コーパス検索結果 (１語後でソート)
通し番号をクリックするとPubMedの該当ページを表示します
1 hic-level fisheries expand ("fishing through marine food webs").
2 interactions that structure the base of the marine food web.
3 potential large-scale impacts on the Arctic marine food web.
4 AA exposure for organisms at the base of the marine food web.
5 now, supporting the trophic transfer in the marine food web.
6 enguins and other organisms in the Antarctic marine food web.
7 buting to the bioaccumulation of MeHg in the marine food web.
8 ethylmercury prior to incorporation into the marine food web.
9 en global climate fluctuations and the polar marine food web.
10 ends and associated uncertainties across the marine food web.
11 f the potent neurotoxin methylmercury in the marine food web.
12 litate entry of T. gondii into the nearshore marine food web.
13 ynthesis, changing energy fluxes through the marine food web.
14 ic organisms and are major components of the marine food web.
15 an readily pass from the water column to the marine food web.
16 als, thus "fishing-down" this element of the marine food web.
17 esis fuels primary production at the base of marine food webs.
18 s in carbon fixation and energy flow through marine food webs.
19 eds to be accounted for to better comprehend marine food webs.
20 and mechanisms of their entry into Antarctic marine food webs.
21 been found in species spanning all levels of marine food webs.
22 lso recorded profound changes at the base of marine food webs.
23 dynamics, and thus biogeochemical cycles and marine food webs.
24 matic predators that play a key role in most marine food webs.
25 n and constitute a vital trophic link within marine food webs.
26 g uptake and trophic transfer at the base of marine food webs.
27 non-consumptive effects of top predators in marine food webs.
28 lankton dynamics, biogeochemical cycles, and marine food webs.
29 communities, with cascading consequences for marine food webs.
30 primary production and form the base of many marine food webs.
31 valence of undiscovered HOCs accumulating in marine food webs.
32 is important to understanding its entry into marine food webs.
33 l mercury and subsequently bioaccumulated in marine food webs.
34 thotrophy and organic matter assimilation in marine food webs.
35 obal biogeochemical cycles and production in marine food webs.
36 bioaccumulation and trophic transfer through marine food webs.
37 that biomagnify into upper trophic levels of marine food webs.
38 ffected by processes at the bottom of Arctic marine food webs.
39 ich marks the entry of mercury into northern marine food webs.
40 basis of some of the world's most productive marine food webs.
41 itat is a major entry point for mercury into marine food webs.
42 ter basic nutrient and carbon fluxes through marine food webs.
43 sight on how future climate change can alter marine food webs.
44 for microplastic transfer through Antarctic marine food webs.
45 spatial distribution of Hg in North Atlantic marine food webs.
46 e routes of carbon transfer from the base of marine food webs.
47 l predators, adding complexity and nuance to marine food webs.
48 tivities, with far-reaching consequences for marine food webs.
49 oplastics and microfibers, are ubiquitous in marine food webs.
51 polyfluoroalkyl substances (PFAS) enter the marine food web, accumulate in organisms, and potentiall
52 kton communities, which form the base of the marine food web and are a crucial element of the carbon
53 important as they form the foundation of the marine food web and are crucial in the carbon cycle.
55 biological uptake at the base of the Arctic marine food web and may explain the elevated MeHg concen
56 primary production and higher levels of the marine food web and they play an important role in media
57 a noteworthy route by which petroleum enters marine food webs and a previously overlooked biological
59 Here, we explore protistan trophic modes in marine food webs and broader biogeochemical influences.
60 arine environment by serving as the basis of marine food webs and by playing central roles in the bio
62 kton, also known as algae, form the basis of marine food webs and drive marine carbon sequestration.
65 nd heightened concern about their impacts on marine food webs and global fisheries, it has become inc
66 magnitude of phytoplankton blooms that fuel marine food webs and influence global biogeochemical cyc
67 n that accumulates in predominantly tropical marine food webs and leads to ciguatera fish poisoning.
69 y production exerts a fundamental control on marine food webs and the flux of carbon into the deep oc
70 a large influence on the future stability of marine food webs and the functioning of global biogeoche
71 minate human participation in pre-industrial marine food webs and the long-term role of fisheries in
72 ining when predators collapse ("fishing down marine food webs") and when low-trophic-level fisheries
73 nktonic organic matter forms the base of the marine food web, and its nutrient content (C:N:P(org)) g
74 PUAs) are bioactive on various levels of the marine food web, and yet the potential for these molecul
77 iability provides information on function of marine food webs, biogeochemical cycles and copepod heal
78 y have played key roles in the regulation of marine food webs, biogeochemical cycles, and Earth's cli
79 ocean pH, with potentially severe impacts on marine food webs, but empirical data documenting ocean p
80 insula allow us to assess how ice influences marine food webs by modulating solar inputs to the ocean
81 ries in the world but also play key roles in marine food webs by transferring energy from plankton to
84 ton primary production is at the base of the marine food web; changes in primary production have dire
85 uce PCB pollution, their biomagnification in marine food webs continues to cause severe impacts among
87 herring (Clupea pallasii), a cornerstone of marine food webs, generally spawn on marine macroalgae i
88 e world's oceans in recent decades, altering marine food webs, habitats and biogeochemical processes
90 he Cumberland Sound (Nunavut, Canada) arctic marine food web in the presence of transient species usi
91 an readily pass from the water column to the marine food web in three laboratory-constructed estuarin
93 consumers (heterotrophs) at the base of the marine food web is being increasingly replaced by the pa
95 at effect this has on arsenic cycling within marine food webs is essential to clarify the role of the
96 nitial magnitude of MMHg uptake into pelagic marine food webs is influenced by the degree of primary
98 osynthetic primary production at the base of marine food webs is often limited by the availability of
101 This effect, described as fishing down the marine food web, is observed when the trophic level of t
103 mple food chains, transfer to a more complex marine food web model in which cascades are induced by v
105 ator is potentially important to advances in marine food web modelling, fisheries science and the dyn
107 MHg) is a neurotoxicant that biomagnifies in marine food webs, reaching high concentrations in apex p
109 ally less newsworthy - they are the basis of marine food webs, supporting fisheries and charismatic m
110 salmon, which are short-lived, feed lower in marine food webs than other salmon species, and had the
112 s and siliceous phytoplankton at the base of marine food webs that in turn helped fuel diversificatio
113 , but despite their vital ecological role in marine food-webs, the impact of microplastics on zooplan
114 ers which determine biomass flows in coastal marine food web: the trophic transfer efficiency (TTE) a
115 changes in the isotopic baseline and compare marine food webs through time after an appropriate corre
116 pheric Hg loading have rapidly propagated up marine food webs to a commercially important species.
117 vironment, from ecotoxicity and new links in marine food webs to the fate of the plastics in the wate
118 , thereby, have far reaching consequences on marine food webs unless safeguards are in place to avoid
119 iants shape the structure and functioning of marine food webs via trophic top-down controls, landscap
121 rgy-flux models suggest that Middle Triassic marine food webs were able to support several large-bodi
123 ance, and thus biomass, near the base of the marine food web with potentially significant feedback ef
125 nsidered a valuable energy source for Arctic marine food webs, yet the extent remains unclear through