Abstract:Abstract. Organic matter (OM) exchanges between adjacent habitats affect the dynamics and functioning of coastal systems, as well as the role of the different primary producers as energy and nutrient sources in food webs. Elemental (C, N, C : N) and isotope (δ 13 C) signatures and fatty acid (FA) profiles were used to assess the influence of geomorphological setting in two climatic seasons on the export and fate of mangrove OM across a tidally influenced tropical area, Gazi Bay (Kenya). The main results indica… Show more
“…6A). The association of lagoons and tidal systems with riverine inputs can lead to a dominant contribution of allochthonous carbon to these systems (Signa et al, 2017;Watanabe & Kuwae, 2015), which may partly explain the higher OC stocks found in these environments (Fig 2B), and is coherent with the trend of more positive Δ 13 C values (more dominated by allochthonous C) found, particularly, in lagoons (Fig. 4B).…”
To understand global drivers of seagrass carbon stocks, we compiled data on species traits and stocks at multiple geomorphological settings. Globally, we identify large and long-lived seagrass species in lagoon environments as key in providing climate regulation services. The Mediterranean is a hotspot of seagrass carbon sequestration, given the distinct capacity of Posidonia oceanica to support large stocks.
“…6A). The association of lagoons and tidal systems with riverine inputs can lead to a dominant contribution of allochthonous carbon to these systems (Signa et al, 2017;Watanabe & Kuwae, 2015), which may partly explain the higher OC stocks found in these environments (Fig 2B), and is coherent with the trend of more positive Δ 13 C values (more dominated by allochthonous C) found, particularly, in lagoons (Fig. 4B).…”
To understand global drivers of seagrass carbon stocks, we compiled data on species traits and stocks at multiple geomorphological settings. Globally, we identify large and long-lived seagrass species in lagoon environments as key in providing climate regulation services. The Mediterranean is a hotspot of seagrass carbon sequestration, given the distinct capacity of Posidonia oceanica to support large stocks.
“…Two seasonal rivers -Kidogoweni to the northwest and Mkurumudji to the southwest of the bay drains into the Bay. This is in addition to seepage points (Signa et al 2017) that provide the Bay with freshwater input. According to Koppen climate classi cation, the climate of Gazi Bay may be classi ed as tropical wet/dry that is ideal for supporting mangrove growth.…”
Section: Methodsmentioning
confidence: 99%
“…This management block is located 3-5 km from Makongeni village (Fig. 1) and has no direct freshwater in uence (Signa et al 2017). The eastern block is largely managed by Kenya Forest Service (KFS), a state forest agency in charge of forests in Kenya, and there is minimal community involvement.…”
Participatory forestry has been recognized as a tool for improving tropical forest management. The current study assessed the impacts of participatory forest management (PFM) on the structure and regeneration of a mangrove forest at Gazi Bay, Kenya. Data were collected along belt transects
perpendicular to the waterline in both co-managed and state-managed mangrove forests. Basal area and standing density were significantly higher in the co-managed mangrove forests (16 m2/ha and 4 341 tree/ha) as compared to the state forests (eastern block 10.3 m2/ha and
2 673 trees/ha; western block 6.2 m2/ha and 2 436 trees/ha). There were significantly higher (p = 0.0068) densities of merchantable poles in community-managed as compared to state-managed forests. Natural regeneration patterns in community-managed and state-managed forests
were deemed adequate to support the recovery of both forests. The results demonstrate that community participation contributes to improved management of mangrove forests and is in agreement with the principles of sustainable forest management.
“…Identification of principal OM pathways of the food web was carried out using a qualitative approach. Differences in δ 13 C values have been shown to provide information on the contribution of sympagic vs. benthic and pelagic sources to the diet of Antarctic consumers (Calizza et al, 2018;Norkko et al, 2007), reliably reflecting differences in OM pathways between organisms (Careddu et al, 2015;Rossi et al, 2015;Signa et al, 2017b). Similarly, δ 15 N values are known to increase unequivocally across trophic levels, and therefore, provide a robust base to identify trophic position of consumers within food webs (Mancinelli et al, 2013;Post, 2002) The effect of the horizontal and vertical food web structure (i.e.…”
Section: Data Elaboration and Statisticsmentioning
Despite in the last decades a vast amount of literature has focused on trace element (TE) contamination in Antarctica, the assessment of the main pathways driving TE transfer to the biota is still an overlooked issue. This limits the ability to predict how variations in sea-ice dynamics and productivity due to climate change will affect TE allocation in food webs. Here, food web structure of Tethys Bay (Terra Nova Bay, Ross Sea, Antarctica) was first characterised using carbon and nitrogen stable isotopes (δ 13 C, δ 15 N) of organic matter sources (sediment and planktonic, benthic and sympagic primary producers) and consumers (zooplankton, benthic invertebrates and vertebrates). Then, relationships between TEs (Cd, Cr, Co, Cu, Hg, Ni, Pb and V) and stable isotopes were assessed in order to evaluate if and how horizontal (organic matter pathways) and vertical (trophic position) food web features influence TE transfer to the biota. Regressions between log[TE] and δ 13 C revealed that the sympagic pathway drives accumulation of V in primary consumers and of Cd and Hg in secondary consumers, and that a coupled benthic/planktonic pathway drives Pb transfer to all consumers. Regressions between log[TE] and δ 15 N showed that only Hg biomagnifies across trophic levels, while all the others TEs showed a biodilution pattern, consistent with patterns observed in temperate food webs. Although the Cd behavior needs further investigations, the present findings provide new insights about the role of basal sources in the transfer of TEs in polar systems, especially important nowadays in light of the forecasted trophic changes potentially resulting from future climate change-induced modification of sea-ice dynamics.Capsule : Depiction of trace element transfer in the Antarctic food web highlighted an important role of both sympagic and phytoplanktonic pathways, suggesting that forecasted modification of sea-ice dynamics due to climate change may alter contaminant accumulation and biomagnification patterns.
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