Author:
Boon Paul I.,Bird Fiona L.,Bunn Stuart E.
Abstract
Biffarius arenosus had a mean δ13C of
–15·4 ± 0·2‰ and a mean
δ15N of 5·9 ± 0·1‰
(n = 38), and
Trypea australiensis had a mean
δ13C of –16·3 ± 0·3 and
a mean δ15N of 7·6 ± 0·1
(n = 20). The δ13C
signatures of the only mangrove species present
(Avicennia marina) and the most abundant saltmarsh plant
(Sarcocornia quinqueflora) indicated that they were not
major food sources. Seagrasses, predominantly
Heterozostera tasmanica, had mean
δ13C and δ15N values
of –11·7 ± 0·2‰ (n
= 65) and 3·9 ± 0·2‰
(n = 62), respectively. Seagrass epiphytes had
mean δ13C and δ15N
values of –17·9 ± 0·4‰ and 4·6
± 0·3‰ (n = 27),
respectively. A mixture of seagrasses and their epiphytes was the most likely
source of organic carbon for B. arenosus. Benthic
microalgae, such as diatoms, were a possible food source, but phospholipid
biomarkers indicated a meagre abundance of diatoms in the sediments, and
microscopy of shrimp guts revealed few or no diatom frustules. For
T. australiensis, food sources were less easily
distinguished than for B. arenosus, but they could
include seagrass epiphytes plus the green macroalgae
Enteromorpha spp. and/or the brown alga
Chordaria cladisiphon.
Subject
Ecology,Aquatic Science,Ecology, Evolution, Behavior and Systematics,Oceanography
Cited by
34 articles.
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