Abstract:Salt marshes exist at the interface of the marine and the terrestrial system. Shore height differences and associated variations in inundation frequency result in altered abiotic conditions, plant communities, and resource input into the belowground system. These factors result in three unique zones, the upper salt marsh (USM), the lower salt marsh (LSM), and the pioneer zone (PZ). Marine detritus, such as micro‐ and macroalgae, is typically flushed into the PZ daily, with storm surges moving both salt marsh d… Show more
“…However, it declined from the USM to the LSM to the PZ, suggesting that the use of plant-associated resources decreases with decreasing shore height supporting our first hypothesis. These findings are in line with the decline in plant marker PLFAs in soil with decreasing shore height reported by Rinke et al (2022). However, plant biomarker NLFA concentrations in consumers also varied with season.…”
Section: Changes In Energy Channelling With Season and Salt Marsh Zon...supporting
confidence: 88%
“…Although being generally high across salt marsh zones and seasons, averaging 30.7 % of total marker NLFAs (excluding unspecific NLFAs), bacterial NLFA marker concentration of soil animals was highest in the PZ, implying that bacteria-associated resources increase with inundation frequency. This contrasts the results of Mueller et al (2020) suggesting that soil bacteria density declines at lower shore height, but is conform to earlier findings that generally bacteria dominate the decomposer system in salt marsh soils in particular in the PZ , Rinke et al 2022. Although being generally high, bacterial NLFA marker concentration in each zone varied with season indicating changes in bacterial prey with season.…”
Section: Changes In Energy Channelling With Season and Salt Marsh Zon...supporting
confidence: 81%
“…Contrasting the general pattern of increased channelling of bacterial resources with decreasing shore hight, the bacterial NLFA marker declined at lower elevations in Amischa sp. and Ochthebius sp., suggesting that the access of bacterial resources in these species declines with inundation frequency, which is consistent with changes in bacterial PLFAs across salt marsh zones (Rinke et al 2022). Presumably, these comparatively large species are more sensitive to removal of litter due to frequent inundations, which detrimentally affects their access to bacterial resources.…”
Section: Spatial Changes In Energy Channelling Through Salt Marsh Taxasupporting
confidence: 64%
“…It was highest in October and about 50% lower in April and July, suggesting maximum channelling of fungi to higher trophic levels in autumn. This contrasts low fungal marker PLFAs in soil of the USM and LSM in autumn as reported by Rinke et al (2022), but coincides with the peak of dead organic matter of salt marsh plants in autumn , likely boosting saprotrophic fungi . Therefore, increased channelling of fungi in autumn likely reflects the input of plant litter material with associated saprotrophic fungi contributing to the predominant use of autochthonous resources by the salt marsh food web.…”
Section: Changes In Energy Channelling With Season and Salt Marsh Zon...supporting
confidence: 47%
“…Contrasting the overall uniform use of fungal resources across salt marsh zones, fungal NLFA marker concentrations declined with decreasing shore height in Mesostigmata, whereas in Amischa sp., Staphylinidae larvae and Ochthebius sp. fungal NLFA marker increased in the LSM, matching soil fungal PLFA patterns (Rinke et al 2022).…”
Section: Spatial Changes In Energy Channelling Through Salt Marsh Taxamentioning
Salt marshes are located at the border between the marine and terrestrial system. Because they are formed as sediment accumulates, they comprise a gradient of shore height with differing inundation frequencies and associated abiotic soil conditions. Along this gradient both autochthonous vascular plant resources, as well as allochthonous marine algal or detrital resources are available, with the availability of both varying with season and salt marsh zone. However, little is known on the importance of either resource for the soil animal food web. We investigated both spatial and temporal resource use of the soil macro-and mesofauna of the salt marsh using neutral lipid fatty acids (NLFAs). Generally, irrespective of season and zone the soil animal food web predominantly relied on carbon originating from autochthonous vascular plants and associated bacteria and fungi. Although being only minor, allochthonous resources of marine origin contributed to soil food web nutrition across salt marsh zones and seasons. The contribution of algae to soil food web nutrition depended on inundation frequency and season, i.e. algal productivity. Overall, the results demonstrate that the salt marsh soil fauna in large relies on autochthonous resources originating from vascular plants, with the contribution of allochthonous marine resources being only minor and restricted to few taxa.
“…However, it declined from the USM to the LSM to the PZ, suggesting that the use of plant-associated resources decreases with decreasing shore height supporting our first hypothesis. These findings are in line with the decline in plant marker PLFAs in soil with decreasing shore height reported by Rinke et al (2022). However, plant biomarker NLFA concentrations in consumers also varied with season.…”
Section: Changes In Energy Channelling With Season and Salt Marsh Zon...supporting
confidence: 88%
“…Although being generally high across salt marsh zones and seasons, averaging 30.7 % of total marker NLFAs (excluding unspecific NLFAs), bacterial NLFA marker concentration of soil animals was highest in the PZ, implying that bacteria-associated resources increase with inundation frequency. This contrasts the results of Mueller et al (2020) suggesting that soil bacteria density declines at lower shore height, but is conform to earlier findings that generally bacteria dominate the decomposer system in salt marsh soils in particular in the PZ , Rinke et al 2022. Although being generally high, bacterial NLFA marker concentration in each zone varied with season indicating changes in bacterial prey with season.…”
Section: Changes In Energy Channelling With Season and Salt Marsh Zon...supporting
confidence: 81%
“…Contrasting the general pattern of increased channelling of bacterial resources with decreasing shore hight, the bacterial NLFA marker declined at lower elevations in Amischa sp. and Ochthebius sp., suggesting that the access of bacterial resources in these species declines with inundation frequency, which is consistent with changes in bacterial PLFAs across salt marsh zones (Rinke et al 2022). Presumably, these comparatively large species are more sensitive to removal of litter due to frequent inundations, which detrimentally affects their access to bacterial resources.…”
Section: Spatial Changes In Energy Channelling Through Salt Marsh Taxasupporting
confidence: 64%
“…It was highest in October and about 50% lower in April and July, suggesting maximum channelling of fungi to higher trophic levels in autumn. This contrasts low fungal marker PLFAs in soil of the USM and LSM in autumn as reported by Rinke et al (2022), but coincides with the peak of dead organic matter of salt marsh plants in autumn , likely boosting saprotrophic fungi . Therefore, increased channelling of fungi in autumn likely reflects the input of plant litter material with associated saprotrophic fungi contributing to the predominant use of autochthonous resources by the salt marsh food web.…”
Section: Changes In Energy Channelling With Season and Salt Marsh Zon...supporting
confidence: 47%
“…Contrasting the overall uniform use of fungal resources across salt marsh zones, fungal NLFA marker concentrations declined with decreasing shore height in Mesostigmata, whereas in Amischa sp., Staphylinidae larvae and Ochthebius sp. fungal NLFA marker increased in the LSM, matching soil fungal PLFA patterns (Rinke et al 2022).…”
Section: Spatial Changes In Energy Channelling Through Salt Marsh Taxamentioning
Salt marshes are located at the border between the marine and terrestrial system. Because they are formed as sediment accumulates, they comprise a gradient of shore height with differing inundation frequencies and associated abiotic soil conditions. Along this gradient both autochthonous vascular plant resources, as well as allochthonous marine algal or detrital resources are available, with the availability of both varying with season and salt marsh zone. However, little is known on the importance of either resource for the soil animal food web. We investigated both spatial and temporal resource use of the soil macro-and mesofauna of the salt marsh using neutral lipid fatty acids (NLFAs). Generally, irrespective of season and zone the soil animal food web predominantly relied on carbon originating from autochthonous vascular plants and associated bacteria and fungi. Although being only minor, allochthonous resources of marine origin contributed to soil food web nutrition across salt marsh zones and seasons. The contribution of algae to soil food web nutrition depended on inundation frequency and season, i.e. algal productivity. Overall, the results demonstrate that the salt marsh soil fauna in large relies on autochthonous resources originating from vascular plants, with the contribution of allochthonous marine resources being only minor and restricted to few taxa.
Sulfur-oxidizing and sulfate-reducing bacteria in salt marsh sediments are major controllers of ecosystem-scale carbon cycling. Cross-site comparisons of S-cycling communities are difficult given the rampant uncultured microbial diversity in sediment, yet comparisons are essential for revealing biogeographic, phylogenetic and functionally significant variation. Here, we use deep shotgun metagenomic sequencing data to construct and compare metagenome-assembled genomes (MAGs) of sulfur-cycling bacteria from Massachusetts and Alabama salt marshes that contrast in seasonality and sediment organic matter content. Samples were collected from sediments under Sporobolus alterniflorus and Sporobolus pumilus in separate MA vegetation zones, and under Sporobolus alterniflorus and Juncus roemerianus co-rooted in AL marsh. We grouped metagenomic data by plant species and site and identified 38 MAGs that included pathways for dissimilatory sulfate reduction or sulfide oxidation. Phylogenetic analyses indicated that 30 of the 38 were affiliated with uncultivated lineages. Read-mapping to MAGs showed significant differentiation of AL and MA samples, differentiation of samples taken in S. alterniflorus and S. pumilus vegetation zones in MA, but no differentiation of samples taken under S. alterniflorus and J. roemerianus that were rooted together in AL marsh. Pangenomic analyses of eight ubiquitous MAGs also detected site- and vegetation- specific genomic features, including varied sulfur-cycling operons, carbon fixation pathways, fixed single nucleotide variants, and active diversity-generating retroelements. This genetic diversity, detected at multiple scales even within uncultured groups, suggests evolutionary relationships affected by distance and local environment, and demonstrates differential microbial capacities for sulfur and carbon cycling in salt marsh sediments.
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