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Artículos de revistas sobre el tema "Southern high latitude marine ecosystems"

Autor: Grafiati

Publicado: 25 de mayo de 2024

Última modificación: 31 de julio de 2025

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1

Paterson, J. Terrill, Jay J. Rotella, Kevin R. Arrigo, and Robert A. Garrott. "Tight coupling of primary production and marine mammal reproduction in the Southern Ocean." Proceedings of the Royal Society B: Biological Sciences 282, no. 1806 (2015): 20143137. http://dx.doi.org/10.1098/rspb.2014.3137.

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Polynyas are areas of open water surrounded by sea ice and are important sources of primary production in high-latitude marine ecosystems. The magnitude of annual primary production in polynyas is controlled by the amount of exposure to solar radiation and sensitivity to changes in sea-ice extent. The degree of coupling between primary production and production by upper trophic-level consumers in these environments is not well understood, which prevents reliable predictions about population trajectories for species at higher trophic levels under potential future climate scenarios. In this stud

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2

Arfianti, T., and MJ Costello. "Global biogeography of marine amphipod crustaceans: latitude, regionalization, and beta diversity." Marine Ecology Progress Series 638 (March 19, 2020): 83–94. http://dx.doi.org/10.3354/meps13272.

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Studying the biogeography of amphipod crustaceans is of interest because they play an important role at lower trophic levels in ecosystems. Because they lack a planktonic larval stage, it has been hypothesized that marine benthic amphipod crustaceans may have short dispersal distances, high endemicity, and spatial turnover in species composition, and consequently high global species richness. In this study, we examined over 400000 distribution records of 4876 amphipod species, and identified 12 regions of endemicity. The number and percent of endemic species peaked at 30°-35°S and coincided wi

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3

Contreras, L., J. Pross, P. K. Bijl, et al. "Southern high-latitude terrestrial climate change during the Paleocene–Eocene derived from a marine pollen record (ODP Site 1172, East Tasman Plateau)." Climate of the Past Discussions 10, no. 1 (2014): 291–340. http://dx.doi.org/10.5194/cpd-10-291-2014.

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Abstract. Reconstructing the early Paleogene climate dynamics of terrestrial settings in the high southern latitudes is important to assess the role of high-latitude physical and biogeochemical processes in the global climate system. However, whereas a number of high-quality Paleogene climate records has become available for the marine realm of the high southern latitudes over the recent past, the long-term evolution of coeval terrestrial climates and ecosystems is yet poorly known. We here explore the climate and vegetation dynamics on Tasmania from the middle Paleocene to the early Eocene (6

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4

Contreras, L., J. Pross, P. K. Bijl, et al. "Southern high-latitude terrestrial climate change during the Palaeocene–Eocene derived from a marine pollen record (ODP Site 1172, East Tasman Plateau)." Climate of the Past 10, no. 4 (2014): 1401–20. http://dx.doi.org/10.5194/cp-10-1401-2014.

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Abstract. Reconstructing the early Palaeogene climate dynamics of terrestrial settings in the high southern latitudes is important to assess the role of high-latitude physical and biogeochemical processes in the global climate system. However, whereas a number of high-quality Palaeogene climate records has become available for the marine realm of the high southern latitudes over the recent past, the long-term evolution of coeval terrestrial climates and ecosystems is yet poorly known. We here explore the climate and vegetation dynamics on Tasmania from the middle Palaeocene to the early Eocene

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5

Song, Zhixuan. "Projected impacts of global warming scenarios on marine ecosystems: Insights from the CMIP6 model." Theoretical and Natural Science 37, no. 1 (2024): 1–21. http://dx.doi.org/10.54254/2753-8818/37/20240153.

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Rising oceanic temperatures and increased heat content have triggered a decline in marine biodiversity and the degradation of ecosystem services. This study employs the Coupled Model Intercomparison Project Phase 6 (CMIP6) to analyze variables within the Nutrient-Phytoplankton-Zooplankton-Detritus (NPZD) framework. Focusing on two contrasting Shared Socioeconomic Pathways (SSPs) - SSP1-2.6 (low-warming scenario) and SSP5-8.5 (high-warming scenario) - we assess future impacts of climate-related factors on marine ecosystems across major oceanic regions. Under the high-warming SSP5-8.5 scenario,

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6

Son, Min Ho, Chung Il Lee, Joo Myun Park, et al. "The Northward Habitat Expansion of the Korean Top Shell Turbo sazae (Gastropoda: Vetigastropoda: Turbinidae) in the Korean Peninsula: Effects of Increasing Water Temperature." Journal of Marine Science and Engineering 8, no. 10 (2020): 782. http://dx.doi.org/10.3390/jmse8100782.

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Recent global climate change often leads to poleward expansions of habitat range of marine organisms in response to increasing water temperature at high latitude. This study investigated latitudinal distribution patterns of Turbo sazae from 2009 to 2018 along the southern and eastern coasts of Korea to verify whether gradual increases in seawater temperature in the East Sea/Sea of Japan (hereafter East/Japan Sea) accelerate changes in the geographic distribution of T. sazae. Between 2009 and 2018, underwater SCUBA surveys were conducted at 19 subtidal rocky shore habitats from the southern and

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7

Beltran, Roxanne S., A. Marm Kilpatrick, Greg A. Breed, et al. "Seasonal resource pulses and the foraging depth of a Southern Ocean top predator." Proceedings of the Royal Society B: Biological Sciences 288, no. 1947 (2021): 20202817. http://dx.doi.org/10.1098/rspb.2020.2817.

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Seasonal resource pulses can have enormous impacts on species interactions. In marine ecosystems, air-breathing predators often drive their prey to deeper waters. However, it is unclear how ephemeral resource pulses such as near-surface phytoplankton blooms alter the vertical trade-off between predation avoidance and resource availability in consumers, and how these changes cascade to the diving behaviour of top predators. We integrated data on Weddell seal diving behaviour, diet stable isotopes, feeding success and mass gain to examine shifts in vertical foraging throughout ice break-out and

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8

Loeb, Valerie J., Eileen E. Hofmann, John M. Klinck, Osmund Holm-Hansen, and Warren B. White. "ENSO and variability of the Antarctic Peninsula pelagic marine ecosystem." Antarctic Science 21, no. 2 (2008): 135–48. http://dx.doi.org/10.1017/s0954102008001636.

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AbstractThe West Antarctic Peninsula region is an important source of Antarctic krill (Euphausia superba) in the Southern Ocean. From 1980–2004 abundance and concentration of phytoplankton and zooplankton, krill reproductive and recruitment success and seasonal sea ice extent here were significantly correlated with the atmospheric Southern Oscillation Index and exhibited three- to five-year frequencies characteristic of El Niño–Southern Oscillation (ENSO) variability. This linkage was associated with movements of the Southern Antarctic Circumpolar Current Front and Boundary, a changing influen

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9

Rodgers, K. B., J. Lin, and T. L. Frölicher. "Emergence of multiple ocean ecosystem drivers in a large ensemble suite with an Earth system model." Biogeosciences 12, no. 11 (2015): 3301–20. http://dx.doi.org/10.5194/bg-12-3301-2015.

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Abstract. Marine ecosystems are increasingly stressed by human-induced changes. Marine ecosystem drivers that contribute to stressing ecosystems – including warming, acidification, deoxygenation and perturbations to biological productivity – can co-occur in space and time, but detecting their trends is complicated by the presence of noise associated with natural variability in the climate system. Here we use large initial-condition ensemble simulations with an Earth system model under a historical/RCP8.5 (representative concentration pathway 8.5) scenario over 1950–2100 to consider emergence c

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10

Steneck, Robert S., Michael H. Graham, Bruce J. Bourque, et al. "Kelp forest ecosystems: biodiversity, stability, resilience and future." Environmental Conservation 29, no. 4 (2002): 436–59. http://dx.doi.org/10.1017/s0376892902000322.

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Kelp forests are phyletically diverse, structurally complex and highly productive components of coldwater rocky marine coastlines. This paper reviews the conditions in which kelp forests develop globally and where, why and at what rate they become deforested. The ecology and long archaeological history of kelp forests are examined through case studies from southern California, the Aleutian Islands and the western North Atlantic, well-studied locations that represent the widest possible range in kelp forest biodiversity. Global distribution of kelp forests is physiologically constrained by ligh

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11

Murray, Alison E., and Joseph J. Grzymski. "Diversity and genomics of Antarctic marine micro-organisms." Philosophical Transactions of the Royal Society B: Biological Sciences 362, no. 1488 (2007): 2259–71. http://dx.doi.org/10.1098/rstb.2006.1944.

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Marine bacterioplanktons are thought to play a vital role in Southern Ocean ecology and ecosystem function, as they do in other ocean systems. However, our understanding of phylogenetic diversity, genome-enabled capabilities and specific adaptations to this persistently cold environment is limited. Bacterioplankton community composition shifts significantly over the annual cycle as sea ice melts and phytoplankton bloom. Microbial diversity in sea ice is better known than that of the plankton, where culture collections do not appear to represent organisms detected with molecular surveys. Broad

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12

Dorschel, B., J. Gutt, D. Piepenburg, M. Schröder, and J. E. Arndt. "The influence of the geomorphological and sedimentological settings on the distribution of epibenthic assemblages on a flat topped hill on the over-deepened shelf of the western Weddell Sea (Southern Ocean)." Biogeosciences 11, no. 14 (2014): 3797–817. http://dx.doi.org/10.5194/bg-11-3797-2014.

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Abstract. Epibenthos communities play an important role in the marine ecosystems of the Weddell Sea. Information on the factors controlling their structure and distribution are, however, still rare. In particular, the interactions between environmental factors and biotic assemblages are not fully understood. Nachtigaller Hill, a newly discovered seabed structure on the over-deepened shelf of the northwest Weddell Sea (Southern Ocean), offers a unique site to study these interactions in a high-latitude Antarctic setting. Based on high-resolution bathymetry and georeferenced biological data, the

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13

Dorschel, B., J. Gutt, D. Piepenburg, M. Schröder, and J. E. Arndt. "The influence of the geo-morphological and sedimentological settings on the distribution of epibenthic assemblages on a flat topped hill on the over-deepened shelf of the Western Weddell Sea." Biogeosciences Discussions 11, no. 1 (2014): 1631–72. http://dx.doi.org/10.5194/bgd-11-1631-2014.

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Abstract. Epibenthos communities play an important role in the marine ecosystems of the Weddell Sea. Information on the factors controlling their structure and distribution are, however, still rare. Especially the interactions between environmental factors and biotic assemblages are not fully understood. Nachtigaller Hill, a newly discovered seabed structure on the over-deepened shelf of the Northwest Weddell Sea (Southern Ocean), offers a unique site to study these interactions in a high-latitude Antarctic setting. Based on high-resolution bathymetry, geo-referenced biological data, the effec

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14

Fagan, Adam J., Tatsuro Tanioka, Alyse A. Larkin, Jenna A. Lee, Nathan S. Garcia, and Adam C. Martiny. "Elemental stoichiometry of particulate organic matter across the Atlantic Ocean." Biogeosciences 21, no. 19 (2024): 4239–50. http://dx.doi.org/10.5194/bg-21-4239-2024.

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Abstract. Recent studies show that stoichiometric elemental ratios of marine ecosystems are not static at Redfield proportions but vary systematically between biomes. However, the wider Atlantic Ocean is undersampled for particulate organic matter (POM) elemental composition, especially when it comes to phosphorus (i.e., POP). Thus, it is uncertain how environmental variation in this region translates into shifts in the C:N:P ratio. To address this, we analyzed hydrography, genomics, and POM concentrations from 877 stations on the meridional transects AMT28 and C13.5, spanning the Atlantic Oce

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15

Crame, J. Alistair. "Evolution of taxonomic diversity gradients in the marine realm: evidence from the composition of Recent bivalve faunas." Paleobiology 26, no. 2 (2000): 188–214. http://dx.doi.org/10.1666/0094-8373(2000)026<0188:eotdgi>2.0.co;2.

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A major new inventory of living marine Bivalvia (Mollusca) is based on 29 regional faunas. These again pick out strong latitudinal and longitudinal gradients in taxonomic diversity, but there are indications that the patterns are not so regular as previously thought. There are signs of asymmetry between the Northern and Southern Hemisphere latitudinal gradients, with the former tending to be more regular than the latter. Northern gradients are also characterized by a marked inflection at approximately 30°N, and the three Australian provinces seem to form a distinct “hot-spot” in the Southern H

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16

Rodgers, K. B., J. Lin, and T. L. Frölicher. "Emergence of multiple ocean ecosystem drivers in a large ensemble suite with an earth system model." Biogeosciences Discussions 11, no. 12 (2014): 18189–227. http://dx.doi.org/10.5194/bgd-11-18189-2014.

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Abstract. Marine ecosystems are increasingly impacted by human-induced changes. Ocean ecosystem drivers – including warming, acidification, deoxygenation and perturbations to biological productivity – can co-occur in space and time, but detecting their trends is complicated by the presence of noise associated with natural variability in the climate system. Here we use Large Initial-Condition Ensemble Simulations with a comprehensive Earth System Model under a historical/RCP8.5 pathway over 1950–2100 to consider emergence characteristics for the four individual and combined drivers. Using a one

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17

Trathan, P. N., J. Forcada, and E. J. Murphy. "Environmental forcing and Southern Ocean marine predator populations: effects of climate change and variability." Philosophical Transactions of the Royal Society B: Biological Sciences 362, no. 1488 (2007): 2351–65. http://dx.doi.org/10.1098/rstb.2006.1953.

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The Southern Ocean is a major component within the global ocean and climate system and potentially the location where the most rapid climate change is most likely to happen, particularly in the high-latitude polar regions. In these regions, even small temperature changes can potentially lead to major environmental perturbations. Climate change is likely to be regional and may be expressed in various ways, including alterations to climate and weather patterns across a variety of time-scales that include changes to the long interdecadal background signals such as the development of the El Niño–S

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18

Le Grix, Natacha, Jakob Zscheischler, Keith B. Rodgers, Ryohei Yamaguchi, and Thomas L. Frölicher. "Hotspots and drivers of compound marine heatwaves and low net primary production extremes." Biogeosciences 19, no. 24 (2022): 5807–35. http://dx.doi.org/10.5194/bg-19-5807-2022.

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Abstract. Extreme events can severely impact marine organisms and ecosystems. Of particular concern are multivariate compound events, namely when conditions are simultaneously extreme for multiple ocean ecosystem stressors. In 2013–2015 for example, an extensive marine heatwave (MHW), known as the Blob, co-occurred locally with extremely low net primary productivity (NPPX) and negatively impacted marine life in the northeast Pacific. Yet, little is known about the characteristics and drivers of such multivariate compound MHW–NPPX events. Using five different satellite-derived net primary produ

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19

Song, Yangjinan, and Xianqing Lv. "Study of Phytoplankton Biomass and Environmental Drivers in and around the Ross Sea Marine Protected Area." Journal of Marine Science and Engineering 11, no. 4 (2023): 747. http://dx.doi.org/10.3390/jmse11040747.

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The Southern Ocean plays a vital role in the global climate system and the life cycle of high-latitude marine life. Phytoplankton is an important source of primary productivity in this ecosystem. Its future changes could affect Southern Ocean geochemistry, carbon export, and higher trophic organisms. To better protect Antarctica, three different marine protected areas (MPA) have been established in the Ross Sea region. Because time-continuous and regionally complete data are difficult to obtain in this region, we obtained data from ocean model outputs to understand the spatiotemporal variabili

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20

Mendoza-Segura, Clara, Emilio Fernández, and Pedro Beca-Carretero. "Predicted Changes in the Biogeographical Range of Gracilaria vermiculophylla under Present and Future Climate Scenarios." Journal of Marine Science and Engineering 11, no. 2 (2023): 367. http://dx.doi.org/10.3390/jmse11020367.

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Global change effects have favoured the introduction of new species in marine ecosystems in recent years. Gracilaria vermiculophylla, a red seaweed native from the north-eastern Pacific, has successfully colonised large regions in the Northern Hemisphere. In this research, we implemented species distribution models (SDMs) to (i) examine which were the most important environmental factors defining the presence of G. vermiculophylla at a global scale, and (ii) determine the potential current and future distribution of G. vermiculophylla based on two climate scenarios (representative concentratio

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21

Mays, Chris, Vivi Vajda, Tracy D. Frank, et al. "Refined Permian–Triassic floristic timeline reveals early collapse and delayed recovery of south polar terrestrial ecosystems." GSA Bulletin 132, no. 7-8 (2019): 1489–513. http://dx.doi.org/10.1130/b35355.1.

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Abstract The collapse of late Permian (Lopingian) Gondwanan floras, characterized by the extinction of glossopterid gymnosperms, heralded the end of one of the most enduring and extensive biomes in Earth’s history. The Sydney Basin, Australia, hosts a near-continuous, age-constrained succession of high southern paleolatitude (∼65–75°S) terrestrial strata spanning the end-Permian extinction (EPE) interval. Sedimentological, stable carbon isotopic, palynological, and macrofloral data were collected from two cored coal-exploration wells and correlated. Six palynostratigraphic zones, supported by

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22

Savenko, O., and A. Friedlaender. "New sightings of the Southern right whales in West Antarctic Peninsula waters." Ukrainian Antarctic Journal 20, no. 1(24) (2022): 104–12. http://dx.doi.org/10.33275/1727-7485.1.2022.693.

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Southern right whales (SRW) in the southwest Atlantic are recognized as slowly recovering after the massive population decline induced by harvesting. SRWs spend summer months in high-latitude feeding grounds and migrate to mid-latitude wintering grounds in autumn, where breeding occurs. Only a few sightings are known for the Antarctic waters as far south as 64° S. The West Antarctic Peninsula is a biologically productive area experiencing marine ecosystem transformations caused by climate changing at one of the fastest rates on Earth. The continental shelf of this region is important for krill

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23

Wang, S., D. Bailey, K. Lindsay, J. K. Moore, and M. Holland. "Impact of sea ice on the marine iron cycle and phytoplankton productivity." Biogeosciences 11, no. 17 (2014): 4713–31. http://dx.doi.org/10.5194/bg-11-4713-2014.

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Abstract. Iron is a key nutrient for phytoplankton growth in the surface ocean. At high latitudes, the iron cycle is closely related to the dynamics of sea ice. In recent decades, Arctic sea ice cover has been declining rapidly and Antarctic sea ice has exhibited large regional trends. A significant reduction of sea ice in both hemispheres is projected in future climate scenarios. In order to adequately study the effect of sea ice on the polar iron cycle, sea ice bearing iron was incorporated in the Community Earth System Model (CESM). Sea ice acts as a reservoir for iron during winter and rel

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Wang, S., D. Bailey, K. Lindsay, K. Moore, and M. Holland. "Impacts of sea ice on the marine iron cycle and phytoplankton productivity." Biogeosciences Discussions 11, no. 2 (2014): 2383–418. http://dx.doi.org/10.5194/bgd-11-2383-2014.

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Abstract. Iron is a key nutrient for phytoplankton growth in the surface ocean. At high latitudes, the iron cycle is closely related to sea ice. In recent decades, Arctic sea ice cover has been declining rapidly and Antarctic sea ice has exhibited large regional trends. A significant reduction of sea ice in both hemispheres is projected in future climate scenarios. To study impacts of sea ice on the iron cycle, iron sequestration in ice is incorporated to the Biogeochemical Elemental Cycling (BEC) model. Sea ice acts as a reservoir of iron during winter and releases iron to the surface ocean i

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25

Weller, Gunter. "Regional impacts of climate change in the Arctic and Antarctic." Annals of Glaciology 27 (1998): 543–52. http://dx.doi.org/10.3189/1998aog27-1-543-552.

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Regional assessments of impacts due to global climate change are a high priority in the international programs on global-change research. in the polar regions, climate models indicate an amplification of global greenhouse warming, but there are large differences between the results of various models, and uncertainties about the magnitude and timing of the expected changes. Also, the observed high-latitude climate trends over the past few decades are much more regional and patchy than predicted by the models. As a first step in assessing possible climate impacts, model results are compared with

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26

Brown, Kristy, Jacquomo Monk, Joel Williams, Andrew Carroll, David Harasti, and Neville Barrett. "Depth and benthic habitat influence shallow and mesophotic predatory fishes on a remote, high-latitude coral reef." PLOS ONE 17, no. 3 (2022): e0265067. http://dx.doi.org/10.1371/journal.pone.0265067.

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Predatory fishes on coral reefs continue to decline globally despite playing key roles in ecosystem functioning. Remote atolls and platform reefs provide potential refugia for predator populations, but quantitative information on their spatial distribution is required to establish accurate baselines for ongoing monitoring and conservation management. Current knowledge of predatory fish populations has been derived from targeted shallow diver-based surveys (<15 m). However, the spatial distribution and extent of predatory fishes on outer mesophotic shelf environments has remained under descr

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McBride, Margaret M., Padmini Dalpadado, Kenneth F. Drinkwater, et al. "Krill, climate, and contrasting future scenarios for Arctic and Antarctic fisheries." ICES Journal of Marine Science 71, no. 7 (2014): 1934–55. http://dx.doi.org/10.1093/icesjms/fsu002.

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Abstract Arctic and Antarctic marine systems have in common high latitudes, large seasonal changes in light levels, cold air and sea temperatures, and sea ice. In other ways, however, they are strikingly different, including their: age, extent, geological structure, ice stability, and foodweb structure. Both regions contain very rapidly warming areas and climate impacts have been reported, as have dramatic future projections. However, the combined effects of a changing climate on oceanographic processes and foodweb dynamics are likely to influence their future fisheries in very different ways.

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Malviya, Shruti, Eleonora Scalco, Stéphane Audic, et al. "Insights into global diatom distribution and diversity in the world’s ocean." Proceedings of the National Academy of Sciences 113, no. 11 (2016): E1516—E1525. http://dx.doi.org/10.1073/pnas.1509523113.

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Diatoms (Bacillariophyta) constitute one of the most diverse and ecologically important groups of phytoplankton. They are considered to be particularly important in nutrient-rich coastal ecosystems and at high latitudes, but considerably less so in the oligotrophic open ocean. The Tara Oceans circumnavigation collected samples from a wide range of oceanic regions using a standardized sampling procedure. Here, a total of ∼12 million diatom V9-18S ribosomal DNA (rDNA) ribotypes, derived from 293 size-fractionated plankton communities collected at 46 sampling sites across the global ocean euphoti

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Mora-Soto, Alejandra, Mauricio Palacios, Erasmo Macaya, et al. "A High-Resolution Global Map of Giant Kelp (Macrocystis pyrifera) Forests and Intertidal Green Algae (Ulvophyceae) with Sentinel-2 Imagery." Remote Sensing 12, no. 4 (2020): 694. http://dx.doi.org/10.3390/rs12040694.

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Giant kelp (Macrocystis pyrifera) is the most widely distributed kelp species on the planet, constituting one of the richest and most productive ecosystems on Earth, but detailed information on its distribution is entirely missing in some marine ecoregions, especially in the high latitudes of the Southern Hemisphere. Here, we present an algorithm based on a series of filter thresholds to detect giant kelp employing Sentinel-2 imagery. Given the overlap between the reflectances of giant kelp and intertidal green algae (Ulvophyceae), the latter are also detected on shallow rocky intertidal areas

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Mega, Aline, Teresa Rodrigues, Emília Salgueiro, Mária Padilha, Henning Kuhnert, and Antje H. L. Voelker. "The Early–Middle Pleistocene Transition in the Gulf of Cadiz (NE Atlantic) – an interplay between subtropical gyre and extremely cold surface waters." Climate of the Past 21, no. 5 (2025): 919–39. https://doi.org/10.5194/cp-21-919-2025.

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Abstract. Besides the shift in dominant orbital cyclicity depicted in paleoclimate proxy records, the Mid-Pleistocene Transition or Early–Middle Pleistocene Transition (EMPT) was linked to a change in the deep thermohaline circulation. Those changes contributed to more intense and longer-lasting glacial periods and cooler sea surface temperatures (SSTs) during glacials. Within the Atlantic Ocean, the Iberian Margin is considered a key location to study climatic variations influenced by both high- and low-latitude processes. In this study we focus on IODP Site U1387 on the southern Portuguese m

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Chevassus, Emmanuel, Kirsten N. Fossum, Darius Ceburnis, et al. "Marine organic aerosol at Mace Head: effects from phytoplankton and source region variability." Atmospheric Chemistry and Physics 25, no. 7 (2025): 4107–29. https://doi.org/10.5194/acp-25-4107-2025.

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Abstract. Organic aerosol (OA) is recognized as a significant component of particulate matter (PM), yet their specific composition and sources, especially over remote areas, remain elusive due to the overall scarcity of high-resolution online data. In this study, positive matrix factorization was performed on organic aerosol mass spectra obtained from high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) measurements to resolve sources contributing to coastal PM. The focus was on a summertime period marked by enhanced biological productivity with prevailing pristine maritime co

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Vedenin, Andrey A., Eteri I. Musaeva, Daria N. Zasko, and Alexander L. Vereshchaka. "Zooplankton communities in the Drake Passage through environmental boundaries: a snapshot of 2010, early spring." PeerJ 7 (November 7, 2019): e7994. http://dx.doi.org/10.7717/peerj.7994.

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Background Spatial distribution of zooplankton communities influenced by various environmental factors is always important for understanding pelagic ecosystems. The area of the Drake Passage (Southern Ocean) is of particular interest owing to the high spatial and temporal variability of hydrological parameters affecting marine fauna. This study provides a survey of zooplankton composition and spatial distribution along a transect in the Drake Passage sampled during the 31th Cruise of RV “Akademik Sergey Vavilov” in November, 2010. The main aim was to trace the main regularities in spatial zoop

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Saha, Korak, Prasanjit Dash, James Frech, Huai-Min Zhang, Paul DiGiacomo, and Steven D. Miller. "Trends in Satellite-Based Ocean Parameters through Integrated Time Series Decomposition and Spectral Analysis. Part II: NOAA/NCEI Blended Seawinds." Journal of Atmospheric and Oceanic Technology 42, no. 3 (2025): 281–94. https://doi.org/10.1175/jtech-d-24-0008.1.

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Abstract Seawind is essential in studying extreme weather and climate events globally over the oceans. It has significant impacts through air–sea interactions, upper ocean mixing, and energy flux generation. The sea surface wind is also a critical element in blue economy strategic planning, offshore renewable energy, marine transportation, marine ecosystem, and fisheries. As per the Intergovernmental Panel on Climate Change (IPCC) working group report, there is low confidence level in wind trends due to insufficient evidence. This study uses signal decomposition, namely, the multiple seasonal-

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Laufkötter, C., M. Vogt, N. Gruber, et al. "Drivers and uncertainties of future global marine primary production in marine ecosystem models." Biogeosciences 12, no. 23 (2015): 6955–84. http://dx.doi.org/10.5194/bg-12-6955-2015.

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Abstract. Past model studies have projected a global decrease in marine net primary production (NPP) over the 21st century, but these studies focused on the multi-model mean rather than on the large inter-model differences. Here, we analyze model-simulated changes in NPP for the 21st century under IPCC's high-emission scenario RCP8.5. We use a suite of nine coupled carbon–climate Earth system models with embedded marine ecosystem models and focus on the spread between the different models and the underlying reasons. Globally, NPP decreases in five out of the nine models over the course of the

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35

Laufkötter, C., M. Vogt, N. Gruber, et al. "Drivers and uncertainties of future global marine primary production in marine ecosystem models." Biogeosciences Discussions 12, no. 4 (2015): 3731–824. http://dx.doi.org/10.5194/bgd-12-3731-2015.

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Abstract. Past model studies have projected a global decrease in marine net primary production (NPP) over the 21st century, but these studies focused on the multi-model mean and mostly ignored the large inter-model differences. Here, we analyze model simulated changes of NPP for the 21st century under IPCC's high emission scenario RCP8.5 using a suite of nine coupled carbon–climate Earth System Models with embedded marine ecosystem models with a focus on the spread between the different models and the underlying reasons. Globally, five out of the nine models show a decrease in NPP over the cou

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36

Ver Straeten, Charles. "An introduction to the Devonian Period, and the Devonian in New York State and North America." Bulletins of American Paleontology, no. 403-404 (July 2023): 11–102. http://dx.doi.org/10.32857/bap.2023.403.03.

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The Devonian strata in New York State were the standard section for North America for over 100 years, and remain a significant reference for regional to global correlation and research. Since publication of L. V. Rickard’s (1975) New York Devonian correlation chart, various higher-resolution stratigraphic analyses have been employed, sometimes at bed-by-bed scale. These include sequence-, bio-, event-, chemo-, and other -stratigraphic approaches, along with increasingly finer-resolution geochronologic dating of airfall volcanic tephras. Results have led to many new interpretations and insights

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37

Huber, Brian T., Maria Rose Petrizzo, and Kenneth G. MacLeod. "Planktonic Foraminiferal Endemism at Southern High Latitudes Following the Terminal Cretaceous Extinction." Journal of Foraminiferal Research 50, no. 4 (2020): 382–402. http://dx.doi.org/10.2113/gsjfr.50.4.382.

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Abstract Austral planktonic foraminiferal assemblages from immediately above the Cretaceous/Paleogene (K/Pg) boundary at Ocean Drilling Program Hole 690C (Maud Rise, Weddell Sea) and International Ocean Drilling Program Hole U1514C (southeast Indian Ocean) show a much different record of post-extinction recovery than anywhere outside the circum-Antarctic region. Species of Woodringina and Parvularugoglobigerina, genera with well-documented evolutionary successions within the early Danian P0 and Pα biozones at tropical/subtropical and mid-latitude localities, are absent from southern high latit

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38

Mace, Gerald G., Sally Benson, Ruhi Humphries, Peter M. Gombert, and Elizabeth Sterner. "Natural marine cloud brightening in the Southern Ocean." Atmospheric Chemistry and Physics 23, no. 2 (2023): 1677–85. http://dx.doi.org/10.5194/acp-23-1677-2023.

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Abstract. The number of cloud droplets per unit volume (Nd) is a fundamentally important property of marine boundary layer (MBL) liquid clouds that, at constant liquid water path, exerts considerable controls on albedo. Past work has shown that regional Nd has a direct correlation to marine primary productivity (PP) because of the role of seasonally varying, biogenically derived precursor gases in modulating secondary aerosol properties. These linkages are thought to be observable over the high-latitude oceans, where strong seasonal variability in aerosol and meteorology covary in mostly prist

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39

Bednaršek, N., J. Možina, M. Vogt, C. O'Brien, and G. A. Tarling. "The global distribution of pteropods and their contribution to carbonate and carbon biomass in the modern ocean." Earth System Science Data 4, no. 1 (2012): 167–86. http://dx.doi.org/10.5194/essd-4-167-2012.

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Abstract. Pteropods are a group of holoplanktonic gastropods for which global biomass distribution patterns remain poorly described. The aim of this study was to collect and synthesise existing pteropod (Gymnosomata, Thecosomata and Pseudothecosomata) abundance and biomass data, in order to evaluate the global distribution of pteropod carbon biomass, with a particular emphasis on temporal and spatial patterns. We collected 25 939 data points from several online databases and 41 scientific articles. These data points corresponded to observations from 15 134 stations, where 93% of observations w

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40

Colombo, Stefanie M., Alexander Wacker, Christopher C. Parrish, Martin J. Kainz, and Michael T. Arts. "A fundamental dichotomy in long-chain polyunsaturated fatty acid abundance between and within marine and terrestrial ecosystems." Environmental Reviews 25, no. 2 (2017): 163–74. http://dx.doi.org/10.1139/er-2016-0062.

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Polyunsaturated fatty acids (PUFA), especially long-chain (i.e., ≥20 carbons) polyunsaturated fatty acids (LC-PUFA), are fundamental to the health and survival of marine and terrestrial organisms. Therefore, it is imperative that we gain a better understanding of their origin, abundance, and transfer between and within these ecosystems. We evaluated the natural variation in PUFA distribution and abundance that exists between and within these ecosystems by amassing and analyzing, using multivariate and analysis of variance (ANOVA) methods, >3000 fatty acid (FA) profiles from marine and terre

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41

Moline, Mark A., Nina J. Karnovsky, Zachary Brown, et al. "High Latitude Changes in Ice Dynamics and Their Impact on Polar Marine Ecosystems." Annals of the New York Academy of Sciences 1134, no. 1 (2008): 267–319. http://dx.doi.org/10.1196/annals.1439.010.

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42

Hunt, George L., Kenneth F. Drinkwater, Kevin Arrigo, et al. "Advection in polar and sub-polar environments: Impacts on high latitude marine ecosystems." Progress in Oceanography 149 (December 2016): 40–81. http://dx.doi.org/10.1016/j.pocean.2016.10.004.

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43

Carballeira, Rafael, and Xabier Pontevedra-Pombal. "Diatoms in Paleoenvironmental Studies of Peatlands." Quaternary 3, no. 2 (2020): 10. http://dx.doi.org/10.3390/quat3020010.

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The great diversity of diatoms in aquatic ecosystems and their close relationship with water chemistry make them one of the most informative and widely used biological proxies in paleoenvironmental studies of wetlands, except for peatland ecosystems. Currently, significant controversy still exists over the preservation of diatoms in peat. However, considerable evidence indicates that diatoms remain in good condition in minerotrophic peatlands, and they have been successfully used in paleoenvironmental studies in high-latitude regions and especially in Southern Europe.

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44

Whalen, Matthew A., Ross D. B. Whippo, John J. Stachowicz, et al. "Climate drives the geography of marine consumption by changing predator communities." Proceedings of the National Academy of Sciences 117, no. 45 (2020): 28160–66. http://dx.doi.org/10.1073/pnas.2005255117.

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The global distribution of primary production and consumption by humans (fisheries) is well-documented, but we have no map linking the central ecological process of consumption within food webs to temperature and other ecological drivers. Using standardized assays that span 105° of latitude on four continents, we show that rates of bait consumption by generalist predators in shallow marine ecosystems are tightly linked to both temperature and the composition of consumer assemblages. Unexpectedly, rates of consumption peaked at midlatitudes (25 to 35°) in both Northern and Southern Hemispheres

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45

Brandt, A., J. A. Crame, H. Polz, and M. R. A. Thomson. "Late Jurassic tethyan ancestry of Recent southern high-latitude marine isopods (Crustacea, Malacostraca)." Palaeontology 42, no. 4 (1999): 663–75. http://dx.doi.org/10.1111/1475-4983.00090.

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46

Bell, Phil R., Federico Fanti, Mark T. Mitchell, and Philip J. Currie. "Marine reptiles (Plesiosauria and Mosasauridae) from the Puskwaskau Formation (Santonian–Campanian), west-central Alberta." Journal of Paleontology 88, no. 1 (2014): 187–94. http://dx.doi.org/10.1666/13-043.

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Plesiosaurs and mosasaurs are identified from the Puskwaskau Formation of west-central Alberta, Canada. These deposits record the final stages during which the Western Interior Seaway remained open to the Boreal Sea to the North and therefore are important for determining the ranges of high-latitude marine reptiles. Polycotylid and elasmosaurid plesiosaurs shared these waters with russellosaurine (including plioplatecarpine) mosasaurs suggesting a diverse ecology of large-bodied marine predators occupied these high-latitude waters in the early Campanian. This locality, situated at 65°N paleola

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47

Lamy, Frank, Dierk Hebbeln, and Gerold Wefer. "High-Resolution Marine Record of Climatic Change in Mid-latitude Chile during the Last 28,000 Years Based on Terrigenous Sediment Parameters." Quaternary Research 51, no. 1 (1999): 83–93. http://dx.doi.org/10.1006/qres.1998.2010.

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AbstractMarine sediment cores from the continental slope off mid-latitude Chile (33°S) were studied with regard to grain-size distributions and clay mineral composition. The data provide a 28,000-yr14C accelerator mass spectrometry-dated record of variations in the terrigenous sediment supply reflecting modifications of weathering conditions and sediment source areas in the continental hinterland. These variations can be interpreted in terms of the paleoclimatic evolution of mid-latitude Chile and are compared to existing terrestrial records. Glacial climates (28,000–18,000 cal yr B.P.) were g

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48

Varela, Augusto Nicolás, María Sol Raigemborn, Patricio Emmanuel Santamarina, Sabrina Lizzoli, Thierry Adatte, and Ulrich Heimhofer. "Carbon Isotopic Signature and Organic Matter Composition of Cenomanian High-Latitude Paleosols of Southern Patagonia." Geosciences 11, no. 9 (2021): 378. http://dx.doi.org/10.3390/geosciences11090378.

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The Cenomanian Mata Amarilla Formation (MAF) in southern Patagonia (~55° S paleolatitude, Austral-Magallanes Basin, Argentina) is composed mainly of stacked fluvial deposits with intercalated paleosols, which document Cenomanian environments at high-paleolatitudes in the Southern Hemisphere. We performed a multiproxy study of the paleosols and sediments of the MAF in order to (1) understand the composition of the soil- and sediment-derived organic matter (OM), (2) apply carbon isotope stratigraphy as a tool to correlate patterns obtained from the MAF with existing marine and non-marine δ13Corg

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49

Holst, T., A. Arneth, S. Hayward, et al. "BVOC ecosystem flux measurements at a high latitude wetland site." Atmospheric Chemistry and Physics Discussions 8, no. 6 (2008): 21129–69. http://dx.doi.org/10.5194/acpd-8-21129-2008.

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Abstract. In this study, we present summertime concentrations and fluxes of biogenic volatile organic compounds (BVOCs) measured at a sub-arctic wetland in northern Sweden using a disjunct eddy-covariance (DEC) technique based on a proton transfer reaction mass spectrometer (PTR-MS). The vegetation at the site was dominated by Sphagnum, Carex and Eriophorum spp. The performance of the DEC system was assessed by comparing H3O+-ion cluster formed with water molecules (H3O+(H2O) at m37) with water vapour concentration measurements made using an adjacent humidity sensor, and from a comparison of s

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50

Jones, Miranda C., and William W. L. Cheung. "Multi-model ensemble projections of climate change effects on global marine biodiversity." ICES Journal of Marine Science 72, no. 3 (2014): 741–52. http://dx.doi.org/10.1093/icesjms/fsu172.

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Abstract Species distribution models (SDMs) are important tools to explore the effects of future global changes in biodiversity. Previous studies show that variability is introduced into projected distributions through alternative datasets and modelling procedures. However, a multi-model approach to assess biogeographic shifts at the global scale is still rarely applied, particularly in the marine environment. Here, we apply three commonly used SDMs (AquaMaps, Maxent, and the Dynamic Bioclimate Envelope Model) to assess the global patterns of change in species richness, invasion, and extinctio

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