scholarly journals Biological Response of Planktic Foraminifera to Decline in Seawater pH

Biology ◽  
2022 ◽  
Vol 11 (1) ◽  
pp. 98
Author(s):  
Shuaishuai Dong ◽  
Yanli Lei ◽  
Hongsheng Bi ◽  
Kuidong Xu ◽  
Tiegang Li ◽  
...  
Keyword(s):  
Biological Response ◽  
Biological Processes ◽  
Geological Time ◽  
Planktic Foraminifera ◽  
Geological Time Scale ◽  
Marine Food Web ◽  
Seawater Ph ◽  
Geochemical Indices ◽  
Marine Food ◽  
Biological Development

Understanding the way in which a decline in ocean pH can affect calcareous organisms could enhance our ability to predict the impacts of the potential decline in seawater pH on marine ecosystems, and could help to reconstruct the paleoceanographic events over a geological time scale. Planktic foraminifera are among the most important biological proxies for these studies; however, the existing research on planktic foraminifera is almost exclusively based on their geochemical indices, without the inclusion of information on their biological development. Through a series of on-board experiments in the western tropical Pacific (134°33′54″ E, 12°32′47″ N), the present study showed that the symbiont-bearing calcifier Trilobatus sacculifer—a planktic foraminifer—responded rapidly to a decline in seawater pH, including losing symbionts, bleaching, etc. Several indices were established to quantify the relationships between these biological parameters and seawater pH, which could be used to reconstruct the paleoceanographic seawater pH. We further postulated that the loss of symbionts in planktic foraminifera acts as an adaptive response to the stress of low pH. Our results indicate that an ongoing decline in seawater pH may hinder the growth and calcification of planktic foraminifera by altering their biological processes. A reduction in carbonate deposition and predation could have profound effects on the carbon cycle and energy flow in the marine food web.

2. Marine biological processes

2020 ◽  
pp. 22-47
Author(s):  
Philip V. Mladenov
Keyword(s):  
Primary Productivity ◽  
Marine Mammals ◽  
Global Ocean ◽  
Biological Processes ◽  
Marine Microbes ◽  
Factors Affecting ◽  
Marine Food Web ◽  
Marine Biological ◽  
Marine System ◽  
Marine Food

Roughly half of the planet’s primary production—the synthesis of organic matter by chlorophyll-bearing organisms using light energy from the sun—is produced within the Global Ocean. The primary producers in the oceans are phytoplanktonic microbes suspended in the sunlit surface layer. These energy-fixing microorganisms form the basis of the marine food web, the network of pathways through which food energy is transferred to all the other organisms in the marine system including other microbes, zooplankton, fish, marine mammals, and, ultimately, humans. ‘Marine biological processes’ outlines the four main groups of marine microbes—bacteria, archaea, protists, and viruses—and discusses the factors affecting marine primary productivity.

scholarly journals Complexities of disturbance response in a marine food web

2021 ◽  
Author(s):  
Kristy A. Lewis ◽  
Robert R. Christian ◽  
Charles W. Martin ◽  
Kira L. Allen ◽  
Ashley M. McDonald ◽  
...  
Keyword(s):  
Food Web ◽  
Marine Food Web ◽  
Disturbance Response ◽  
Marine Food

The Role of Ammonites in the Mesozoic Marine Food Web Revealed by Jaw Preservation

Science ◽  
2011 ◽  
Vol 331 (6013) ◽  
pp. 70-72 ◽  
Author(s):  
I. Kruta ◽  
N. Landman ◽  
I. Rouget ◽  
F. Cecca ◽  
P. Tafforeau
Keyword(s):  
Food Web ◽  
Marine Food Web ◽  
Marine Food

scholarly journals Inter-annual cascade effect on marine food web: A benthic pathway lagging nutrient supply to pelagic fish stock

PLoS ONE ◽  
2017 ◽  
Vol 12 (9) ◽  
pp. e0184512 ◽  
Author(s):  
Lohengrin Dias de Almeida Fernandes ◽  
Eduardo Barros Fagundes Netto ◽  
Ricardo Coutinho ◽  
Keyword(s):  
Food Web ◽  
Nutrient Supply ◽  
Pelagic Fish ◽  
Fish Stock ◽  
Marine Food Web ◽  
Cascade Effect ◽  
Marine Food

Trophic transfer of heavy metals in the marine food web based on tissue residuals

2021 ◽  
Vol 772 ◽  
pp. 145064
Author(s):  
Yongfei Gao ◽  
Ruyue Wang ◽  
Yanyu Li ◽  
Xuebin Ding ◽  
Yueming Jiang ◽  
...  
Keyword(s):  
Heavy Metals ◽  
Food Web ◽  
Trophic Transfer ◽  
Web Based ◽  
Marine Food Web ◽  
Marine Food

Phytoplankton in the embayments of King George Island (Antarctic Peninsula): a review with emphasis on diatoms

Polar Record ◽  
2018 ◽  
Vol 54 (2) ◽  
pp. 158-175 ◽  
Author(s):  
Priscila Kienteca Lange ◽  
Ryszard Ligowski ◽  
Denise Rivera Tenenbaum
Keyword(s):  
Antarctic Peninsula ◽  
Early Summer ◽  
Western Antarctic Peninsula ◽  
King George Island ◽  
Accurate Identification ◽  
Phytoplankton Assemblages ◽  
Marine Food Web ◽  
Planktonic Diatoms ◽  
Local Material ◽  
Marine Food

ABSTRACTConsidering that phytoplankton assemblages are good bioindicators of environmental conditions, the sensitivity of the Western Antarctic Peninsula (WAP) to climate change, and the importance of some areas of its islands as Antarctic Specially Managed Areas, this work assembles published datasets on phytoplankton biodiversity and ecology in confined coastal areas (embayments) of King George Island, WAP. Over 33 years (1980–2013), 415 species from 122 genera have been identified to species level, being mostly diatoms (371 species), with 10 new species described with local material (6 diatoms, 4 cyanobacteria). The importance of diatoms was indicated by the frequent occurrence of Corethron pennatum, Pseudogomphonema kamtshaticum, and abundant benthic genera in the plankton (e.g. Navicula, Cocconeis). The increased contribution of dinoflagellates after 2010 suggests marked changes in the water column. Early-summer blooms differ between the bays' eastern and western shores, with terrestrial melting and wind-driven upwelling inducing the dominance of benthic species at eastern shores, whereas planktonic diatoms (Thalassiosira, Pseudo-nizschia, and Chaetoceros) are most abundant along western shores and central areas. The importance of an accurate identification of organisms that are becoming key ecological components of the region is discussed, as recent changes in the microflora may affect the entire marine food web.

Neogene and Quaternary coexisting in the geological time scale: The inclusive compromise

2009 ◽  
Vol 96 (4) ◽  
pp. 249-262 ◽  
Author(s):  
Brian McGowran ◽  
Bill Berggren ◽  
Frits Hilgen ◽  
Fritz Steininger ◽  
Marie-Pierre Aubry ◽  
...  
Keyword(s):  
Time Scale ◽  
Geological Time ◽  
Geological Time Scale

scholarly journals Rheological profiles in the Central- Eastern Mediterranean

1997 ◽  
Vol 40 (4) ◽  
Author(s):  
M. Viti ◽  
D. Albarello ◽  
E. Mantovani
Keyword(s):  
Heat Flow ◽  
Large Scale ◽  
Eastern Mediterranean ◽  
Mediterranean Area ◽  
Geological Time ◽  
Western Turkey ◽  
Geological Time Scale ◽  
Total Strength ◽  
The Mediterranean ◽  
Wet Rocks

Seismological investigations have provided an estimate of the gross structnral features of the crust/upper mantle system in the Mediterranean area. However, this information is only representative of the short-term me- chanical behaviour of rocks and cannot help us to understand slow deformations and related tectonic processes on the geological time scale. In this work strength envelopes for several major structural provinces of the Mediterranean area have been tentatively derived from seismological stratification and heat flow data, on the assumption of constant and uniforrn strain rate (10-16 S-1), wet rocks and conductive geotherm. It is also shown how the uncertainties in the reconstruction of thermal profiles can influence the main rheological prop- erties of the lithosphere, as thickness and total strength. The thickest (50-70 km) and strongest mechanical lithospheres correspond to the coldest zones (with heat flow lower than or equal to 50 mW m-2), i.e., the Io- nian and Levantine mesozoic basins, the Adriatic and Eurasian foreland zones and NW Greece. Heat flows larger than 65 mW m-2, generally observed in extensional zones (Tyrrhenian, Sicily Channel, Northern Aegean, Macedonia and Western Turkey), are mostly related to mechanical lithospheres thinner than 20 km. The characteristics of strength envelopes, and in particular the presence of soft layers in the crust, suggest a reasonable interpretation of some large-scale features which characterize the tectonic evolution of the Central- Eastem Mediterranean.

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