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Global Change Biology · 2026 · Vol. 32 · Issue 4 · Wiley
Understanding delayed biodiversity responses to global changes is crucial for anticipating future ecosystem dynamics and informing conservation. Here, we analysed a 32‐year time series of benthic megafauna from the North Sea (Dogger Bank) to assess extinction debt and immigration credit using a probabilistic species pool framework. Within this framework, we generated suitability estimates for both observed diversity (i.e., spe...
Plant and Soil · 2026 · Springer
Background Cereal crops dominate arable agriculture and underpin global food supply. Cereal grain yield is closely related to crop nitrogen (N) uptake. However, excessive inputs of N fertiliser in cereal production systems can have negative environmental consequences and represent high financial risk for farmers. Scope This review explores opportunities to reduce the current reliance of the global staples, wheat ( Triticum aes...
Limnology and Oceanography · 2026 · Vol. 71 · Issue 1 · Wiley
Nitrification is a key process in the aquatic nitrogen (N) cycle, but its products, nitrate (NO 3 − ) and nitrous oxide (N 2 O), contribute to eutrophication and greenhouse gas emissions, particularly in eutrophic lakes. Variations in in‐lake N cycling and N 2 O production pathways, as a function of seasonality and artificial oxygenation, remain poorly understood. We investigated nitrification in the artificially oxygenated eu...
Limnology and Oceanography · 2026 · Vol. 71 · Issue 1 · Wiley
Organotrophic denitrification is an important nitrogen (N) removal process in lakes, but alternative N reduction processes such as lithotrophic sulfur (S)‐oxidizing denitrification may be greatly underappreciated. We studied the redox transition zone (RTZ) in the meromictic water column of the North Basin of Lake Lugano (Switzerland) to characterize N transformation pathways coupled to the S and carbon (C) cycles. Incubations...
Limnology and Oceanography · 2025 · Vol. 70 · Issue 4 · Wiley
Upwelling systems and their associated oxygen deficient zones (ODZs) are hotspots of nitrous oxide (N 2 O) production in the ocean. The Benguela Upwelling System (BUS) is a highly productive region and an important, yet variable source of N 2 O to the atmosphere. This study examined underlying processes and microbial key players governing N 2 O production in the BUS during the austral winter. 15 N‐tracer incubation experiments...
Limnology and Oceanography · 2024 · Vol. 69 · Issue 8 · Wiley
Past changes in the input/output, and internal cycling, of bioavailable nitrogen (N) in marine and lacustrine environments can be reconstructed by analyzing the N isotopic composition (δ 15 N) of organic matter in the sedimentary record. To verify, and eliminate, potential biases of bulk sedimentary δ 15 N (δ 15 N bulk ) signatures by diagenetic alteration and external N inputs, we applied, for the first time, the diatom‐bound...
Global Change Biology · 2024 · Vol. 30 · Issue 1 · Wiley
Warming and eutrophication influence carbon (C) processing in sediments, with implications for the global greenhouse‐gas budget. Temperature effects on sedimentary C loss are well understood, but the mechanism of change in turnover through priming with labile organic matter (OM) is not. Evaluating changes in the magnitude of priming as a function of warming, eutrophication, and OM stoichiometry, we incubated sediments with 13...
Limnology and Oceanography · 2023 · Vol. 68 · Issue 2 · Wiley
Marine oxygen‐deficient zones represent a natural source of nitrous oxide (N 2 O), a potent greenhouse gas and ozone‐depleting agent. To investigate controls on N 2 O production, the responses of ammonia oxidation (AO) to nitrite () and N 2 O with respect to oxygen (O 2 ), ammonium () and concentrations were evaluated using tracer incubations in the Eastern Tropical North Pacific. Within the oxycline, additions of and O 2 stim...
Limnology and Oceanography · 2023 · Vol. 68 · Issue 1 · Wiley
Accumulation of methane in oxic waters of lakes and the ocean has been widely reported. Despite the importance for the greenhouse gas budget, mechanistic controls of such “methane paradox” remain elusive. Here, we use a combination of CH 4 concentration and isotopic (δ 13 C CH4 , δD H2O and δ 18 O H2O ) measurements, plankton incubations and microbial community assessments to demonstrate the existence of the methane paradox in...
The Journal of Membrane Biology · 2022 · Vol. 255 · Issue 4-5 · Springer
We studied the transleaflet coupling of compositionally asymmetric liposomes in the fluid phase. The vesicles were produced by cyclodextrin-mediated lipid exchange and contained dipalmitoyl phosphatidylcholine (DPPC) in the inner leaflet and different mixed-chain phosphatidylcholines (PCs) as well as milk sphingomyelin (MSM) in the outer leaflet. In order to jointly analyze the obtained small-angle neutron and X-ray scattering...
Limnology and Oceanography · 2022 · Vol. 67 · Issue 8 · Wiley
Lakes can be important sources of the potent greenhouse gas nitrous oxide (N 2 O) to the atmosphere, but to what extent abiotic processes may contribute to lacustrine N 2 O production remains uncertain. We assessed pathways of N 2 O production and reduction in the water column of meromictic and iron‐rich Lake La Cruz, Spain, including chemodenitrification‐induced N 2 O formation via the reaction of reactive nitrogen (N) (e.g.,...
Limnology and Oceanography · 2021 · Vol. 66 · Issue 12 · Wiley
Daphne Donis; Evanthia Mantzouki; Daniel F. McGinnis; Dominic Vachon; Irene Gallego; Hans‐Peter Grossart; Lisette N. de Senerpont Domis; Sven Teurlincx; Laura Seelen; Miquel Lürling; Yvon Verstijnen; Valentini Maliaka; Jeremy Fonvielle; Petra M. Visser; Jolanda Verspagen; Maria van Herk; Maria G. Antoniou; Nikoletta Tsiarta; Valerie McCarthy; Victor C. Perello; Danielle Machado‐Vieira; Alinne Gurjão de Oliveira; Dubravka Špoljarić Maronić; Filip Stević; Tanja Žuna Pfeiffer; Itana Bokan Vucelić; Petar Žutinić; Marija Gligora Udovič; Anđelka Plenković‐Moraj; Luděk Bláha; Rodan Geriš; Markéta Fránková; Kirsten Seestern Christoffersen; Trine Perlt Warming; Tõnu Feldmann; Alo Laas; Kristel Panksep; Lea Tuvikene; Kersti Kangro; Judita Koreivienė; Jūratė Karosienė; Jūratė Kasperovičienė; Ksenija Savadova‐Ratkus; Irma Vitonytė; Kerstin Häggqvist; Pauliina Salmi; Lauri Arvola; Karl Rothhaupt; Christos Avagianos; Triantafyllos Kaloudis; Spyros Gkelis; Manthos Panou; Theodoros Triantis; Sevasti‐Kiriaki Zervou; Anastasia Hiskia; Ulrike Obertegger; Adriano Boscaini; Giovanna Flaim; Nico Salmaso; Leonardo Cerasino; Sigrid Haande; Birger Skjelbred; Magdalena Grabowska; Maciej Karpowicz; Damian Chmura; Lidia Nawrocka; Justyna Kobos; Hanna Mazur‐Marzec; Pablo Alcaraz‐Párraga; Elżbieta Wilk‐Woźniak; Wojciech Krztoń; Edward Walusiak; Ilona Gagala‐Borowska; Joana Mankiewicz‐Boczek; Magdalena Toporowska; Barbara Pawlik‐Skowronska; Michał Niedźwiecki; Wojciech Pęczuła; Agnieszka Napiórkowska‐Krzebietke; Julita Dunalska; Justyna Sieńska; Daniel Szymański; Marek Kruk; Agnieszka Budzyńska; Ryszard Goldyn; Anna Kozak; Joanna Rosińska; Elżbieta Szeląg‐Wasielewska; Piotr Domek; Natalia Jakubowska‐Krepska; Kinga Kwasizur; Beata Messyasz; Aleksandra Pełechata; Mariusz Pełechaty; Mikolaj Kokocinski; Beata Madrecka‐Witkowska; Iwona Kostrzewska‐Szlakowska; Magdalena Frąk; Agnieszka Bańkowska‐Sobczak; Michał Wasilewicz; Agnieszka Ochocka; Agnieszka Pasztaleniec; Iwona Jasser; Ana M. Antão‐Geraldes; Manel Leira; Vitor Vasconcelos; Joao Morais; Micaela Vale; Pedro M. Raposeiro; Vítor Gonçalves; Boris Aleksovski; Svetislav Krstić; Hana Nemova; Iveta Drastichova; Lucia Chomova; Spela Remec‐Rekar; Tina Elersek; Lars‐Anders Hansson; Pablo Urrutia‐Cordero; Andrea G. Bravo; Moritz Buck; William Colom‐Montero; Kristiina Mustonen; Don Pierson; Yang Yang; Jessica Richardson; Christine Edwards; Hannah Cromie; Jordi Delgado‐Martín; David García; Jose Luís Cereijo; Joan Gomà; Mari Carmen Trapote; Teresa Vegas‐Vilarrúbia; Biel Obrador; Ana García‐Murcia; Monserrat Real; Elvira Romans; Jordi Noguero‐Ribes; David Parreño Duque; Elísabeth Fernández‐Morán; Bárbara Úbeda; José Ángel Gálvez; Núria Catalán; Carmen Pérez‐Martínez; Eloísa Ramos‐Rodríguez; Carmen Cillero‐Castro; Enrique Moreno‐Ostos; José María Blanco; Valeriano Rodríguez; Jorge Juan Montes‐Pérez; Roberto L. Palomino; Estela Rodríguez‐Pérez; Armand Hernández; Rafael Carballeira; Antonio Camacho; Antonio Picazo; Carlos Rochera; Anna C. Santamans; Carmen Ferriol; Susana Romo; Juan Miguel Soria; Arda Özen; Tünay Karan; Nilsun Demir; Meryem Beklioğlu; Nur Filiz; Eti Levi; Uğur Iskin; Gizem Bezirci; Ülkü Nihan Tavşanoğlu; Kemal Çelik; Koray Ozhan; Nusret Karakaya; Mehmet Ali Turan Koçer; Mete Yilmaz; Faruk Maraşlıoğlu; Özden Fakioglu; Elif Neyran Soylu; Meral Apaydın Yağcı; Şakir Çınar; Kadir Çapkın; Abdulkadir Yağcı; Mehmet Cesur; Fuat Bilgin; Cafer Bulut; Rahmi Uysal; Köker Latife; Reyhan Akçaalan; Meriç Albay; Mehmet Tahir Alp; Korhan Özkan; Tuğba Ongun Sevindik; Hatice Tunca; Burçin Önem; Hans Paerl; Cayelan C. Carey; Bastiaan W. Ibelings
To determine the drivers of phytoplankton biomass, we collected standardized morphometric, physical, and biological data in 230 lakes across the Mediterranean, Continental, and Boreal climatic zones of the European continent. Multilinear regression models tested on this snapshot of mostly eutrophic lakes (median total phosphorus [TP] = 0.06 and total nitrogen [TN] = 0.7 mg L −1 ), and its subsets (2 depth types and 3 climatic...
Cell and Tissue Research · 2021 · Vol. 385 · Issue 2 · Springer
Proteases play a central role in regulating renal pathophysiology and are increasingly evaluated as actionable drug targets. Here, we review the role of proteolytic systems in inflammatory kidney disease. Inflammatory kidney diseases are associated with broad dysregulations of extracellular and intracellular proteolysis. As an example of a proteolytic system, the complement system plays a significant role in glomerular inflamm...