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1. Elevated boron in cod otoliths from the low-salinity Åland Sea: A unique marker for a new population in the Baltic Sea?

   https://doi.org/10.1093/mcfafs/vtaf022  

   Heimbrand, Yvette; Limburg, Karin E (July 2025, Marine and Coastal Fisheries)

   ABSTRACT ObjectiveThe purpose of this study was to understand the possible provenance of a unique population of Atlantic Cod Gadus morhua that is found in the low-salinity Åland Sea region of the northern Baltic Sea. This population consists of large, healthy individuals, in contrast to the Atlantic Cod in the rest of the Baltic Sea. MethodsWe used laser ablation inductively coupled plasma mass spectrometry to measure levels of boron (as B:Ca) in the otoliths of Atlantic Cod in regions throughout the Baltic Sea. We examined both lifetime chronologies and concentrations in the core region that corresponds to birth and early life. ResultsWe found that B:Ca concentrations were 31 to 348 times higher in the otoliths of cod that occupy the Åland Sea, including in the core region. These concentrations were much higher than expected given that boron is linearly, positively proportional to salinity, which is higher in the southern Baltic Sea, and other populations displayed very low concentrations by comparison. ConclusionsBased on the otolith B:Ca as a unique marker, we suggest that the cod that are sampled in the Åland Sea may be a separate population from those that inhabit the rest of the Baltic Sea. This would not prevent it from mixing with other populations but could point to a separate spawning area. The source of the elevated boron is currently unknown, but the widespread occurrence in cod otoliths from the Åland Sea indicates an extensive nonpoint source. 

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2. Holocene Spatiotemporal Redox Variations in the Southern Baltic Sea

   https://doi.org/10.3389/feart.2021.671401  

   Hardisty, Dalton S.; Riedinger, Natascha; Planavsky, Noah J.; Asael, Dan; Bates, Steven M.; Lyons, Timothy W. (May 2021, Frontiers in Earth Science)

   null (Ed.)

   Low oxygen conditions in the modern Baltic Sea are exacerbated by human activities; however, anoxic conditions also prevailed naturally over the Holocene. Few studies have characterized the specific paleoredox conditions (manganous, ferruginous, euxinic) and their frequency in southern Baltic sub-basins during these ancient events. Here, we apply a suite of isotope systems (Fe, Mo, S) and associated elemental proxies (e.g., Fe speciation, Mn) to specifically define water column redox regimes through the Baltic Holocene in a sill-proximal to sill-distal transect (Lille Belt, Bornholm Basin, Landsort Deep) using samples collected during the Integrated Ocean Drilling Program Expedition 347. At the sill-proximal Lille Belt, there is evidence for anoxic manganous/ferruginous conditions for most of the cored interval following the transition from the Ancylus Lake to Littorina Sea but with no clear excursion to more reducing or euxinic conditions associated with the Holocene Thermal Maximum (HTM) or Medieval Climate Anomaly (MCA) events. At the sill-distal southern sub-basin, Bornholm Basin, a combination of Fe speciation, pore water Fe, and solid phase Mo concentration and isotope data point to manganous/ferruginous conditions during the Ancylus Lake-to-Littorina Sea transition and HTM but with only brief excursions to intermittently or weakly euxinic conditions during this interval. At the western Baltic Proper sub-basin, Landsort Deep, new Fe and S isotope data bolster previous Mo isotope records and Fe speciation evidence for two distinct anoxic periods but also suggest that sulfide accumulation beyond transient levels was largely restricted to the sediment-water interface. Ultimately, the combined data from all three locations indicate that Fe enrichments typically indicative of euxinia may be best explained by Fe deposition as oxides following events likely analogous to the periodic incursions of oxygenated North Sea waters observed today, with subsequent pyrite formation in sulfidic pore waters. Additionally, the Mo isotope data from multiple Baltic Sea southern basins argue against restricted and widespread euxinic conditions, as has been demonstrated in the Baltic Proper and Bothnian Sea during the HTM or MCA. Instead, similar to today, each past Baltic anoxic event is characterized by redox conditions that become progressively more reducing with increasing distance from the sill. 

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3. Comparison of biological and ecological long-term trends related to northern hemisphere climate in different marine ecosystems

   https://doi.org/10.3897/natureconservation.34.30209  

   Kröncke, Ingrid; Neumann, Hermann; Dippner, Joachim W.; Holbrook, Sally; Lamy, Thomas; Miller, Robert; Padedda, Bachisio Mario; Pulina, Silvia; Reed, Daniel C.; Reinikainen, Marko; et al (May 2019, Nature Conservation)

   Data from five sites of the International Long Term Ecological Research (ILTER) network in the North-Eastern Pacific, Western Arctic Ocean, Northern Baltic Sea, South-Eastern North Sea and in the Western Mediterranean Sea were analyzed by dynamic factor analysis (DFA) to trace common multi-year trends in abundance and composition of phytoplankton, benthic fauna and temperate reef fish. Multiannual trends were related to climate and environmental variables to study interactions. Two common trends in biological responses were detected, with temperature and climate indices as explanatory variables in four of the five LTER sites considered. Only one trend was observed at the fifth site, the Northern Baltic Sea, where no explanatory variables were identified. Our findings revealed quasi-synchronous biological shifts in the different marine ecosystems coincident with the 2000 climatic regime shift and provided evidence on a possible further biological shift around 2010. The observed biological modifications were coupled with abrupt or continuous increase in sea water and air temperature confirming the key-role of temperature in structuring marine communities. 

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4. Changes in population depth distribution and oxygen stratification are involved in the current low condition of the eastern Baltic Sea cod (<i>Gadus morhua</i>)

   https://doi.org/10.5194/bg-18-1321-2021  

   Casini, Michele; Hansson, Martin; Orio, Alessandro; Limburg, Karin (January 2021, Biogeosciences)

   null (Ed.)

   Abstract. During the past 20 years, hypoxic areas have expanded rapidly in theBaltic Sea, which has become one of the largest marine “dead zones” in theworld. At the same time, the most important commercial fish population ofthe region, the eastern Baltic cod, has experienced a drastic reduction inmean body condition, but the processes behind the relation betweendeoxygenation and condition remain elusive. Here we use extensive long-termmonitoring data on cod biology and distribution as well as on hydrologicalvariations to investigate the processes that relate deoxygenation and codcondition during the autumn season. Our results show that the depthdistribution of cod has increased during the past 4 decades at the sametime of the expansion, and shallowing, of waters with oxygen concentrationsdetrimental to cod performance. This has resulted in a progressivelyincreasing spatial overlap between the cod population and low-oxygenatedwaters after the mid-1990s. This spatial overlap and the actual oxygenconcentration experienced by cod therein statistically explained a largeproportion of the changes in cod condition over the years. These resultscomplement previous analyses on fish otolith microchemistry that alsorevealed that since the mid-1990s, cod individuals with low condition wereexposed to low-oxygen waters during their life. This study helps to shedlight on the processes that have led to a decline of the eastern Baltic codbody condition, which can aid the management of this population currently indistress. Further studies should focus on understanding why the codpopulation has moved to deeper waters in autumn and on analyzing the overlapwith low-oxygen waters in other seasons to quantify the potential effects ofthe variations in physical properties on cod biology throughout the year. 

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5. Extracellular superoxide production by key microbes in the global ocean

   https://doi.org/10.1002/lno.11247  

   Sutherland, Kevin M.; Coe, Allison; Gast, Rebecca J.; Plummer, Sydney; Suffridge, Christopher P.; Diaz, Julia M.; Bowman, Jeff S.; Wankel, Scott D.; Hansel, Colleen M. (July 2019, Limnology and Oceanography)

   ABSTRACT Bacteria and eukaryotes produce the reactive oxygen species superoxide both within and outside the cell. Although superoxide is typically associated with the detrimental and sometimes fatal effects of oxidative stress, it has also been shown to be involved in a range of essential biochemical processes, including cell signaling, growth, differentiation, and defense. Light‐independent extracellular superoxide production has been shown to be widespread among many marine heterotrophs and phytoplankton, but the extent to which this trait is relevant to marine microbial physiology and ecology throughout the global ocean is unknown. Here, we investigate the dark extracellular superoxide production of five groups of organisms that are geographically widespread and represent some of the most abundant organisms in the global ocean. These includeProchlorococcus,Synechococcus,Pelagibacter,Phaeocystis, andGeminigera. Cell‐normalized net extracellular superoxide production rates ranged seven orders of magnitude, from undetectable to 14,830 amol cell⁻¹h⁻¹, with the cyanobacteriumProchlorococcusbeing the lowest producer and the cryptophyteGeminigerabeing the most prolific producer. Extracellular superoxide production exhibited a strong inverse relationship with cell number, pointing to a potential role in cell signaling. We demonstrate that rapid, cell‐number–dependent changes in the net superoxide production rate bySynechococcusandPelagibacterarose primarily from changes in gross production of extracellular superoxide, not decay. These results expand the relevance of dark extracellular superoxide production to key marine microbes of the global ocean, suggesting that superoxide production in marine waters is regulated by a diverse suite of marine organisms in both dark and sunlit waters. 

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