Sven Pallacks

ORCID: 0000-0002-8215-0007
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About
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Research Areas
  • Marine Biology and Ecology Research
  • Marine and coastal ecosystems
  • Geology and Paleoclimatology Research
  • Ocean Acidification Effects and Responses
  • Coral and Marine Ecosystems Studies
  • Isotope Analysis in Ecology
  • Marine animal studies overview
  • Geological and Geophysical Studies Worldwide
  • Methane Hydrates and Related Phenomena

Universitat Autònoma de Barcelona
2021-2024

Abstract The cycling of biologically produced calcium carbonate (CaCO 3 ) in the ocean is a fundamental component global carbon cycle. Here, we present experimental determinations situ coccolith and foraminiferal calcite dissolution rates. We combine these rates with solid phase fluxes, dissolved tracers, historical data to constrain alkalinity cycle shallow North Pacific Ocean. coccolithophores demonstrate nonlinear dependence on saturation state. Dissolution all three major calcifying...

10.1029/2022gb007388 article EN publisher-specific-oa Global Biogeochemical Cycles 2022-05-01

Abstract Planktonic calcifying organisms play a key role in regulating ocean carbonate chemistry and atmospheric CO 2 . Surprisingly, references to the absolute relative contribution of these calcium production are lacking. Here we report quantification pelagic North Pacific, providing new insights on three main planktonic groups. Our results show that coccolithophores dominate living (CaCO 3 ) standing stock, with coccolithophore calcite comprising ~90% total CaCO production, pteropods...

10.1038/s41467-023-36177-w article EN cc-by Nature Communications 2023-02-20

Abstract Anthropogenic carbon dioxide emissions directly or indirectly drive ocean acidification, warming and enhanced stratification. The combined effects of these processes on marine planktic calcifiers at decadal to centennial timescales are poorly understood. Here, we analyze size normalized foraminiferal shell weight, geochemistry, supporting proxies from 3 sediment cores in the Mediterranean Sea spanning several centuries. Our results allow us investigate response surface-dwelling...

10.1038/s43247-023-00947-7 article EN cc-by Communications Earth & Environment 2023-08-28

The increase in anthropogenic induced warming over the last two centuries is impacting marine environment.Planktic foraminifera are a globally distributed calcifying zooplankton responding sensitively to changes sea surface temperatures and interacting with food web structure.Here, we study high resolution multicore records from western Mediterranean Sea regions (Alboran Balearic basins), areas highly affected by both natural climate change warming.Cores cover time interval Medieval Climate...

10.1016/j.gloplacha.2021.103549 article EN cc-by-nc-nd Global and Planetary Change 2021-06-24

Abstract Marine functional connectivity (MFC) refers to the flows of organic matter, genes, and energy that are caused by active passive movements marine organisms. Occurring at various temporal spatial scales, MFC is a dynamic, constantly evolving global ecological process, part overall connectivity, but with its own distinct specific patterns. Geological historical archives changes in distributions, life histories, migration species can provide baselines for deciphering long-term trends...

10.1093/icesjms/fsae117 article EN cc-by ICES Journal of Marine Science 2024-09-03

<p>The increase in anthropogenic induced warming over the last two centuries is impacting marine environments. Marine planktic calcifying organisms interact sensitively to changes sea surface temperatures (SST), and food web structure. Here, we study high resolution multicore records from western Mediterranean Sea regions (Alboran Balearic basins), areas highly affected by both natural climate change warming. Cores cover time interval Medieval Climate Anomaly (MCA) present....

10.5194/egusphere-egu21-13653 article EN 2021-03-04
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