Job offer: Postdoctoral researcher in Ocean Biogeochemistry
"The High Meadows Environmental Institute at Princeton University is seeking a Postdoctoral research associate or more senior researcher in the area of ocean biophysical modeling to work with Professor Laure Resplandy. The researcher will investigate the impact of climate change and human perturbations on ocean oxygenation and coastal hypoxia. The researcher will specifically examine how riverine nutrient loadings and aerosol deposition control oxygen levels and how the risk of coastal hypoxia, which is crucial for ecosystem and ecosystem services, will evolve in the future. The position is funded by an NSF CAREER grant (Award # 2042672).
The ideal candidate will have a strong background in numerical modeling, but candidates with the necessary background in geophysical fluid dynamics and/or ocean biogeochemistry will be given full consideration. A Ph.D. in Geosciences or related field is required. The position is available for one year, with a possibility for renewal contingent upon satisfactory performance and funding. Postdoctoral appointments are initially for one year with the renewal for subsequent years based on satisfactory performance and continued funding. A competitive salary is offered commensurate with experience and qualifications.
Applicants should apply online to https://www.princeton.edu/acad-positions/position/24941."
Ostracod response to monsoon and OMZ variability over the past 1.2 Myr
"We present the first continuous middle through late Pleistocene record of fossil ostracods from the Maldives in the northern Indian Ocean, derived from sediment cores taken at Site U1467 by Expedition 359 of the International Ocean Discovery Program (IODP). Site U1467 lies at 487 m water depth in the Inner Sea of the Maldives archipelago, an ideal place for studying the effects of the South Asian Monsoon (SAM) system on primary productivity, intermediate depth ocean circulation, and the regional oxygen minimum zone (OMZ). [...]".
Source: Science Direct
Authors: Carlos A. Alvarez Zarikian et al.
Biotic induction and microbial ecological dynamics of Oceanic Anoxic Event 2
"Understanding the causal mechanisms of past marine deoxygenation is critical to predicting the long-term Earth systems response to climate change. However, the processes and events preceding widespread carbon burial coincident with oceanic anoxic events remain poorly constrained. Here, we report a comprehensive biomarker inventory enveloping Oceanic Anoxic Event 2 that captures microbial communities spanning epipelagic to benthic environments in the southern proto-North Atlantic Ocean. We identify an abrupt, sustained increase in primary productivity that predates Oceanic Anoxic Event 2 by ∼220 ± 4 thousand years, well before other geochemical proxies register biogeochemical perturbations. [...]".
Source: Communications Earth & Environment
Authors: Gregory T. Connock et al.
Oceanic anoxia and extinction in the latest Ordovician
"The Late Ordovician (Hirnantian) mass extinction (LOME) was marked by two discrete pulses of high species turnover rates attributed to glacial cooling (LOME-1) and subsequent expansion of anoxic marine conditions (LOME-2). However, the mechanisms and extent of global marine anoxia remain controversial. In this study, we present uranium isotope (U) data from a new Ordovician-Silurian (O-S) boundary carbonate section in the Southwest China to explore the extent/duration of the global marine anoxia, and links to the LOME. [...]".
Source: Science Direct
Authors: Mu Liu et al.
On anomalously high sub-surface dissolved oxygen in the Indian sector of the Southern Ocean
"The Southern Ocean (SO) plays a critical role in global ocean productivity and carbon cycling. Bio-Argo floats deployed in the Indian sector of the Southern Ocean provides new insights into the biogeochemical processes. Here we report significantly higher dissolved oxygen (DO) (~ 310 μmol/kg) in summer of 2014–2015 for one float (F1) and winter of 2014 in other float (F2) at sub-surface layer in the subantarctic region of the SO. The summer DO peak in F1 was 10% higher than those during the summer of succeeding year, while the winter DO peak in F2 was 20% higher than those during the winter of succeeding year. [...]".
Source: Journal of Oceanography
Authors: Prince Prakash et al.
Coastlines at Risk of Hypoxia From Natural Variability in the Northern Indian Ocean
"Coastal hypoxia—harmfully low levels of oxygen—is a mounting problem that jeopardizes coastal ecosystems and economies. The northern Indian Ocean is particularly susceptible due to human-induced impacts, vast naturally occurring oxygen minimum zones, and strong variability associated with the seasonal monsoons and interannual Indian Ocean Dipole (IOD). We assess how natural factors influence the risk of coastal hypoxia by combining a large set of oxygen measurements with satellite observations to examine how the IOD amplifies or suppresses seasonal hypoxia tied to the Asian Monsoon. We show that on both seasonal and interannual timescales hypoxia is controlled by wind- and coastal Kelvin wave-driven upwelling of oxygen-poor waters onto the continental shelf and reinforcing biological feedbacks (increased subsurface oxygen demand). [...]".
Source: Global Biogeochemical Cycles
Authors: Jenna Pearson et al.
Trace elements V, Ni, Mo and U: A geochemical tool to quantify dissolved oxygen concentration in the oxygen minimum zone of the north-eastern Pacific
"Deoxygenation of the water column in the oceans and in the oxygen minimum zone (OMZ) has become relevant due to its connection with global climate change. The variability of the OMZ has been inferred by in situ measurements for the last 70 years and qualitatively assessed through the monitoring of trace elements and the nitrogen stable isotope ratio (δ15N) of organic matter on several time scales. The V, Ni, Mo and U concentrations in surface sediments and the dissolved oxygen concentration in the water column of La Paz Bay and the Mazatlán margin were used to propose an exponential regression model. This model will allow the inference of the dissolved oxygen concentration in the sedimentary records from the Alfonso Basin in La Paz Bay and in the Mazatlán margin over the last 250 years. [...]".
Source: Science Direct
Authors: Alberto Sánchez et al.
Widespread oxyregulation in tropical corals under hypoxia
"Hypoxia (low oxygen stress) is increasingly reported on coral reefs, caused by ocean deoxygenation linked to coastal nutrient pollution and ocean warming. While the ability to regulate respiration is a key driver of hypoxia tolerance in many other aquatic taxa, corals' oxyregulatory capabilities remain virtually unexplored. Here, we examine O2-consumption patterns across 17 coral species under declining O2partial pressure (pO2). All corals showed ability to oxyregulate, but total positive regulation (Tpos) varied between species, ranging from 0.41 (Pocillopora damicornis) to 2.42 (P. acuta). [...]".
Source: Science Direct
Authors: David J. Hughes et al.
Marine anoxia linked to abrupt global warming during Earth’s penultimate icehouse
"Piecing together the history of carbon (C) perturbation events throughout Earth’s history has provided key insights into how the Earth system responds to abrupt warming. Previous studies, however, focused on short-term warming events that were superimposed on longer-term greenhouse climate states. Here, we present an integrated proxy (C and uranium [U] isotopes and paleo CO2) and multicomponent modeling approach to investigate an abrupt C perturbation and global warming event (∼304 Ma) that occurred during a paleo-glacial state. We report pronounced negative C and U isotopic excursions coincident with a doubling of atmospheric CO2 partial pressure and a biodiversity nadir. [...]".
Source: Proceedings of the National Academy of Sciences
Authors: Jitao Chen et al.
Geochemistry of sediments in contact with oxygen minimum zone of the eastern Arabian Sea: Proxy for palaeo-studies
"The Arabian Sea encompasses oxygen minimum zone with denitrifying conditions. For the present study, sediments were collected across three transects off Goa transect (GT), Mangalore transect (MT) and Kochi transect (KT) in contact with water column dissolved oxygen (DO) range of 1.4–118.0 µM. Sediments were investigated for texture, clay mineralogy, total organic carbon (Corg), total nitrogen, CaCO3, δ15N, δ13C, metal content to infer their distribution with changing DO and their use as possible palaeo-proxies. The Corg (0.9–8.6%) is largely marine and δ15N from GT and MT preserves signatures of higher water column denitrification. [...]".
Source: Journal of Earth System Science
Authors: Pratima M. Kessarkar et al.
It is possible to subscribe to our email newsletter list.
Depending on the amount of publications and articles, we will summarize the activities on this blog in a newsletter for everyone not following the blog regularly.
If you want to subscribe to the email list to receive the newsletter, please send an email to email@example.com with the header "subscribe".
If you want to unsubscribe from the newsletter, please send an email to firstname.lastname@example.org with the header "unsubscribe".
As a regular member to the list you cannot forward any messages. If you want to suggest new articles or would like to contact us because of any other issue, please send an email to email@example.com.