{"refrec":{"BRefID":323294,"RR":"<b>Kerimoglu, O.; Große, F.; Kreus, M.; Lenhart, H.-J.; van Beusekom, J.E.E.</b> (2018). A model-based projection of historical state of a coastal ecosystem: relevance of phytoplankton stoichiometry. <i>Sci. Total Environ. 639</i>: 1311-1323. <a href=\"https://dx.doi.org/10.1016/j.scitotenv.2018.05.215\" target=\"_blank\">https://dx.doi.org/10.1016/j.scitotenv.2018.05.215</a>","BEntID":316766,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Sci. Total Environ. 639</i>: 1311-1323. <a href=\"https://dx.doi.org/10.1016/j.scitotenv.2018.05.215\" target=\"_blank\">https://dx.doi.org/10.1016/j.scitotenv.2018.05.215</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kerimoglu, O.; Große, F.; Kreus, M.; Lenhart, H.-J.; van Beusekom, J.E.E.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kerimoglu, O. <i>et al.</i>","Englishabstract":"We employed a coupled physical-biogeochemical modelling framework for the reconstruction of the historic (H), pre-industrial state of a coastal system, the German Bight (southeastern North Sea), and we investigated its differences with the recent, control (C) state of the system. According to our findings: i) average winter concentrations of dissolved inorganic nitrogen and phosphorus (DIN and DIP) concentrations at the surface are similar to 70-90% and similar to 50-70% lower in the H state than in the C state within the nearshore waters, and differences gradually diminish towards off-shore waters; ii) differences in average growing season chlorophyll a (Chl) concentrations at the surface between the two states are mostly less than 50%; iii) in the off-shore areas, Chl concentrations in the deeper layers are affected less than in the surface layers; iv) reductions in phytoplankton carbon (C) biomass under the H state are weaker than those in Chl, due to the generally lower Chl: C ratios; v) in some areas the differences in growth rates between the two states are negligible, due to the compensation by lower light limitation under the H state, which in turn explains the lower Chl: C ratios; vi) zooplankton biomass, and hence the grazing pressure on phytoplankton is lower under the H state. This trophic decoupling is caused by the low nutritional quality (i.e., low N:C and P:C) of phytoplankton. These results call for increased attention to the relevance of the acclimation capacity and stoichiometric flexibility of phytoplankton for the prediction of their response to environmental change.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"A model-based projection of historical state of a coastal ecosystem: relevance of phytoplankton stoichiometry","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-02 01:32:01.803574","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Eutrophication; Pristine conditions; Reconstruction; Adaptation;Acclimation","OtherDescriptors":null,"Notes":null,"AnaPub":2018,"MonPub":null,"DateUpdate":"2020-04-16","DateCreate":"2020-04-07","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000436806200127","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.scitotenv.2018.05.215"},"refs":null,"anarec":{"AnaID":323294,"PubliDate":2018,"Pagination":"1311-1323","XtraPublOfAnaID":null,"ISBN":null,"Volume":"639","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43780,"SerRR":"Science of the Total Environment. 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