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Ventilation of the Upper Oxygen Minimum Zone in the Coastal Region Off Mexico: Implications of El Niño 2015–2016

Abstract.

"As a result of anthropogenic activities, it has been predicted that the ocean will be challenged with rising temperature, increased stratification, ocean acidification, stronger more frequent tropical storms, and oxygen depletion. In the tropical Pacific off central Mexico all these phenomena are already occurring naturally, providing a laboratory from which to explore ocean biogeochemical dynamics that are predicted under future anthropogenic forcing conditions. "

Source: Frontiers in Marine Science
Authors: Pablo N. Trucco-Pignata et al.
DOI: 10.3389/fmars.2019.00459

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Quantifying the Relative Importance of Riverine and Open‐Ocean Nitrogen Sources for Hypoxia Formation in the Northern Gulf of Mexico

Abstract.

"The Mississippi and Atchafalaya River System discharges large amounts of freshwater and nutrients into the northern Gulf of Mexico (NGoM). These lead to increased stratification and elevate primary production in the outflow region. Consequently, hypoxia (oxygen <62.5 mmol/m3), extending over an area of roughly 15,000 km2, forms every summer in bottom waters. [...]"

Source: JGR Oceans
Authors: Fabian Große et al.
DOI: 10.1029/2019JC015230

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A Synthesis of Opportunities for Applying the Telecoupling Framework to Marine Protected Areas

Abstract.

"The world’s oceans face unprecedented anthropogenic threats in the globalized era that originate from all over the world, including climate change, global trade and transportation, and pollution. Marine protected areas (MPAs) serve important roles in conservation of marine biodiversity and ecosystem resilience, but their success is increasingly challenged in the face of such large-scale threats. [...]"

Source: Sustainability
Authors: Vanessa Hull et al.
DOI: 10.3390/su11164450

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The effect of marine aggregate parameterisations on nutrients and oxygen minimum zones in a global biogeochemical model

Abstract.

"Particle aggregation determines the particle flux length scale and affects the marine oxygen concentration and thus the volume of oxygen minimum zones (OMZs) that are of special relevance for ocean nutrient cycles and marine ecosystems and that have been found to expand faster than can be explained by current state-of-the-art models. [...]"

Source: Biogeosciences
Author: Daniela Niemeyer et al.
DOI: 10.5194/bg-16-3095-2019

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The influence of dissolved organic matter on the marine production of carbonyl sulfide (OCS) and carbon disulfide (CS2) in the Peruvian upwelling

Abstract.

"Oceanic emissions of the climate-relevant trace gases carbonyl sulfide (OCS) and carbon disulfide (CS2) are a major source to their atmospheric budget. Their current and future emission estimates are still uncertain due to incomplete process understanding and therefore inexact quantification across different biogeochemical regimes.  [...]"

Source: Ocean Science
Authors: Sinikka T. Lennartz et al.
DOI: 10.5194/os-15-1071-2019

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Study tests resilience of the Salish Sea to climate change impacts

"What will the ecology of the Salish Sea look like in the year 2095?

It's an important question for millions of people who live along and near the shores of this intricate, interconnected network of coastal waterways, inlets, bays, and estuaries that encompasses Puget Sound in Washington state and the deep waters of southwest British Columbia. A research team from PNNL found that the inner Salish Sea is resilient, and that future response to climate change—while significant—will be less severe than the open ocean. [...]"

Source: phys.org

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High-resolution underwater laser spectrometer sensing provides new insights into methane distribution at an Arctic seepage site

Abstract.

"Methane (CH4) in marine sediments has the potential to contribute to changes in the ocean and climate system. Physical and biochemical processes that are difficult to quantify with current standard methods such as acoustic surveys and discrete sampling govern the distribution of dissolved CH4 in oceans and lakes. [...]"

Source: Ocean Science
Authors: Pär Jansson et al. 
DOI: 10.5194/os-15-1055-2019

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Brief oxygenation events in locally anoxic oceans during the Cambrian solves the animal breathing paradox

Abstract.

"Oxygen is a prerequisite for all large and motile animals. It is a puzzling paradox that fossils of benthic animals are often found in black shales with geochemical evidence for deposition in marine environments with anoxic and sulfidic bottom waters. It is debated whether the geochemical proxies are unreliable, affected by diagenesis, or whether the fossils are transported from afar or perhaps were not benthic.  [...]"

Source: Scientific Reports
Authors: Tais W. Dahl et al.
DOI: 10.1038/s41598-019-48123-2

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Global Perspectives on Observing Ocean Boundary Current Systems

Abstract.

"Ocean boundary current systems are key components of the climate system, are home to highly productive ecosystems, and have numerous societal impacts. Establishment of a global network of boundary current observing systems is a critical part of ongoing development of the Global Ocean Observing System. The characteristics of boundary current systems are reviewed, focusing on scientific and societal motivations for sustained observing. Techniques currently used to observe boundary current systems are reviewed, followed by a census of the current state of boundary current observing systems globally. The next steps in the development of boundary current observing systems are considered, leading to several specific recommendations. [...]"

Source: Frontiers in Marine Science
Authors: Robert E. Todd et al.
DOI: 10.3389/fmars.2019.00423

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Microbial diversity of the Arabian Sea in the Oxygen minimum zones by metagenomics approach

Abstract.

"Large oxygen depleted areas known as oxygen minimum zones (OMZ) have been observed in the Arabian Sea and recent reports indicate that these areas are expanding at an alarming rate. In marine waters, oxygen depletion may also be related to global warming and the temperature rise, acidification and deoxygenation can lead to major consequences wherein the plants, fish and other biota will struggle to survive in the ecosystem. [...]"

Source: bioRxiv
Authors: Mandar S Paingankar et al.
DOI: 10.1101/731828

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