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1 discovered fresco from Isidoro Bianchi (XVII century).
2 us group relocated to Siberia in seventeenth century.
3 r breeding phenology by 5-12 d over the last century.
4 ly emerged in Central Europe in the mid-19th century.
5 aker (non-stationary) in the early twentieth century.
6 t decreases in tree regeneration in the 21st century.
7 unattainable by some at the turn of the 21st century.
8 rojected to expand by 23% by the end of this century.
9 rough waterfalls and dolines for more than a century.
10 s of its body size in slightly more than one century.
11 sses the trends and strategies over the past century.
12 lan for ocular health care needs in the 21st century.
13 methods for their synthesis for more than a century.
14 heat spells causing dieback in the late 20th century.
15 tic and population pressures over the 21(st) century.
16 h Canadians who colonized Quebec in the 17th century.
17 ve been used as physical evidence for over a century.
18 d as one of the great challenges of the 21st century.
19 modate projected temperature change for this century.
20 lecting no improvement through the past half-century.
21 f the most common white pigments of the 20th century.
22 reted natural products date back well over a century.
23 action of transportation energy needs by mid-century.
24 ns could lessen damages by $1.3 billion this century.
25 in CA precipitation through the twenty-first century.
26 nscaled climate simulations for the mid-21st century.
27 forced to leave the Sahel by the end of this century.
28 , with an average increase of 2.8% by end of century.
29 ble to collapse, as melt rates increase this century.
30 increases in glacial melt over the past half century.
31 he golden age of antibiotics of the mid-20th century.
32 ns from wood products built up over the last century.
33 h enhancement by one-third by the end of the century.
34 h applied pressure has been known for over a century.
35 ive effects of greater heat and drought this century.
36 owel disease is a global disease in the 21st century.
37 turning point in the middle of twenty-first Century.
38 O3-depleting substance emitted in this 21st century.
39 river flow reconstruction for the twentieth century.
40 nts performed by Luigi Galvani in the 18(th) century.
41 recovery) have increased over the twentieth century.
42 able evidence accumulated over the past half century.
43 and has experienced SOC change over the past century.
44 introductions across Europe since the 19(th)-century.
45 carbon cycle to global change over the next century.
46 n the southeastern United States during this century.
47 inty in relative change in NPP over the past century.
48 ng is projected to intensify over the coming century.
49 na woody vegetation change spanning the last century.
50 1,3-diyne linkage has been known for over a century.
51 e 6%, a sixfold increase since the late 20th century.
52 ttle Ice Age until the beginning of the 19th Century.
53 s, to multiple tsunamis within the span of a century.
54 t to shifts in climate over the rest of this century.
55 e expanded substantially in the twenty-first century.
56 w) at the sub-basin scale over the past half-century.
57 tive greenhouse gas forcing through the 21st century.
58 n peaked during the first decade of the 20th century.
59 ogate to study human biology for more than a century.
60 of Arctic Ocean bottom water during the last century.
61 eturn to levels observed pre-1980 later this century.
62 ape that survived intact until the late 20th century.
63 porally realistic projections for the coming century.
64 ecast changes in tree growth during the 21st century.
65 re droughts are expected in the twenty-first century.
66 multidecadal variability extending back six centuries.
67 ds will exceed prethaw stocks in a matter of centuries.
68 of the fact that it will likely persist for centuries.
69 hese man-made ecosystems after less than two centuries.
70 captivated the imagination of biologists for centuries.
71 0 degrees to 750 degrees C for only years to centuries.
72 onmental and climate records spanning recent centuries.
73 rption has been extensively investigated for centuries.
74 hannels have been changing over the past few centuries.
75 d CO2 , but only over the course of multiple centuries.
76 n subalpine forest communities in the coming centuries.
77 ents of many leading violinists for over two centuries.
79 century AD, which persisted until the 8(th) century [1]; the renowned Black Death of the 14(th) cent
80 [1]; the renowned Black Death of the 14(th) century [2, 3], with recurrent outbreaks until the 18(th
81 ], with recurrent outbreaks until the 18(th) century [4]; and the most recent 19(th) century pandemic
84 demics: the Plague of Justinian in the 6(th) century AD, which persisted until the 8(th) century [1];
85 they were generally established in the 20th century after most of the agricultural expansion had occ
90 commercial introduction three-quarters of a century ago, fluid catalytic cracking has been one of th
92 overy of the crown ethers by Pedersen half a century ago, the chemistry of wholly synthetic macrocycl
95 ve evolved from 'snail picking' campaigns, a century ago, to modern wide-scale human treatment campai
99 es of human olfaction but from a famous 19th-century anatomist's hypothesis that the evolution of hum
100 ire, yet it has formed during the past seven centuries and represents the greatest accumulation rates
101 -understory plant species over the last half-century and compare these shifts to changes in climate.
102 about 5,000 km(2) of wetlands over the past century and concern exists whether remaining wetlands wi
103 exported to North America in the early 20th century and progressively acquired the USA300 characteri
104 ncrease of women in the news during the 20th century and the change of geographic focus for various c
105 58% in contemporary conditions to 86% by mid-century and to 91% of lakes by late century, based on me
106 e of structural biology for more than half a century and will continue to remain so, a major limitati
107 al simplicity, has been studied for nearly a century and yet an unequivocal structural description of
108 problem") has been pondered by thinkers for centuries, and is regarded as among the deepest unsolved
109 ity to the watershed scale could persist for centuries, and why the disruption of this self-organizin
110 oil bacteria has been appreciated for over a century, and advances in chemical analysis and genome se
111 terminous United States (U.S.) over the past century, and report trends in spring and fall frost timi
112 e temperature values over the late twentieth century are accompanied by higher levels of interannual
113 However, the scientific methods of this 21st century are changing with the increased power and speed
114 stant, asylum applications by the end of the century are predicted to increase, on average, by 28% (9
117 sing CH4 emissions until the end of the 21st century as indicated by an atmospheric CH4 and CO2 conce
119 d suggests that TOC dynamics during the 20th century at these sites were primarily driven by changes
122 probably during the civil wars of the first century BC, and its peaking in extent during the relativ
123 y declining field during the sixth to second centuries BCE, the new record provides further support f
126 rming over the remainder of the twenty-first century but modelled estimates of warming vary by a fact
127 less frequently since the start of the 21st century, but civil insecurity outside the contexts of of
128 cell cues have been determined over the past century, but in the past decade, our molecular understan
132 pen landscapes, that had been maintained for centuries by traditional practices, markedly reduced whi
133 ccur with increasing frequency in the coming century - can stress and ultimately kill native coldwate
134 to a time transect spanning the 7(th)-11(th) centuries CE) yielded sufficient autosomal genome covera
138 Here we quantify the impact of twenty-first century climate change on ice-free areas under two Inter
139 animals at CO2 levels that far exceed end-of-century climate change projections (sometimes >10 000 mu
140 timing changes in response to projected 21st century climate change, and how the temporal resolution
145 ances in cardiac surgery toward the mid-20th century created a need for an artificial means of stimul
146 tment of the Cancer Moonshot within the 21st Century Cures Act in the USA arrived at a propitious mom
147 dances of these species had projected end-of-century declines in scleractinian calcification of >50%
148 to test for significant short-duration (1-2 centuries) demographic events known from one documented
149 ra and Baja California during the early 21st century, driven by the same environmental circumstances
150 have significantly altered over the last two centuries due to historical land-use and climate change.
151 ckground levels at the beginning of the 19th century due to emissions from gold/silver mining and Hg
153 ave changed significantly across decades and centuries during glacial-interglacial cycles, likely cau
154 el rise events over timescales of decades to centuries during the last deglaciation, previously recog
156 ered by Alexis Carrel and others in the 20th century, eventually provided a reliably effective treatm
158 g projection for the end of the twenty-first century for the steepest radiative forcing scenario is a
159 mental abundance was first noted in the past century from observations of planets in our own Solar Sy
160 he binders of a historical fresco of the XVI century from the Flemish painter Paul Brill and of a rec
161 ree with monitoring data, and maximum 20(th) century GEM levels of 3.9 +/- 0.5 ng m(-3) were 15 +/- 4
163 this behaviour to earthquake occurrence over centuries, given numerous potentially active faults, rem
164 ull climate model, with a 3 degrees C end-of-century global-average warming yielding regional increas
165 from 1.3 to 2 mmy(-1) Here we present a 20th-century GMSL reconstruction computed using an area-weigh
166 ases previously associated with the mid-19th century Gold Rush now coincide with early-20th century i
169 s driven neuroscientific enquiry in the last century has been the nature of differences in the prefro
170 f anthropogenic climate change over the last century has been the rise in global mean temperature.
171 hnological progress since the late twentieth century has centred on semiconductor devices, such as tr
175 nexus have primarily focused on mid- to end-century horizons and have not considered the full range
176 imatic conditions are projected for the 21st century; however, the role played by extreme climatic ev
180 heat-related mortality risks across the 21st century in New York City, and they highlight the importa
184 ntury Gold Rush now coincide with early-20th century industrial emissions, aligning the UFG record wi
187 o very slow fragmentation (projected to take centuries) into small particles through photo-, physical
188 pendent of the admixture, showing that a few centuries is sufficient to produce detectable genetic st
189 l mean sea level (GMSL) rose during the 20th century is uncertain, with little consensus between vari
192 s the Chichibabin reaction enters its second century, it is appropriate to re-examine the life of thi
193 ough the phenomenon is known for more than a century, it is not clear how cells perceive the external
194 to fall in the late half of the twenty-first century - largely due to reduced precipitation, enhanced
196 , changes to the resource base over the last century (likely due to the spread of invasive cheatgrass
198 of the vascular plants of the Americas has a centuries-long history, but it is only in recent decades
201 has been the subject of study for almost two centuries, many aspects of 2D chiral surface chemistry h
202 ry rates during the first decade of the 21st century mask a shift from firearm deaths towards a rapid
205 spective warming scenario, by the end of the century more than half of the area currently capable of
206 ating inflammation and infection in the 21st century: new hints from decoding resolution mediators an
207 ither current (pCO2 370 muatm) or end-of-the-century OA (pCO2 1,100 muatm) scenarios, crossed in an o
208 one of the most intense El Ninos of the past century, OCO-2 measurements of [Formula: see text] and f
209 )C, survived through cryptobiosis during six centuries of cold-based glacier burial in Antarctica, 2)
212 h-resolution flow network that simulates how centuries of seasonal nomadic herding could shape discre
213 ancestral vertebrate character, resolving a century of debate over whether the ancestral vertebrate
214 e surveyed enzymological data accrued from a century of experimentation and generated a genome-scale
218 es in ecological communities has motivated a century of research into the mechanisms that maintain bi
223 e environment as a consequence of about half century of use in different fields of applications.
224 show that the spatial patterns observable in centuries-old Balinese rice terraces are also created by
227 er et al. shed new light on Theodor Boveri's century-old hypothesis by demonstrating that aneuploidy
232 Full-length barcodes obtained from all three century-old Venezuelan syntypes of U. kikkawai show that
233 ause oPOM can reside in soils for decades to centuries, organic matter accumulating under future rate
235 2, a jellifying agent commonly added in 20th century paint tube formulations, proved decisive for the
236 (th) century [4]; and the most recent 19(th) century pandemic, in which Y. pestis spread worldwide [5
240 tures or relocate, fish acclimated to end-of-century predicted temperatures (i.e. 31 or 33 degrees C)
241 geographic distributions sampled in the 20th century prior to climate change with resurveys of distri
246 50 and a peak value near the end of the 20th century, reflecting interactions between anthropogenic a
252 ed to strengthen throughout the twenty-first century, suggesting that the Sahel will experience parti
253 Here we show that, over the twenty first century, temperate drylands may contract by a third, pri
254 ncholia in the late nineteenth and twentieth century textbooks closely resembled each other, both rep
257 estimate of GPP growth during the twentieth century that is based on long-term atmospheric carbonyl
263 CMIP5 simulations suggest that, during this century, the likelihood of autumn transatlantic migrants
264 in nematodes, rodents and humans for over a century, the mechanisms underlying the effects of probio
266 iomedical research has evolved over the past century, the terminology employed to categorize it has f
267 ve been extensively investigated in the last century, the traditional approaches employed in the past
268 e mechanisms have been known for more than a century, their cellular and molecular underpinnings are
269 tinues to rise further into the twenty-third century, then the associated large increase in radiative
270 success story of the first half of the 20th century, then the decline in mortality from coronary hea
272 ic functions of life, and over the past half-century, these natural micellar structures have inspired
275 on and selective breeding have been used for centuries to adapt plant and animal species for human us
276 tropical cyclones in New York City in coming centuries to increase greatly compared with preindustria
278 ten equation has been widely used for over a century to estimate the enzyme kinetic parameters from r
281 taking us, by the middle of the twenty-first century, to values of CO2 not seen since the early Eocen
285 oject ice-free conditions during summer this century under realistic emission scenarios, reflecting t
287 " of over ten billion people within the next century, unprecedented demands will be placed on food, e
288 ge period (LIA, here defined as c. 16th-18th centuries) via persistent, blocked atmospheric condition
290 In 1816, the coldest summer of the past two centuries was observed over northeastern North America a
291 limate, at least up to the start of the 21st century, was favorable for fishery productivity in the H
292 RCP8.5 projections for the end of the 21(st) century, we find that in the global, multi-model mean, p
295 asters dating from the 14th to the late 19th centuries were analyzed using synchrotron-based X-ray di
296 will be the most vulnerable in the late 21st century when climatic conditions will be analogous to th
297 approaches to the disease began in the 18th century when leading physicians, such as Rene Laennec an
298 to about 14 cm would be expected in the 21st century, with continuing contributions lasting more than
299 of these soil carbon stocks over the 20(th) century, with models either gaining or losing over 20 Pg
300 drofluorocarbon substitutes in the next half-century would also contribute to centuries of future TSL
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