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1 ent for microbial community and arsenic (As) biogeochemistry.
2 cean linked to global impacts on climate and biogeochemistry.
3 and is thus of limited importance for ocean biogeochemistry.
4 ver-influenced water may influence estuarine biogeochemistry.
5 l to understanding OMZ functioning and ocean biogeochemistry.
6 key role microbes play in modulating Earth's biogeochemistry.
7 al for risk assessments of ocean ecology and biogeochemistry.
8 speciation, subsurface redox conditions, and biogeochemistry.
9 of dissolved organic S (DOS) in affecting S biogeochemistry.
10 e the role of animals in oxygen minimum zone biogeochemistry.
11 al structure and porewater samples for redox biogeochemistry.
12 ommunity structure, biotic interactions, and biogeochemistry.
13 oxygenation event gave rise to modern marine biogeochemistry.
14 ems, and microbes drive most of its relevant biogeochemistry.
15 st affected by simultaneous changes in ocean biogeochemistry.
16 h water bodies and may strongly affect their biogeochemistry.
17 understorey lichen flora and changes in soil biogeochemistry.
18 omplementing other metrics of plant nutrient biogeochemistry.
19 ts increasing our understanding of organic P biogeochemistry.
20 oils is of vital importance to environmental biogeochemistry.
21 profound consequences for marine ecology and biogeochemistry.
22 l fluxes that have a global impact on marine biogeochemistry.
23 eded additional attention to global nitrogen biogeochemistry.
24 g our understanding of the effects on global biogeochemistry.
25 ausing profound changes in planetary methane biogeochemistry.
26 crobe-host interactions, bioremediation, and biogeochemistry.
27 and therefore a central component of Earth's biogeochemistry.
28 to increase our understanding of marine DOM biogeochemistry.
29 ve substantial effects on soil processes and biogeochemistry.
30 ties, sediment characteristics, and sediment biogeochemistry.
31 ultimately regulate oceanic productivity and biogeochemistry.
32 ven these temporal changes in regional ocean biogeochemistry.
33 land-cover change on microbial roles in soil biogeochemistry.
34 and atmospheric conditions as well as ocean biogeochemistry.
35 s to phages with ramifications for ecosystem biogeochemistry.
36 e molecular targets used in hydrogen isotope biogeochemistry.
37 terior profoundly impacts global climate and biogeochemistry.
38 s and describe the impact of viruses on soil biogeochemistry.
39 versity, ecophysiology, trophic dynamics and biogeochemistry.
40 pathways and their relationships to in situ biogeochemistry.
41 nkton are fundamental to Earth's ecology and biogeochemistry.
42 ntitatively link microbial diversity to soil biogeochemistry.
43 ductivity are becoming a widely used tool in biogeochemistry.
44 rise due to changing hydrology and resulting biogeochemistry.
45 poorly understood effects on vegetation and biogeochemistry.
46 changes, and hence for ecosystems and ocean biogeochemistry.
47 ur, not just sulfate, is important to marine biogeochemistry.
48 hlights the importance of Rhizaria for ocean biogeochemistry.
49 nistic understanding of how fish alter ocean biogeochemistry.
50 iated arsenic redox changes in paddy arsenic biogeochemistry.
51 largely neglected in most models of Europan biogeochemistry.
52 acteria and archaea play key roles in global biogeochemistry.
53 t mycorrhizal types differ strongly in their biogeochemistry.
54 use DVMs have a crucial role in global ocean biogeochemistry.
55 portant consequences for understanding viral biogeochemistry.
56 predicting future changes in marine nitrogen biogeochemistry.
57 rimental and modeling studies of terrestrial biogeochemistry.
58 teractions play a key role in oceanic carbon biogeochemistry.
59 ing patterns in global soil biodiversity and biogeochemistry.
60 t step towards an understanding of meteorite biogeochemistry.
61 hic flow variability and its impact on ocean biogeochemistry.
62 ncing global ocean circulation, climate, and biogeochemistry.
63 symbionts and their role in ecosystem-level biogeochemistry.
64 , with implications for regional ecology and biogeochemistry.
65 s likely play an important role mediating Se biogeochemistry.
66 Land Model (CLM4.5) with vertically-resolved biogeochemistry.
67 anisms that may strongly influence hyporheic biogeochemistry.
68 tical uncertainty in understanding hyporheic biogeochemistry.
69 ronutrient, iron plays a key role in oceanic biogeochemistry.
70 subsurface microbiota on carbon cycling and biogeochemistry.
71 tions for ecosystem services, processes, and biogeochemistry.
72 mework for linking ocean thermodynamics with biogeochemistry.
73 ture, but also impact hydrology, ecology and biogeochemistry.
74 widely theorized to affect ocean-basin scale biogeochemistry(1-3), but has never been examined compre
75 elps to regulate biodiversity(1,2), nutrient biogeochemistry(3), greenhouse gas emissions(4), and the
76 (,)(10) ecology,(2)(,)(11) oceanography, and biogeochemistry.(4)(,)(12)(,)(13) However, the historica
78 nses, we observed consistent impacts on soil biogeochemistry aligned with belowground drivers of tree
80 Saanich Inlet-a seasonally anoxic fjord with biogeochemistry analogous to oxygen minimum zones (OMZs)
81 tudes because of cold temperature effects on biogeochemistry and (ii) the N/P ratio increases with me
82 e as systems biology, microbiology, ecology, biogeochemistry and analytical chemistry are enhancing o
83 faunal group because of their role in marine biogeochemistry and as a food source for commercial fish
85 sformed into novel ecosystems with habitats, biogeochemistry and biological communities outside the n
88 d South Pacific have direct implications for biogeochemistry and carbon export in oligotrophic gyres.
89 ential for dynamic changes in Southern Ocean biogeochemistry and circulation on human timescales.
94 lating with seasonal shifts in hydrology and biogeochemistry and clustering into three groups: winter
96 nual N(2) fixation and thus pelagic ecology, biogeochemistry and CO(2) sequestration, the projected i
97 Microbial communities consume oxygen, alter biogeochemistry and compress habitat in aquatic ecosyste
98 h provided unique insights into trench water biogeochemistry and contaminant cycling in a redox oscil
100 ssolved oxygen (DO) concentrations shape the biogeochemistry and ecological structure of aquatic ecos
101 ur results highlight the key roles of sulfur biogeochemistry and ecology in influencing estuarine fis
102 n boreal ecosystems with distinct hydrology, biogeochemistry and ecology that influence their carbon
105 o forecast climate change effects on dryland biogeochemistry and ecosystem functions lag behind many
107 global numerical model of ocean circulation, biogeochemistry and ecosystems suggests that Crocosphaer
109 ion of a high-resolution regional model with biogeochemistry and forecasts from NOAA's Climate Foreca
110 ntal-scale consequences for soil and aquatic biogeochemistry and global-scale consequences for the pe
111 he atmosphere to the oceans, affecting ocean biogeochemistry and hence having feedback effects on cli
114 t ecosystem models describing hyporheic zone biogeochemistry and its influence over riverine ecosyste
116 cal link between contemporary aquatic carbon biogeochemistry and paleo-conditions in the watershed, a
119 face of oceans provides a link between ocean biogeochemistry and the atmospheric chemistry of the mar
120 lity of this mechanism to affect large-scale biogeochemistry and the pathways by which hydrothermal i
121 he surface ocean, their roles in ecology and biogeochemistry, and approaches that can be used to anal
122 e the relationship between sediment texture, biogeochemistry, and biological activity in the Columbia
123 ns at the intersection of marine ecology, Fe biogeochemistry, and both human and environmental health
125 and trophic structure, species composition, biogeochemistry, and climate, drawing on special feature
126 t includes forest dynamics, microbe-mediated biogeochemistry, and competition for nitrogen and phosph
127 methods (e.g., analyses of dental calculus, biogeochemistry, and dental microwear) have only been de
129 We examined a global ocean circulation, biogeochemistry, and ecosystem model that indicated a de
132 lankton communities and affect productivity, biogeochemistry, and the efficacy of the biological pump
133 iotic ones is important in resource geology, biogeochemistry, and the search for life in the universe
134 Marine viruses are critical drivers of ocean biogeochemistry, and their abundances vary spatiotempora
136 unities have a strong impact on the regional biogeochemistry as evidenced by the low partial pressure
137 DOM is also important for marine sulfur biogeochemistry as the largest water column reservoir of
138 r light on potential fungal roles in U and P biogeochemistry as well as the application of these mech
139 data provide the first insights into uranium biogeochemistry at high pH and have significant implicat
140 the potential to affect carbon and nutrient biogeochemistry at local and possibly regional scales.
141 on deposition fluxes and their effect on the biogeochemistry at the ocean surface should be constrain
142 l hypoxic environments is relevant to global biogeochemistry because coastal hypoxia is increasing wo
143 h sediments to investigate the links between biogeochemistry, burial, and microbial community assembl
144 rface processes such as soil erosion or lake biogeochemistry but are attributed mainly to PPP applica
145 rtant role in dissolved organic matter (DOM) biogeochemistry, but its relationship with the fluoresce
146 5)N are two important proxy measures of soil biogeochemistry, but they were rarely examined as to the
147 ale eddies may play a critical role in ocean biogeochemistry by increasing nutrient supply, primary p
148 acteria play an indispensable role in marine biogeochemistry by recycling dissolved organic matter.
149 OE and its impact on microbial evolution and biogeochemistry can be aided by characterizing the cycli
150 , and the corresponding shifts in the lake's biogeochemistry, carbon cycling and food web structure.
151 mulas, enhancing our understanding of marine biogeochemistry, chemodiversity, and ecological processe
152 ntially through their effects on belowground biogeochemistry--could either promote (i.e., for the 0.1
153 emistry, we apply ecological theory, aqueous biogeochemistry, DNA sequencing and ultra-high-resolutio
155 oorganisms are a major engine of terrestrial biogeochemistry, driving the turnover of soil organic ma
156 tation is understudied in modern and ancient biogeochemistry due to a lack of environmental biomarker
160 from wetlands, suggest new frontiers in CH4 biogeochemistry, examine relationships between methanoge
161 09,540 occurrences for 2,506 species), water biogeochemistry, flood duration, and elevation, with riv
162 microbial communities strongly influence the biogeochemistry, food webs, and climate of our planet.
163 est regrowth shapes community succession and biogeochemistry for decades, including in the Upper Grea
164 notably in physiology and medicine, isotope biogeochemistry, forensic science, and palaeoclimatology
165 obtained a lake-sediment record of fire and biogeochemistry from a subalpine forest in Colorado, USA
166 mass, even after controlling for climate and biogeochemistry, further demonstrating the importance of
168 Conceptual and empirical advances in soil biogeochemistry have challenged long-held assumptions ab
169 trial, and wetland) and response categories (biogeochemistry, hydrography, mobile biota, sedentary fa
171 ify their impacts on watershed hydrology and biogeochemistry, illustrating that ecosystem feedbacks t
173 nce of ocean thermodynamics, circulation and biogeochemistry in a global biochemistry and circulation
179 ts the breadth of conditions influencing the biogeochemistry in shallow CO2-rich hydrothermal systems
182 and better predict human impacts on nitrogen biogeochemistry in the changing ocean of the Anthropocen
183 and inorganic C (DOC and DIC, respectively) biogeochemistry in the Congo Basin, six lowland streams
184 nds for large pelagic fishes and the natural biogeochemistry in this region facilitates seawater MeHg
185 s study allows for a better constraint of Co biogeochemistry in various natural and engineered enviro
186 pears of great interest especially in marine biogeochemistry, in carbon capture and storage and in ma
187 apable of mediating key steps in sedimentary biogeochemistry, including anaerobic degradation of poly
188 face ocean per year and contribute to marine biogeochemistry, including the sequestration of carbon d
189 understanding of crop ecophysiology and soil biogeochemistry increases average yields for rice, wheat
191 By representing fine-scale atmosphere-ocean biogeochemistry interactions in our ESM, we pave the way
192 the core microbial processes governing river biogeochemistry is hindered by a lack of genome-resolved
196 nity dynamics and their relationship to lake biogeochemistry is therefore essential to understanding
198 s, critical to our understanding of seawater biogeochemistry, its long-timescale geologic history is
200 ing to be elucidated through a confluence of biogeochemistry, microbiology, ecology, molecular biolog
201 multidisciplinary collaborations, including biogeochemistry, microbiology, zoology, and plant scienc
202 s to peatland ecology, carbon sequestration, biogeochemistry, microbiome research, niche construction
203 Ocean General Circulation Model coupled to a biogeochemistry model for a 50% increase of atmospheric
204 narios using a high-resolution ocean-sea ice-biogeochemistry model with realistic ice-shelf geometry.
205 using seafloor POC flux from a coupled ocean-biogeochemistry model, NEMO-MEDUSA, to investigate globa
206 e this issue, we coupled soil erosion into a biogeochemistry model, running at 1 km(2) resolution acr
208 state of Mato Grosso, using a process-based biogeochemistry model, the Terrestrial Ecosystems Model
209 fossil fuel CO2 emissions and a terrestrial biogeochemistry model, we produce the first estimate of
211 m the surface ocean for food, but most ocean biogeochemistry models predict global decreases in expor
213 work for incorporating microbial activity in biogeochemistry models, which often base biomineralizati
216 ifferent methodologies and spatial scales of biogeochemistry, molecular microbiology, and modeling, a
217 tween climate, the upper ocean, and deep-sea biogeochemistry need to be considered in determining the
218 , on average, > 61% of the variation in soil biogeochemistry occurred within plots, and the effects o
219 idered to dominate the microbial ecology and biogeochemistry of AMZs, recent environmental genomics a
220 geographic extent, relative importance, and biogeochemistry of AOM in 15 North American peatlands sp
224 ted CO2 ] on primary productivity and on the biogeochemistry of carbon (C), N, and phosphorus (P) acr
226 fide precipitates, key phases in the natural biogeochemistry of cobalt and in relevant remediation an
229 affect community structure, metabolism, and biogeochemistry of cyanobacterial mats remains unclear.
231 tant consequences for the thermodynamics and biogeochemistry of ecosystems, both during the winter-to
232 Advancements in understanding the phosphorus biogeochemistry of evolving aquatic environments offer a
233 be increasing and consequently impacting the biogeochemistry of glacial and proglacial ecosystems in
242 impact of increased nutrient loading on the biogeochemistry of mercury (Hg) is challenging to predic
253 Microorganisms play an important role in the biogeochemistry of the ocean surface layer, but spatial
254 e representation of key linkages between the biogeochemistry of the ocean, marine aerosol formation a
255 interactions influence the productivity and biogeochemistry of the ocean, yet they occur in miniscul
256 nisms playing major roles in the ecology and biogeochemistry of the oceans, including performing much
257 study demonstrates how dynamically sediment biogeochemistry of the Peru Margin has responded to glac
262 efine the physical extent, heterogeneity and biogeochemistry of these NRZs, we investigated sediment
264 Presently, little is known about the marine biogeochemistry of Ti and there is a distinct lack of oc
266 ay have a significant impact on the nitrogen biogeochemistry on Caribbean coral reefs by releasing la
268 Evaluation of lacustrine floc Fe, Pb, and Cd biogeochemistry over seasonal (summer, winter) and water
269 ortant role of hydrothermal vents on surface biogeochemistry, potentially fueling local hotspot sinks
270 in serpentinizing fluids and suggest sulfur biogeochemistry provides a key link between terrestrial
271 ng of the nature of high temperature methane biogeochemistry, providing insight into the physiology a
272 arch Community Earth System Model, version 1-Biogeochemistry, Representative Concentration Pathway 8.
273 se protists play a significant role in ocean biogeochemistry, representing an untapped source of know
274 terrestrial contribution to atmosphere-ocean biogeochemistry separated from coeval volcanic fluxes.
275 ed here into a next-generation model of soil biogeochemistry suggests that these differences in physi
276 m atmosphere) ESM simulation including ocean biogeochemistry that is able to resolve TCs, and the cas
277 er moisture availability and a changing soil biogeochemistry that may have impaired a stomatal respon
278 model, a high-resolution regional model with biogeochemistry that simulates seasonal conditions in hi
279 here and shapes tropospheric composition and biogeochemistry through its effects on ozone, other oxid
280 nd exerts a strong influence on water-column biogeochemistry through seafloor geometry and bottom-int
281 ormation about dynamic iron and radionuclide biogeochemistry throughout realistic sediment redox cycl
282 terrestrial ecosystems significantly affects biogeochemistry throughout weathering profiles, the lowe
283 cy, we used recent developments in coccolith biogeochemistry to reconstruct equatorial Atlantic sea s
284 oposed method thus opens new perspectives in biogeochemistry to study interactions between HSs and N
286 n microbiomes; however, the implications for biogeochemistry under environmental change will depend o
288 millions of years with pronounced impacts on biogeochemistry, vegetation, ecological communities and
289 , we predict microbial impacts on subsurface biogeochemistry via iron, sulfur, and complex carbon oxi
290 face water mixing, microbial communities and biogeochemistry, we apply ecological theory, aqueous bio
291 Overall, seawater microbial composition and biogeochemistry were influenced by reef location and hyd
292 rols of seawater CO2-carbonate chemistry and biogeochemistry, which is essential to make accurate pre
293 obal coupled models of ocean circulation and biogeochemistry, which lack this regulatory mechanism an
294 ly is consistently shaped by hydrography and biogeochemistry, while active segments of the community
295 imately arises from gradients of climate and biogeochemistry with implications for the geography of p
296 his phenomenon as a biotic component of lead biogeochemistry, with additional consequences for microb
297 oplankton is one of the foundations of ocean biogeochemistry, with applications in algal physiology,
298 are critically important to soil ecology and biogeochemistry yet are difficult to study due to soil's
299 s central to food production and the Earth's biogeochemistry, yet the molecular basis for its regulat
300 Reduced nitrogen (N) is central to global biogeochemistry, yet there are large uncertainties surro