1 ng P·L-1·h-1 (adults only and adults plus immatures, respectively) in the pelagic region during nighttime vertical migration. Additional P released into and removed from the water column due to predation on zooplankton was estimated at 1.87 and 2.3 ng P·L-1·h-1, respectively. The net daily regeneration of 52.2-181.4 ng P·L-1·day-1 by the G. lacustris population represented 9.5-32.9% of the total P regenerated by the planktonic community. The majority of the P released by G. lacustris represents "new" P to the pelagic zone because it originated in sediments. We conclude that G. lacustris can represent an important link in benthic-pelagic coupling in oligotrophic mountain lakes.


2018 ◽  
Author(s):  
Ricardo Augusto Scrosati ◽  
Julius A. Ellrich

Benthic–pelagic coupling refers to the ecological relationships between benthic and pelagic environments. Studying such links is particularly useful to understand biological variation in intertidal organisms along marine coasts. Filter-feeding invertebrates are ecologically important on marine rocky shores, so they have often been used to investigate benthic–pelagic coupling. Most studies, however, have been conducted on eastern ocean boundaries. To evaluate benthic–pelagic coupling on a western ocean boundary, we conducted a 5-year study spanning 415 km of the Atlantic coast of Nova Scotia (Canada). We hypothesized that the summer size of intertidal barnacles (Semibalanus balanoides) recruited in the preceding spring would be positively related to the nearshore abundance (biomass) of phytoplankton, as phytoplankton constitutes food for the nauplius larvae and benthic stages of barnacles. Every year between 2014 and 2018, we measured summer barnacle size in clearings created before spring recruitment on the rocky substrate at eight wave-exposed locations along this coast. We then examined the annual relationships between barnacle size and chlorophyll-a concentration (Chl-a), a proxy for phytoplankton biomass. For every year and location, we used satellite data to calculate Chl-a averages for a period ranging from the early spring (when most barnacle larvae were in the water) to the summer (when barnacle size was measured after weeks of growth following spring benthic recruitment). The relationships were always positive, Chl-a explaining nearly half, or more, of the variation in barnacle size in four of the five studied years. These are remarkable results because they were based on a relatively limited number of locations (which often curtails statistical power) and point to the relevance of pelagic food supply to explain variation in intertidal barnacle size along this western ocean boundary coast.


Author(s):  
Wenyan Zhang ◽  
Andreas Neumann ◽  
Ute Daewel ◽  
Kai Wirtz ◽  
Justus E.E. Beusekom ◽  
...  

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