An assessment of hydrogen sulfide intrusion in the seagrass Halodule wrightii

Sebastian Rubiano-Rincon, P. Larkin
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Abstract

Hydrogen sulfide (H2S, “sulfide”) is a naturally occurring component of the marine sediment. Eutrophication of coastal waters, however, can lead to an excess of sulfide production that can prove toxic to seagrasses. We used stable sulfur isotope ratio (δ34S) measurements to assess sulfide intrusion in the seagrass Halodule wrightii, a semi-tropical species found throughout the Gulf of Mexico, Caribbean Sea, and both western and eastern Atlantic coasts. We found a gradient in δ34S values (−5.58 ± 0.54‰+13.58 ± 0.30‰) from roots to leaves, in accordance with prior observations and those from other species. The results may also represent the first values reported for H. wrightii rhizome tissue. The presence of sulfide-derived sulfur in varying proportions (15–55%) among leaf, rhizome, and root tissues suggests H. wrightii is able to assimilate sedimentary H2S into non-toxic forms that constitute a significant portion of the plant’s total sulfur content.
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海草中硫化氢入侵的评价
硫化氢(H2S,“硫化物”)是海洋沉积物中自然存在的成分。然而,沿海水域的富营养化可能导致硫化物过量产生,这可能对海草有毒。我们使用稳定的硫同位素比值(δ34S)测量来评估硫化物在海草Halodule wrightii中的入侵,Halodule wrightii是一种遍布墨西哥湾、加勒比海以及大西洋西部和东部海岸的亚热带物种。从根到叶的δ34S值呈−5.58±0.54‰+13.58±0.30‰的梯度,与前人和其他物种的观测结果一致。该结果也可能代表了第一次报道的赖特根组织值。叶片、根茎和根组织中不同比例(15-55%)硫化物衍生的硫的存在表明,wright能够将沉积的H2S吸收成无毒形式,构成植物总硫含量的很大一部分。
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