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2 s in tidal range while reconstructing MIS 5e sea level histories, and we remark that it is possible t
6 s biogeochemical simulations, we show that a sea level fall in this interval caused enhanced pressure
8 a global estimate of microbial loads and air-sea exchanges over the tropical and subtropical oceans b
10 argument that the westward shift of the air-sea coupling region will cause an increase of ENSO frequ
12 on the surface wind stress modulates the air-sea transfer of momentum by providing a sink of mesoscal
16 variations in oceanic chlorophyll (CHL) and sea surface temperature (SST), which is then incorporate
21 paleothermometry of the ostracode Krithe and sea-ice planktic and benthic indicator species, we sugge
28 x, we processed brain sections from seal and sea lion pups for Nissl substance, cytochrome oxidase, a
29 icroscopic examination of fixed seawater and sea ice samples revealed chytrids parasitizing diatoms c
30 he distribution profile between seawater and sea-ice showed a compound-dependency for Arctic samples
33 ermediate depth water (AIW) temperatures and sea-ice cover spanning the last 1.5 million years (Ma)
35 Accurate pH measurements in polar waters and sea ice brines require pH indicator dyes characterized a
37 ern Ross Sea dominate increases in Antarctic sea ice and are outside the range simulated by climate m
38 rends in climate model simulations.Antarctic sea ice extent continues to increase, with autumn sea ic
39 s evident in recent years, whereas Antarctic sea-ice concentration exhibits a generally increasing tr
41 warm Atlantic Ocean water to melt all Arctic sea ice within a few years, a cold halocline limits upwa
44 The consequences of rapid changes in Arctic sea ice have the potential to affect migrations of a num
48 omena, including the evolution of the Arctic sea ice cover, the El Nio Southern Oscillation (ENSO), t
51 thy lowlanders, resting HR was determined at sea level (SL) and after 15-18 days of exposure to 3454
52 tion would be reduced to a greater extent at sea level compared to high altitude after maximal exerci
53 fornia sea lion spend most of their lives at sea, but each also spends time on land to breed and give
54 seven lowlanders, heart rate was measured at sea level and after 2 weeks at high altitude after indiv
56 oraging have focused on predator activity at-sea, with some birds and marine mammals demonstrating co
57 potentially affecting light availability at-sea, such as percentage of cloud cover, did not confound
62 ce extent continues to increase, with autumn sea ice advances in the western Ross Sea particularly an
63 no ad hoc parameterization of the background sea-surface temperature (SST) gradient and a mean easter
64 hypoxic conditions across the entire Baltic sea as revealed by multiple sedimentary records and supp
65 AIS is marine-terminating and grounded below sea level within the Aurora subglacial basin, indicating
67 ollowing moderate-intensity exercise at both sea level and high altitude are mediated via an alpha1 -
69 on of arsenic-bearing mineral oxides in both sea and river water inundations, with less arsenic relea
73 ernates between being primarily regulated by sea ice or glacial discharge from the surrounding ground
74 eal (Mirounga angustirostris) and California sea lion (Zalophus californianus) are members of a diver
75 th the northern elephant seal and California sea lion spend most of their lives at sea, but each also
76 of adult females in the Beaufort and Chukchi seas during two periods with different sea ice character
78 effects of OA on the skeleton of "classical" sea urchins (euechinoids), but the impact of etching on
81 Here we use extreme value theory to combine sea-level projections with wave, tide, and storm surge m
83 tes driven by glacio-eustatically controlled sea-level fall is required to produce the observed drops
84 dinium and its cnidarian hosts (e.g. corals, sea anemones) are the foundation of coral-reef ecosystem
97 tegrate the biogeography of coastal and deep-sea, pelagic and benthic environments, and show how land
98 e suitable ecotoxicological proxies for deep-sea species, dependent on adaptation to habitats with si
99 o environmental sequences obtained from deep-sea environments based on 16S rRNA gene similarity and B
101 e record displays major oscillations in deep-sea temperature and Antarctic ice volume in response to
103 Here we analyze a new high-resolution deep-sea oxygen isotope (delta(18)O) record from the South At
104 ecilosclerid sponges from asphalt-rich, deep-sea oil seeps at Campeche Knolls in the southern Gulf of
110 ately 1,900 times greater than the diffusive sea-air methane efflux (17.3 +/- 4.8 mumol m(-2)d(-1)).
112 greatest sea ice concentration and earliest sea ice advance, while males foraged longer in polynyas
113 water methane seeps and/or strongly elevated sea-air methane flux always increase the global atmosphe
115 ivity in riverine environments (for example, sea-level changes) and the properties of current drainag
116 melanism - a biological means used by extant sea turtle hatchlings to elevate metabolic and growth ra
119 , reflected by more prevalent easterly flow, sea ice loss does not lead to Northern European winter c
124 ed that the ice sheet contribution to future sea level rise could have been underestimated in the lat
125 h-resolution hindcast of hurricane-generated sea states and wave simulations are combined with novel
126 ence of complex interactions between glacial sea level changes, volcanic degassing and atmospheric CO
127 d carbonate weathering during glacioeustatic sea-level regression has been proposed to account for th
131 s, the leading mode of variability of global sea-ice concentration is positively correlated with the
135 ed longer in pack ice in years with greatest sea ice concentration and earliest sea ice advance, whil
137 t time that dugongs (Dugong dugon) and green sea turtles (Chelonia mydas) assist seagrass dispersal.
138 tropical seagrass seeds by dugongs and green sea turtles provides a large-scale mechanism that enhanc
140 tic-Subarctic, i.e. the northern hemisphere, sea ice now exhibits similar levels of seasonality to th
145 We discovered the first FXYD homologue in sea lamprey, a basal jawless vertebrate, which suggests
147 r study clarifies the range of mechanisms in sea ice/terrestrial productivity coupling, allowing the
148 on the degradation of the phytochemicals in sea buckthorn extract was investigated using chromatogra
149 imental results suggest that ions present in sea water, also called smart water, have a significant i
151 s >95% of this flux and is highly soluble in sea water, as indicated by a significant increase in dis
152 n temporarily obscure the long-term trend in sea level rise, in addition to modulating the impacts of
153 , we examine how inter-annual variability in sea ice concentration and advance affect the foraging be
160 vary the hygroscopic growth of the inorganic sea salt within a general circulation model and show tha
164 t bridging knowledge gaps regarding the land-sea transport of per- and polyfluoroalkyl substances (PF
165 emissions (29%) moderate the wintertime land-sea surface air temperature difference and further decre
167 ousands of square kilometers to areas of low sea surface temperatures (14.5 degrees C-17.5 degrees C)
168 Bay were coincident with periods of very low sea level, which were associated with increased soil sal
170 nd ice sheet mass loss ( approximately 1.4 m sea-level equivalent) during the last deglaciation, both
172 ponse to climate change can be in a marginal sea like the Mediterranean Sea compared to the global oc
173 Mediterranean Sea is a mid-latitude marginal sea, particularly responsive to climate change as report
176 ent time in Earth's history when global mean sea level was substantially higher than it is at present
178 t also accurately quantifying how meridional sea-surface temperature patterns will change (structural
179 nthozoan species, and show that in the model sea anemone Aiptasia pallida the TSR domain promotes col
180 bivalve host Abra segmentum through multiple sea-level fluctuations preserved in brackish Holocene de
181 an annually resolved reconstruction of NINO4 sea-surface temperature, located in the central equatori
182 ruction indicates that relatively warm Nino4 sea-surface temperature values over the late twentieth c
185 e performed a structure-function analysis of sea urchin Alx1 using a rescue assay and identified a no
188 Knowledge of the surface composition of sea spray aerosols (SSA) is critical for understanding a
192 ave can also initiate widespread fracture of sea ice and further increase the likelihood of subsequen
193 A search for vwf sequences in the genome of sea squirts, the closest invertebrate relatives of hagfi
194 se, in addition to modulating the impacts of sea level rise through natural periodic undulation in re
195 ts are typically based on simple measures of sea level that do not capture its inherent complexity, e
196 ts suggest a long duration for the period of sea-level rise (533 +/- 2 through 498 +/- 2 ka) encompas
199 s to both observational and proxy records of sea-ice variability, and show persistent patterns of co-
200 addition, this work provides a clear sign of sea level-driven glacial/interglacial oscillations in bi
201 interest because two carnivorous species of sea turtles-hawksbills, Eretmochelys imbricata, and logg
203 nexpected findings from the immune system of sea urchin larvae potentially provide insights into immu
204 le component might reflect co-variability of sea ice and tundra productivity due to a common forcing,
205 ing range revealed that an abrupt warming of sea-surface temperature in the 1990s coincided with stee
207 cation were compared with clicks detected on sea-surface towed hydrophone arrays in the presence of v
208 ce and predation rate of P. helianthoides on sea urchins will likely decrease with future warming.
209 Projected Arctic warming, with more open sea ice leads providing halogen sources that promote AMD
211 1) according to a structure similar to other sea anemone peptides belonging to structural group 9a.
212 t the instrumental record of central Pacific sea-surface temperatures is too short to detect potentia
213 tropical Atlantic and cold northeast Pacific sea surface temperatures (SSTs), as well as positive sea
215 encies might have their origin in periodical sea surface temperature anomalies in the Atlantic Ocean
217 xtensive phytoplankton blooms beneath ponded sea ice during summer, indicating that satellite-based A
218 ace temperatures (SSTs), as well as positive sea level pressure (SLP) anomalies over Hawaii and negat
219 e use island isolation following postglacial sea-level rise, ca. 2.5 ka, to characterize long-term ch
220 an land-bridge islands by rising postglacial sea levels to estimate rates of change in hemosporidian
221 bine modeled storm surges with probabilistic sea-level rise projections to assess future coastal inun
222 s provides insights into physical processes: sea-level rise is often assumed to follow air temperatur
224 erraces are interpreted to record punctuated sea-level rise events over timescales of decades to cent
225 hern Annular Mode, austral season, rainfall, sea surface salinity and sea surface temperature (SST).
226 -term time series of observed and reanalysis sea-ice concentrations data suggest the possibility of t
227 ing occurred significantly later as regional sea ice freeze-up timing became later in the Beaufort, C
228 ration timing as related to delayed regional sea ice freeze-up since the 1990s, using two independent
229 r of hatching success, more so than regional sea surface temperatures (breeding season or winter) and
230 ffects of tides, surges, waves, and relative sea-level rise (SLR), neglecting non-linear feedbacks be
231 eate accurate projections of future relative sea level rise upon which to base planning efforts.
232 esults suggest that with the higher relative sea level (RSL) estimated for the Bahamas during MIS 5e,
236 onnected and separated by falling and rising sea levels associated with the advance and retreat of Pl
237 to the impacts of climate change and rising sea levels, with evidence of global shifts in the distri
239 nown to be present in the region, and rising seas associated with global warming on long timescales a
241 nds suggest that snow deposition, scavenging sea-salt aerosol bound PFAS, plays a role as a significa
245 nd eastward and are characterized by a sharp sea surface temperature (SST) front on the poleward edge
246 f bacterial isolates acquired from a sponge, sea slug, and coral to examine the functional landscape
247 SST anomaly further develops due to the SST-sea level pressure-cloud-longwave radiation positive fee
248 nce of the ice-albedo feedback on summertime sea ice, we find that during some time interval of the s
249 ion of multiple forcings, such as tectonics, sea-level fall and long-term decline in greenhouse gas c
257 When a whale kept its upper jaw above the sea surface, many anchovies in the targeted shoal appear
258 d and natural gas became entrapped below the sea surface, but the quantity entrapped and the sequestr
259 bison first entered North America during the sea level lowstand accompanying marine isotope stage 6,
262 tudied the rate of oil biodegradation in the sea over many years, but with no consensus on results.
263 mass of petroleum fluids dissolved into the sea during ascent from the pared wellhead (1,505 m depth
265 attenuated total reflectance analysis of the sea buckthorn extract revealed a satisfactory thermostab
268 y in the primordial germ cells (PGCs) of the sea urchin embryo (Strongylocentrotus purpuratus) is qui
269 sis is constrained by the limitations of the sea-ice cover record, preliminary statistical analyses o
272 lls provide episodic fluxes of energy to the sea floor that are degraded by a species-rich benthic fa
274 om the pared wellhead (1,505 m depth) to the sea surface, thereby matching observed volatile organic
275 r the supply of DOM from groundwaters to the sea, and that the STE has the potential to act as a temp
278 mic costs but sufficiently connected through sea currents to seed the most exploited fisheries and en
279 ting a marine biosphere-climate link through sea ice melt and low altitude clouds that may have contr
280 ocal/sub-regional component is attributed to sea breeze (cold air advection from ice-covered ocean on
281 uld be impaired at high altitude compared to sea level, (2) endothelial function would be reduced to
283 ride exhibited a dominant coarse mode due to sea salt influence, with substantially diminished concen
284 , amplified warming in Arctic regions due to sea-ice loss and other processes, relative to global mea
285 timates of increased coastal flooding due to sea-level rise have not considered elevated water levels
287 hina, to test the robustness of mangroves to sea level changes in relation to their genetic diversity
288 cord of Labrador Sea productivity related to sea-ice variability in Labrador, Canada that extends wel
290 ey in Rome that was deposited in response to sea-level rise during Marine Isotopic Stage (MIS) 13.
291 to increase surface elevation in response to sea-level rise, for most services there has been no dire
292 ication highlight the non-linear response to sea-level variations, with the potential to amplify or m
294 he potential responses of coastal species to sea-level rise, especially for species that rely on coas
297 sitive to the emissions scenarios underlying sea-level projections, as most of the population decline
300 and a naturally occurring condition in wild sea lions and simultaneously advance general knowledge o
301 dal Oscillation (PDO) years, as well as with sea-level-rise and surface warming, caused primarily by
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