{"refrec":{"BRefID":339209,"RR":"<b>de Smit, J.C.; Bin Mohd Noor, M.S.; Infantes, E.; Bouma, T.J.</b> (2022). Wind exposure and sediment type determine the resilience and response of seagrass meadows to climate change. <i>Limnol. Oceanogr. 67(S1)</i>: S121-S132. <a href=\"https://dx.doi.org/10.1002/lno.11865\" target=\"_blank\">https://dx.doi.org/10.1002/lno.11865</a>","BEntID":335844,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Limnol. Oceanogr. 67(S1)</i>: S121-S132. <a href=\"https://dx.doi.org/10.1002/lno.11865\" target=\"_blank\">https://dx.doi.org/10.1002/lno.11865</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":1,"TerrestrialFlag":0,"Authorstring":"de Smit, J.C.; Bin Mohd Noor, M.S.; Infantes, E.; Bouma, T.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"de Smit, J.C. <i>et al.</i>","Englishabstract":"<p>    Seagrasses and bare sediment represent alternative stable states, with    sediment resuspension being a key driver of system stability via the    Seagrass–Sediment–Light (SSL) feedback. We explore the SSL feedback by    quantifying the sediment stabilization by seagrass, and using these    measurements to calculate under which conditions seagrass ends up in a    turbid environment. We quantified in-situ sediment resuspension velocity    thresholds (<em>u</em><sub>cr</sub>) for <em>Zostera marina</em> growing inmedium to fine sand, using a field flume inducing near-bed wave motion.    <em>u</em><sub>cr</sub> was determined for full length shoots, shoots    clipped to 0.08 m, and removed shoots. We found that rhizomes did notinfluence <em>u</em><sub>cr</sub> of the top sediment layer. Overall,    <em>u</em><sub>cr</sub> was linearly related to blade area, which became    independent for sediment type when normalizing <em>u</em><sub>cr</sub> forthe resuspension threshold after shoot removal. Comparing measured    <em>u</em><sub>cr</sub> against natural wave conditions showed that the    seagrass meadow at the study site is currently stable. Exploring the    effects of changing hydrodynamic conditions revealed that effects of    increasing storminess has limited influence on sediment resuspension and    thus the SSL-feedback. Increasing mean wind velocity had a strongerinfluence on SSL-feedback dynamics by causing more frequent exceedance of    <em>u</em><sub>cr</sub>. The response of seagrasses to increasing wind    pressure depends on bay topography. A fully exposed <em>Z. marina</em>    meadow under low initial turbidity pressure trended toward bistability, as    turbidity pressure increased mainly on bare sediments. The study site and a    fully exposed <em>Z. marina</em> meadow under high initial turbidity    pressure saw an increase in turbidity across all blade areas.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Wind exposure and sediment type determine the resilience and response of seagrass meadows to climate change","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-18 01:32:23.849940","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-04-05","DateCreate":"2021-06-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000662204900001","VABBcode":null,"OpenAcc":1,"DOI":"10.1002/lno.11865"},"refs":null,"anarec":{"AnaID":339209,"PubliDate":2022,"Pagination":"S121-S132","XtraPublOfAnaID":null,"ISBN":null,"Volume":"67","Issue":"S1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43511,"SerRR":"Limnology and Oceanography. 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