4.3 Article

Impact of shelf-transformed waters (STW) on foraminiferal assemblages in the outwash and glacial fjords of Adventfjorden and Hornsund, Svalbard

Journal

OCEANOLOGIA
Volume 59, Issue 4, Pages 525-540

Publisher

POLISH ACAD SCIENCES INST OCEANOLOGY
DOI: 10.1016/j.oceano.2017.04.006

Keywords

Arctic; Fjords; Foraminifera

Categories

Funding

  1. National Science Center [2012/04/A/NZ8/00661]
  2. QUAL project - Academy of Finland [259343]

Ask authors/readers for more resources

A new data set of benthic foraminiferal assemblages from Adventfjorden(tributary fjord of Isfjorden, West Spitsbergen) was compared with the results of a study conducted by Zajaczkowski etal. (2010) in Hornsund (West Spitsbergen). According to Nilsenetal. (2016), Atlantic water inflow to the Isfjorden Trough occurs more readily than to anywhere else along the shelf of Spitsbergen; thus, we compared the foraminiferal assemblages of the outwash Adventfjorden fjord, located in the Isfjorden system, with glacial Hornsund, located in southwest Spitsbergen. Despite the juxtaposition of Adventfjorden and Hornsund the data revealed varying impacts of shelf-transformed water (STW) on the benthic foraminiferal assemblages. Outer and central Adventfjorden was dominated by Adercotryma glomerata, Recurvoides turbinata and Spiroplectammina sp., reflecting the presence of STW, while abundant Melonis barleeanus in the central area of the fjord indicated a large flux of unaltered organic matter. Only the head of the fjord was dominated by the glaciomarine taxa Cassidulina reniforme and Elphidium clavatum. Foraminifera lfauna characteristic of STW-influenced environments (i.e., Nonionellinalabradorica and R. turbinata) were also observed in outer Hornsund. However, the glacier-proximal taxa E. clavatum and C. reniforme were dominant throughout the fjord, demonstrating the impacts of meltwater and high sedimentation. Therefore, it is likely that in Hornsund, glacial impact is a major environmental factor, which is stronger than the influence of STW. (C) 2017 Institute of Oceanology of the Polish Academy of Sciences. Production and hosting by Elsevier Sp. zo.o. This is an open access article under the CC BY-NC-ND license.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.3
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

Article Environmental Sciences

Plastic debris composition and concentration in the Arctic Ocean, the North Sea and the Baltic Sea

Jari Hanninen, Markus Weckstrom, Joanna Pawlowska, Natalia Szymanska, Emilia Uurasjarvi, Marek Zajaczkowski, Samuel Hartikainen, Ilppo Vuorinen

Summary: Neuston samples collected from different locations in the Arctic Ocean, Northern Atlantic Ocean, and the Baltic Sea contained low concentrations of microplastics, mainly consisting of polyethylene fragments. Films and fibers were scarce in the samples analyzed.

MARINE POLLUTION BULLETIN (2021)

Article Biology

Foraminifera-derived carbon contribution to sedimentary inorganic carbon pool: A case study from three Norwegian fjords

Natalia Szymanska, Magdalena Lacka, Katarzyna Koziorowska-Makuch, Karol Kulinski, Joanna Pawlowska, Agnieszka Kujawa, Maciej Mateusz Telesinski, Marek Zajaczkowski

Summary: Norwegian fjords are recognized as carbon burial hot spots due to the large amounts of terrestrial organic matter delivered to their sediments. The contribution of calcareous foraminifera to inorganic carbon pools in sediments varies between southern and northern fjords, with larger species making a significant contribution in the southern fjords. The composition of foraminifera species plays a crucial role in determining the amount of foraminifera-derived carbon in the sediments.

GEOBIOLOGY (2021)

Article Environmental Sciences

Zooplankton and sediment fluxes in two contrasting fjords reveal Atlantification of the Arctic

Agata Weydmann-Zwolicka, Paula Pratnicka, Magdalena Lacka, Sanna Majaneva, Finlo Cottier, Jorgen Berge

Summary: This study assessed the impacts of recent Atlantification on the functioning of zooplankton communities in Svalbard fjords. Results showed that zooplankton in Kongsfjorden were significantly influenced by water temperature and sediment flux, while in Rijpfjorden, sea ice and water temperature played a more significant role in shaping the zooplankton communities.

SCIENCE OF THE TOTAL ENVIRONMENT (2021)

Article Biodiversity Conservation

Could Norwegian fjords serve as an analogue for the future of the Svalbard fjords? State and fate of high latitude fjords in the face of progressive atlantification

Agnieszka Kujawa, Magdalena Lacka, Natalia Szymanska, Joanna Pawlowska, Maciej M. Telesinski, Marek Zajaczkowski

Summary: Benthic foraminifera in the fjords of Svalbard and Norway show similarities in abundance and species composition but significant differences in biodiversity and quantity. The study suggests that Svalbard fjords will remain distinct in the future even under conditions of further warming or atlantification, while Norwegian fjords may experience changes in foraminiferal assemblages due to human activities.

POLAR BIOLOGY (2021)

Article Geography, Physical

The significance of Atlantic Water routing in the Nordic Seas: The Holocene perspective

Maciej M. Telesinski, Magdalena Lacka, Agnieszka Kujawa, Marek Zajaczkowski

Summary: The Nordic Seas play a crucial role in global ocean circulation, and this research reconstructs the history of Atlantic Water advection in this region over the past 14,000 years. The study reveals the influence of various factors on the flow of Atlantic Water and its changes over time.

HOLOCENE (2022)

Article Biology

Metabarcoding reveals high diversity of benthic foraminifera linked to water masses circulation at coastal Svalbard

Ngoc-Loi Nguyen, Joanna Pawlowska, Ines Barrenechea Angeles, Marek Zajaczkowski, Jan Pawlowski

Summary: This study provides the first assessment of Arctic foraminifera diversity based on metabarcoding of sediment DNA samples, revealing high genetic novelty and differences in community composition influenced by water masses.

GEOBIOLOGY (2023)

Article Geography, Physical

Paleoceanography of the Northwestern Greenland Sea and Return Atlantic Current evolution, 35-4 kyr BP

Dhanushka Devendra, Magdalena Lacka, Maciej M. Telesinski, Tine L. Rasmussen, Kamila Sztybor, Marek Zajaczkowski

Summary: This study reconstructs the paleoceanographic forcing of the Atlantic Water flow in the Northwestern Greenland Sea over the past 35,000 years, providing insights into its variability and its impact on climate conditions and environmental changes.

GLOBAL AND PLANETARY CHANGE (2022)

Article Environmental Sciences

Response of benthic foraminifera to environmental successions of cold seeps from Vestnesa Ridge, Svalbard: Implications for interpretations of paleo-seepage environments

Katarzyna Melaniuk, Kamila Sztybor, Tina Treude, Stefan Sommer, Marek Zajaczkowski, Tine L. Rasmussen

Summary: This study examines the response of living benthic foraminifera to environmental successions in a cold-seep ecosystem. The results show that the distribution patterns of foraminifera change according to the progressing environmental succession. However, foraminifera cannot be used as exclusive indicators of past methane seepage intensity.

FRONTIERS IN MARINE SCIENCE (2022)

Article Geography, Physical

Late Holocene Vistula River floods recorded in grain size distributions and diatom assemblages of marine sediments of the Gulf of Gda′nsk (Baltic Sea)

Marta Szczesniak, Mikolaj Kokocinski, Robert Jagodzinski, Krzysztof Pleskot, Marek Zajaczkowski, Witold Szczucinski

Summary: During the 2010 flood of the Vistula River, a thin layer of medium-grained sand deposits extended up to 70 km into the Gulf of Gdańsk (Baltic Sea). The study aimed to identify flood indicators and reveal paleoflood records in sediment cores from the Gulf of Gdańsk. Analysis of surface samples and sediment cores showed that large flood deposits were not preserved after a year in water depth less than 30 m, while deeper cores consisted of sandy mud with unimodal and occasionally bimodal grain size distributions. Diatom analysis supported the interpretation of certain layers as deposited during river flood events. Evaluation of major flood events in the past was challenging due to changes in river mouth positions.

PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY (2023)

Article Oceanography

Dinoflagellate cysts and benthic foraminifera from surface sediments of Svalbard fjords and shelves as paleoenvironmental indicators

Maciej M. Telesinski, Vera Pospelova, Kenneth Neil Mertens, Malgorzata Kucharska, Marek Zajaczkowski

Summary: Due to the Arctic amplification effect, the Svalbard archipelago is an important area for studying ongoing environmental changes. The most important factor controlling the environment in the region is the Atlantic Water, while factors such as sea-ice cover and tidewater glaciers become increasingly important on a local scale. Two dinocyst species can be considered as indicators of regional winter drift ice. However, the relationship between benthic foraminifera and environmental parameters is more difficult to interpret.

OCEANOLOGIA (2023)

Article Geology

FATE OF SWELLING CLAY MINERALS DURING EARLY DIAGENESIS: A CASE STUDY FROM GDANSK BAY (BALTIC SEA)

Marta Kisiel, Michal Skiba, Mateusz Damrat, Artur Kuligiewicz, Katarzyna Maj-szeliga, Magdalena Makiel, Marek Zajaczkowski, Dorota Salata

Summary: The study aimed to understand the early diagenetic transformations of clay minerals in the brackish environment of Gdansk Bay. Samples from the Vistula River loads and sediments of the Vistula delta front and prodelta were analyzed. The mineral compositions, layer charge, and major element content of the clay fractions were determined. The results showed that the illite-smectite mixed layered minerals were present in all samples, with variations in other clay minerals and interlayer charge. The smectite component underwent chloritization and illitization, and changes in mineral composition were attributed to selective adsorption and fixation of K+ from seawater.

ANNALES SOCIETATIS GEOLOGORUM POLONIAE (2023)

No Data Available