Marine Nitrogen Cycling and Food Webs

A special issue of Diversity (ISSN 1424-2818). This special issue belongs to the section "Marine Diversity".

Deadline for manuscript submissions: closed (15 December 2021) | Viewed by 5830

Special Issue Editors


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Guest Editor
Centro Nacional Instituto Español de Oceanografia (IEO-CSIC), Centro Oceanografico de A Coruña, 15001 A Coruña, Spain
Interests: marine plankton ecology; nitrogen cycle; food webs; stable isotopes
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Guest Editor
Instituto Espanol de Oceanografia, Madrid, Spain
Interests: microbial oceanography; molecular ecology; functional structure; organic matter

Special Issue Information

Dear Colleagues,

Nitrogen is a key element in marine food webs. First, because it limits primary producers in most of the ocean. Second, because it is essential for the building of major biomolecules, as proteins and nucleic acids, which are required for maintaining marine life. The nitrogen cycle in the ocean is closely linked with those of other biologically important elements (e.g., carbon and phosphorus cycles) by stoichiometric requirements. Recent recalculations of the global nitrogen cycle have noted a remarkable balance between sources and sinks of nitrogen in the ocean that critically depends on a spatial separation of biologically-mediated assimilation and loss processes. With a longer lifetime of reactive nitrogen in the ocean than in terrestrial ecosystems, about it is still uncertain how the nitrogen cycle will be affected by global changes such as the input of antropogenic nitrogen and the warming of surface waters.

New discoveries have indicated the major importance of the biological control of atmospheric nitrogen fixation and denitrification in much larger areas of the ocean than previously considered (e.g., temperate upwelling regions). The diversity of nitrogen fixers has just started to be revealed using advanced molecular and genomic methods. The impact of fixed nitrogen extends over the entire food web and is transported to traditionally considered nitrogen-deficient regions by long-distance travelling upper consumers (such as tuna). Zooplankton grazing may be one of the main controls of the cycling of nitrogen, affecting, for instance, the spatial decoupling between nitrogen fixation and denitrification, and the remineralization of organic nitrogen by bacteria and archaea, as suggested by recent studies. Zooplankton and mesopelagic fish actively contribute to the transfer of nitrogen, from productive surface waters to deep ocean layers. Methodological developments have also challenged the existing database of experimental nitrogen rate measurements as well as the reconstruction of long-term changes in food webs from alterations in climate and local oceanography affecting the nitrogen cycle.

Major challenges for current research are to determine the consequences of climate change for ocean nitrogen cycling and their effects on other biogeochemical processes and ecosystem functions and services.

The aim of this Special Issue is to provide an overview of recent approaches to the study of the cycling of nitrogen in marine food webs through contributions dealing with the following:

  • The molecular diversity of marine nitrogen fixers;
  • Rates and magnitude of nitrogen cycling (diazotrophy, the uptake and recycling of dissolved inorganic and organic nitrogen);
  • Spatial and temporal patterns of nitrogen-influenced changes in food web structure;
  • Nitrogen control on ocean carbon sequestration;
  • The environmental and climatic influence of ocean nitrogen cycling.

as well as other relevant topics using specific or generic methodologies applied to the nitrogen cycle (e.g., genomics, stable isotopes, microscopic analysis, etc.).

Dr. Antonio Bode
Dr. Marta M. Varela
Guest Editors

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Published Papers (2 papers)

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Research

17 pages, 1857 KiB  
Article
The Role of Cymodocea nodosa and Caulerpa prolifera Meadows as Nitrogen Sinks in Temperate Coastal Lagoons
by Jaime Bernardeau-Esteller, José Miguel Sandoval-Gil, María Dolores Belando, Aranzazu Ramos-Segura, Rocío García-Muñoz, Lazaro Marín-Guirao and Juan Manuel Ruiz
Diversity 2023, 15(2), 172; https://0-doi-org.brum.beds.ac.uk/10.3390/d15020172 - 26 Jan 2023
Cited by 5 | Viewed by 1993
Abstract
In coastal lagoons, marine benthic macrophyte meadows can be an important element in the resistance to eutrophication of the ecosystem, as they can function as temporary nitrogen sinks, limiting the availability of this nutrient for opportunistic organisms. The role of nitrogen sinks for [...] Read more.
In coastal lagoons, marine benthic macrophyte meadows can be an important element in the resistance to eutrophication of the ecosystem, as they can function as temporary nitrogen sinks, limiting the availability of this nutrient for opportunistic organisms. The role of nitrogen sinks for two dominant macrophyte species of Mediterranean coastal lagoons, the seagrass Cymodocea nodosa and the seaweed Caulerpa prolifera, was analysed by two different approaches: (i) studying nitrate (NO3-) and ammonium (NH4+) uptake kinetics of aboveground tissues in a laboratory and (ii) estimating nitrogen stocks and demands of meadows under natural conditions. The studies were carried out in the coastal lagoon of the Mar Menor, which has been subjected to high anthropogenic nitrogen inputs for decades. While both macrophytes were efficient in exploiting NH4+ from the water column, only C. prolifera showed a high NO3- uptake capacity. Large N pools in the C. nodosa and C. prolifera meadows of the Mar Menor were detected, suggesting that these habitats may have the potential to be essential reservoirs for this nutrient. However, the major role of belowground tissues of the seagrasses in nitrogen accumulation may determine important differences between the two species in temporary N storage and sequestration. The data on N demands for the meadows of both macrophytes in the Mar Menor suggest an important contribution of these habitats in controlling the inputs of this nutrient into the lagoon. We conclude that C. nodosa and C. prolifera meadows can play a key role as a sink for dissolved inorganic nitrogen in temperate coastal lagoons, being an important mechanism of resistance to eutrophication. Full article
(This article belongs to the Special Issue Marine Nitrogen Cycling and Food Webs)
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14 pages, 2065 KiB  
Article
Effects of Upwelling Intensity on Nitrogen and Carbon Fluxes through the Planktonic Food Web off A Coruña (Galicia, NW Spain) Assessed with Stable Isotopes
by Antonio Bode, Angel F. Lamas and Carmen Mompeán
Diversity 2020, 12(4), 121; https://doi.org/10.3390/d12040121 - 25 Mar 2020
Cited by 6 | Viewed by 3050
Abstract
The input of new nutrients by upwelling in shelf waters, and the associated carbon and nitrogen fluxes, can be traced by their stable isotope signatures in organic matter. Here, we analyze the relationships between upwelling intensity and natural abundance of stable carbon and [...] Read more.
The input of new nutrients by upwelling in shelf waters, and the associated carbon and nitrogen fluxes, can be traced by their stable isotope signatures in organic matter. Here, we analyze the relationships between upwelling intensity and natural abundance of stable carbon and nitrogen isotopes in seston, sedimented particles, and four plankton size fractions (200 to 5000 µm) sampled monthly during 2010 and 2011 in a seasonal upwelling ecosystem. Upwelling modified the seasonal warming stratification by introducing cold and nutrient-rich waters in subsurface layers, enhancing chlorophyll-a and diatom abundance. Seston and sedimented particles were enriched in heavy nitrogen (but not carbon) isotopes linearly with upwelling intensity, indicating a primary effect of upwelling on phytoplankton production. In contrast, all plankton fractions were enriched in heavy carbon isotopes with upwelling, mainly due to the consumption of diatoms. These results confirm the differential effect of upwelling on nitrogen and carbon fluxes in the plankton food web. Direct effects of the new nitrogen inputs on phytoplankton are less evident with the increase of plankton size as nitrogen is repeatedly recycled, while the enriched carbon of plankton suggests the consumption of diatoms during upwelling. We provide linear equations to assess the influence of changes in upwelling intensity on nitrogen and carbon fluxes in seston and plankton in this ecosystem, as well as to estimate reference baseline values for food web studies. Full article
(This article belongs to the Special Issue Marine Nitrogen Cycling and Food Webs)
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