scholarly journals Spatial and temporal habitat partitioning by calliphorid blowflies

2018 ◽  
Vol 33 (2) ◽  
pp. 228-237 ◽  
Author(s):  
G. Arias‐Robledo ◽  
J. R. Stevens ◽  
R. Wall
Keyword(s):  
2019 ◽  
Vol 609 ◽  
pp. 151-161 ◽  
Author(s):  
CO Bennice ◽  
AP Rayburn ◽  
WR Brooks ◽  
RT Hanlon

Oikos ◽  
1984 ◽  
Vol 42 (3) ◽  
pp. 267 ◽  
Author(s):  
Matti Nummelin ◽  
Kari Vepsäläinen ◽  
John R. Spence ◽  
Kari Vepsalainen

2001 ◽  
Vol 65 (1) ◽  
pp. 99 ◽  
Author(s):  
Timothy M. Gabor ◽  
Eric C. Hellgren ◽  
Nova J. Silvy

1996 ◽  
Vol 36 (3) ◽  
pp. 509-520 ◽  
Author(s):  
TODD FRENCH ◽  
PATRICIA CHAMBERS

2004 ◽  
Vol 20 (4) ◽  
pp. 439-448 ◽  
Author(s):  
Graeme R. Gillespie ◽  
David Lockie ◽  
Michael P. Scroggie ◽  
Djoko T. Iskandar

The habitat associations of stream-breeding frogs were examined along a series of stream transects on Buton Island in south-east Sulawesi, Indonesia. Of the eight frog species located along streams, four were observed breeding in stream habitats. We examined spatial habitat partitioning among these species. Three of the four species were found to be associated with a non-random selection of the available perch sites. Strong partitioning between species in habitat associations was found; partitioning of the available habitat space was primarily associated with differences in proximity to stream features, and in the height of perch sites. General observations indicated that oviposition sites of most species were associated with the microhabitats in which the adult frogs were found. All four stream-breeding species appear to have synchronous breeding phenologies and the spatial relationships of these species within the habitat space appear to reflect partitioning of calling sites and oviposition sites. The stream-breeding frog community in this region of Sulawesi has much lower species richness and less specialized habitat use compared with other tropical stream-breeding frog communities in the region.


The Condor ◽  
2013 ◽  
Vol 115 (2) ◽  
pp. 394-402 ◽  
Author(s):  
Andrew J. Laughlin ◽  
Istvan Karsai ◽  
Fred J. Alsop

2017 ◽  
Vol 22 (2) ◽  
pp. 71
Author(s):  
Jacobus Vijverberg ◽  
Jan Heidweiller ◽  
Jan G. Sevenster ◽  
Koenraad Kortmulder

2021 ◽  
Vol 8 ◽  
Author(s):  
Jacquelyn N. Cresswell ◽  
Peter J. van Hengstum

Karst subterranean estuaries (KSEs) are created from the two- and three-way mixing of saline groundwater, rain, and oceanic water in the subsurface on carbonate landscapes, and this hydrographic framework promotes unique physical processes, biogeochemical cycling, and biological communities. Here we provide evidence that the source and quantity of particulate organic matter (POM) that is delivered to the benthos strongly correlates to benthic habitat partitioning in the oxygenated marine sectors of KSEs. A dataset of benthic foraminifera at 128 different locations from several large flooded cave systems in Bermuda were compiled and evaluated against common environmental characteristics (e.g., tidal exposure, substrate particle size, bulk organic matter, C:N, total organic carbon, and δ13Corg). Benthic areas receiving more carbon isotopically depleted organic matter sources (mean δ13Corg values < −23.2‰, C:N ratios >11), most likely from the terrestrial surface and some marine plankton, were dominated by Trochammina inflata, Bolivina spp., and Helenina anderseni. In contrast, benthic areas receiving more carbon isotopically enriched organic matter sources (mean δ13Corg values > −21.6‰, C:N ratios <10), most likely from marine plankton transported through marine cave openings cave from adjacent coastal waters, were dominated by Spirophthalmidium emaciatum, Spirillina vivipara, Patellina corrugata, and Rotaliella arctica. The benthic foraminifera most distal from any cave entrances were dominated by taxa also known from the deep-sea (e.g., Rotaliella, Spirophthalmidium) in sediment with the lowest bulk organic matter content (mean: 6%), or taxa that prefer hard substrates and are potentially living attached to cave walls (Patellina, Spirillina). While physical groundwater characteristics (e.g., salinity, dissolved oxygen) are expected drivers of benthic ecosystems in KSEs, these results suggest that POM source, quantity, and delivery mechanisms (e.g., groundwater-seawater circulation mechanisms, terrestrial flux) play an important role in benthic habitat partitioning and the spatial variability of biogeochemical cycles in the oxygenated marine sector of KSEs.


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