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  • 1
    Publikationsdatum: 2024-05-14
    Beschreibung: The thermokarst lakes of permafrost regions play a major role in the global carbon cycle. These lakes are sources of methane to the atmosphere although the methane flux is restricted by an ice cover for most of the year. How methane concentrations and fluxes in these waters are affected by the presence of an ice cover is poorly understood. To relate water body morphology, ice formation and methane to each other, we studied the ice of three different water bodies in locations typical of the transition of permafrost from land to ocean in a continuous permafrost coastal region in Siberia. In total, 11 ice cores were analyzed as records of the freezing process and methane composition during the winter season. The three water bodies differed in terms of connectivity to the sea, which affected fall freezing. The first was a bay underlain by submarine permafrost (Tiksi Bay, BY), the second a shallow thermokarst lagoon cut off from the sea in winter (Polar Fox Lagoon, LG) and the third a land-locked freshwater thermokarst lake (Goltsovoye Lake, LK). Ice on all water bodies was mostly methane-supersaturated with respect to atmospheric equilibrium concentration, except for three cores from the isolated lake. In the isolated thermokarst lake, ebullition from actively thawing basin slopes resulted in the localized integration of methane into winter ice. Stable δ13C-CH4 isotope signatures indicated that methane in the lagoon ice was oxidized to concentrations close to or below the calculated atmospheric equilibrium concentration. Increasing salinity during winter freezing led to a micro-environment on the lower ice surface where methane oxidation occurred and the lagoon ice functioned as a methane sink. In contrast, the ice of the coastal marine environment was slightly supersaturated with methane, consistent with the brackish water below. Our interdisciplinary process study shows how water body morphology affects ice formation which mitigates methane fluxes to the atmosphere.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2024-05-14
    Beschreibung: Here we provide particle size and biovolume distribution data from an Underwater Vision Profiler 6, mounted on a BGC Argo Float with the WMO number 6903095. The float was deployed in a cyclonic eddy off Cape Columbine, South Africa on the 13 April 2021 close to the eddy center at 33.07 degree South, 13.89 degree East. Parking depth was set at 300 m and profiling depth initially to 600 m and later increased to 1000 m depth to maintain the float in the eddy. Profiling frequency was every three days. It stayed within this eddy for about five months and then operated East and Southeast of South Africa until it was deliberately picked up on the 17 September 2022 at 34.43 degrees South and 10.21 degrees East.
    Schlagwort(e): 0000a_WMO6903095; 0000p_WMO6903095; 0001a_WMO6903095; 0001p_WMO6903095; 0002a_WMO6903095; 0002p_WMO6903095; 0003a_WMO6903095; 0003p_WMO6903095; 0004a_WMO6903095; 0004p_WMO6903095; 0005a_WMO6903095; 0005p_WMO6903095; 0006a_WMO6903095; 0006p_WMO6903095; 0007a_WMO6903095; 0007p_WMO6903095; 0008a_WMO6903095; 0008p_WMO6903095; 0009a_WMO6903095; 0009p_WMO6903095; 0010a_WMO6903095; 0010p_WMO6903095; 0011a_WMO6903095; 0011p_WMO6903095; 0012a_WMO6903095; 0012p_WMO6903095; 0013a_WMO6903095; 0013p_WMO6903095; 0014a_WMO6903095; 0014p_WMO6903095; 0015a_WMO6903095; 0015p_WMO6903095; 0016a_WMO6903095; 0016p_WMO6903095; 0017a_WMO6903095; 0017p_WMO6903095; 0018a_WMO6903095; 0018p_WMO6903095; 0019a_WMO6903095; 0019p_WMO6903095; 0020a_WMO6903095; 0020p_WMO6903095; 0021a_WMO6903095; 0021p_WMO6903095; 0022a_WMO6903095; 0022p_WMO6903095; 0023a_WMO6903095; 0023p_WMO6903095; 0024a_WMO6903095; 0024p_WMO6903095; 0025a_WMO6903095; 0025p_WMO6903095; 0026a_WMO6903095; 0026p_WMO6903095; 0027a_WMO6903095; 0027p_WMO6903095; 0028a_WMO6903095; 0028p_WMO6903095; 0029a_WMO6903095; 0029p_WMO6903095; 0030a_WMO6903095; 0030p_WMO6903095; 0031a_WMO6903095; 0031p_WMO6903095; 0032a_WMO6903095; 0032p_WMO6903095; 0033a_WMO6903095; 0033p_WMO6903095; 0034a_WMO6903095; 0034p_WMO6903095; 0035a_WMO6903095; 0035p_WMO6903095; 0036a_WMO6903095; 0036p_WMO6903095; 0037a_WMO6903095; 0037p_WMO6903095; 0038a_WMO6903095; 0038p_WMO6903095; 0039a_WMO6903095; 0039p_WMO6903095; 0040a_WMO6903095; 0040p_WMO6903095; 0041a_WMO6903095; 0041p_WMO6903095; 0042a_WMO6903095; 0042p_WMO6903095; 0043a_WMO6903095; 0043p_WMO6903095; 0044a_WMO6903095; 0044p_WMO6903095; 0045a_WMO6903095; 0045p_WMO6903095; 0046a_WMO6903095; 0046p_WMO6903095; 0047a_WMO6903095; 0047p_WMO6903095; 0048a_WMO6903095; 0048p_WMO6903095; 0049a_WMO6903095; 0049p_WMO6903095; 0050a_WMO6903095; 0050p_WMO6903095; 0051a_WMO6903095; 0051p_WMO6903095; 0052a_WMO6903095; 0052p_WMO6903095; 0053a_WMO6903095; 0053p_WMO6903095; 0054a_WMO6903095; 0054p_WMO6903095; 0055a_WMO6903095; 0055p_WMO6903095; 0056a_WMO6903095; 0056p_WMO6903095; 0057a_WMO6903095; 0057p_WMO6903095; 0058a_WMO6903095; 0058p_WMO6903095; 0059a_WMO6903095; 0059p_WMO6903095; 0060a_WMO6903095; 0060p_WMO6903095; 0061a_WMO6903095; 0061p_WMO6903095; 0062a_WMO6903095; 0062p_WMO6903095; 0063a_WMO6903095; 0063p_WMO6903095; 0064a_WMO6903095; 0064p_WMO6903095; 0065a_WMO6903095; 0065p_WMO6903095; 0066a_WMO6903095; 0066p_WMO6903095; 0067a_WMO6903095; 0067p_WMO6903095; 0068a_WMO6903095; 0068p_WMO6903095; 0069a_WMO6903095; 0069p_WMO6903095; 0070a_WMO6903095; 0070p_WMO6903095; 0071a_WMO6903095; 0071p_WMO6903095; 0072a_WMO6903095; 0072p_WMO6903095; 0073a_WMO6903095; 0073p_WMO6903095; 0074a_WMO6903095; 0074p_WMO6903095; 0075a_WMO6903095; 0075p_WMO6903095; 0076a_WMO6903095; 0076p_WMO6903095; 0077a_WMO6903095; 0077p_WMO6903095; 0078a_WMO6903095; 0078p_WMO6903095; 0079a_WMO6903095; 0079p_WMO6903095; 0080a_WMO6903095; 0080p_WMO6903095; 0081a_WMO6903095; 0081p_WMO6903095; 0082a_WMO6903095; 0082p_WMO6903095; 0083a_WMO6903095; 0083p_WMO6903095; 0084a_WMO6903095; 0084p_WMO6903095; 0085a_WMO6903095; 0085p_WMO6903095; 0086a_WMO6903095; 0086p_WMO6903095; 0087a_WMO6903095; 0087p_WMO6903095; 0088a_WMO6903095; 0088p_WMO6903095; 0089a_WMO6903095; 0089p_WMO6903095; 0090a_WMO6903095; 0090p_WMO6903095; 0091a_WMO6903095; 0091p_WMO6903095; 0092a_WMO6903095; 0092p_WMO6903095; 0093a_WMO6903095; 0093p_WMO6903095; 0094a_WMO6903095; 0094p_WMO6903095; 0095a_WMO6903095; 0095p_WMO6903095; 0096a_WMO6903095; 0096p_WMO6903095; 0097a_WMO6903095; 0097p_WMO6903095; 0098a_WMO6903095; 0098p_WMO6903095; 0099a_WMO6903095; 0099p_WMO6903095; 0100a_WMO6903095; 0100p_WMO6903095; 0101a_WMO6903095; 0101p_WMO6903095; 0102a_WMO6903095; 0102p_WMO6903095; 0103a_WMO6903095; 0103p_WMO6903095; 0104a_WMO6903095; 0104p_WMO6903095; 0105a_WMO6903095; 0105p_WMO6903095; 0106a_WMO6903095; 0106p_WMO6903095; 0107a_WMO6903095; 0107p_WMO6903095; 0108a_WMO6903095; 0108p_WMO6903095; 0109a_WMO6903095; 0109p_WMO6903095; 0110a_WMO6903095; 0110p_WMO6903095; 0111a_WMO6903095; 0111p_WMO6903095; 0112a_WMO6903095; 0112p_WMO6903095; 0113a_WMO6903095; 0113p_WMO6903095; 0114a_WMO6903095; 0114p_WMO6903095; 0115a_WMO6903095; 0115p_WMO6903095; 0116a_WMO6903095; 0116p_WMO6903095; 0117a_WMO6903095; 0117p_WMO6903095; 0118a_WMO6903095; 0118p_WMO6903095; 0119a_WMO6903095; 0119p_WMO6903095; 0120a_WMO6903095; 0120p_WMO6903095; 0121a_WMO6903095; 0121p_WMO6903095; 0122a_WMO6903095; 0122p_WMO6903095; 0123a_WMO6903095; 0123p_WMO6903095; 0124a_WMO6903095; 0124p_WMO6903095; 0125a_WMO6903095; 0125p_WMO6903095; 0126a_WMO6903095; 0126p_WMO6903095; 0127a_WMO6903095; 0127p_WMO6903095; 0128a_WMO6903095; 0128p_WMO6903095; 0129a_WMO6903095; 0129p_WMO6903095; 0130a_WMO6903095; 0130p_WMO6903095; 0131a_WMO6903095; 0131p_WMO6903095; 0132a_WMO6903095; 0132p_WMO6903095; 0133a_WMO6903095; 0133p_WMO6903095; 0134a_WMO6903095; 0134p_WMO6903095; 0135a_WMO6903095; 0135p_WMO6903095; 0136a_WMO6903095; 0136p_WMO6903095; 0137a_WMO6903095; 0137p_WMO6903095; 0138a_WMO6903095; 0138p_WMO6903095; 0139a_WMO6903095; 0139p_WMO6903095; 0140a_WMO6903095; 0140p_WMO6903095; 0141a_WMO6903095; 0141p_WMO6903095; 0142a_WMO6903095; 0142p_WMO6903095; 0143a_WMO6903095; 0143p_WMO6903095; 0144a_WMO6903095; 0144p_WMO6903095; 0145a_WMO6903095; 0145p_WMO6903095; 0146a_WMO6903095; 0146p_WMO6903095; 0147a_WMO6903095; 0147p_WMO6903095; 0148a_WMO6903095; 0148p_WMO6903095; 0149a_WMO6903095; 0149p_WMO6903095; 0150a_WMO6903095; 0150p_WMO6903095; 0151a_WMO6903095; 0151p_WMO6903095; 0152a_WMO6903095; 0152p_WMO6903095; 0153a_WMO6903095; 0153p_WMO6903095; 0154a_WMO6903095; 0154p_WMO6903095; 0155a_WMO6903095; 0155p_WMO6903095; 0156a_WMO6903095; 0156p_WMO6903095; 0157a_WMO6903095; 0157p_WMO6903095; 0158a_WMO6903095; 0158p_WMO6903095; 0159a_WMO6903095; 0159p_WMO6903095; 0160a_WMO6903095; 0160p_WMO6903095; 0161a_WMO6903095; 0161p_WMO6903095; 0162a_WMO6903095; 0162p_WMO6903095; 0163a_WMO6903095; 0163p_WMO6903095; 0164a_WMO6903095; 0164p_WMO6903095; 0165a_WMO6903095; 0165p_WMO6903095; 0166a_WMO6903095; 0166p_WMO6903095; 0167a_WMO6903095; 0167p_WMO6903095; 0168a_WMO6903095; 0168p_WMO6903095; 0169a_WMO6903095; 0169p_WMO6903095; 0170a_WMO6903095; 0170p_WMO6903095; 0171a_WMO6903095; 0171p_WMO6903095; 0172a_WMO6903095; 0172p_WMO6903095; 0173a_WMO6903095; 0173p_WMO6903095; 0174a_WMO6903095; 0174p_WMO6903095; 0175a_WMO6903095; 0175p_WMO6903095; 0176a_WMO6903095; 0176p_WMO6903095; 0177a_WMO6903095; 0177p_WMO6903095; 0178a_WMO6903095; 0178p_WMO6903095; 0179a_WMO6903095; 0179p_WMO6903095; 0180a_WMO6903095; 0180p_WMO6903095; 0181a_WMO6903095; 0181p_WMO6903095; 0182a_WMO6903095; 0182p_WMO6903095; 0183a_WMO6903095; 0183p_WMO6903095; ARGOFL; Argo float; Biovolume; DATE/TIME; Event label; in situ imaging; LATITUDE; LONGITUDE; MOPGA-TAD; Particle concentration, fractionated; particle distribution; Pressure, water; Sample code/label; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management; Tropical Atlantic Deoxygenation: gateway dynamics, feedback mechanisms and ecosystem impacts; Volume
    Materialart: Dataset
    Format: text/tab-separated-values, 2518238 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2024-05-13
    Beschreibung: This paper positions possibilities for human geographies of the sea. The growing volume of work under this banner has been largely qualitative in its approach, reflecting, in turn, the questions posed by oceanic scholars. These questions necessitate corresponding methods. Whilst this is not necessarily a problem, and the current corpus of work has offered many significant contributions, in making sense of the human dimensions of maritime worlds, other questions—and methods—may generate knowledge that is useful within this remit of work. This paper considers the place of quantitative approaches in posing lines of enquiry about shipping, one of the prominent areas of concern under the banner of ‘human geographies of the seas’. There is longstanding work in transport geographies concerned with shipping, logistics, freight movement and global connections, which embraces quantitative methods which could be bridged to ask fresh questions about oceanic spatial phenomena past and present. This paper reviews the state of the art of human geographies of the sea and transport geographies and navigates how the former field may be stimulated by some of the interests of the latter and a broader range of questions about society-sea-space relations. The paper focuses on Automatic Identification Systems (or AIS) as a potentially useful tool for connecting debates, and deepening spatial understandings of the seas and shipping beyond current scholarship. To advance the argument the example of shipping layups is used to illustrate or rather, position, the point.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , peerRev
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
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    Unbekannt
    COMPANY OF BIOLOGISTS LTD
    In:  EPIC3Journal of Experimental Biology, COMPANY OF BIOLOGISTS LTD, 217(14), pp. 2555-2568, ISSN: 0022-0949
    Publikationsdatum: 2024-05-13
    Beschreibung: The jumbo squid, Dosidicus gigas, can survive extended forays into the oxygen minimum zone (OMZ) of the Eastern Pacific Ocean. Previous studies have demonstrated reduced oxygen consumption and a limited anaerobic contribution to ATP production, suggesting the capacity for substantial metabolic suppression during hypoxic exposure. Here, we provide a more complete description of energy metabolism and explore the expression of proteins indicative of transcriptional and translational arrest that may contribute to metabolic suppression. We demonstrate a suppression of total ATP demand under hypoxic conditions (1% oxygen, PO2=0.8 kPa) in both juveniles (52%) and adults (35%) of the jumbo squid. Oxygen consumption rates are reduced to 20% under hypoxia relative to air-saturated controls. Concentrations of arginine phosphate (Arg-P) and ATP declined initially, reaching a new steady state (~30% of controls) after the first hour of hypoxic exposure. Octopine began accumulating after the first hour of hypoxic exposure, once Arg-P breakdown resulted in sufficient free arginine for substrate. Octopine reached levels near 30 mmol g−1 after 3.4 h of hypoxic exposure. Succinate did increase through hypoxia but contributed minimally to total ATP production. Glycogenolysis in mantle muscle presumably serves to maintain muscle functionality and balance energetics during hypoxia. We provide evidence that post-translational modifications on histone proteins and translation factors serve as a primary means of energy conservation and that select components of the stress response are altered in hypoxic squids. Reduced ATP consumption under hypoxia serves to maintain ATP levels, prolong fuel store use and minimize the accumulation of acidic intermediates of anaerobic ATP-generating pathways during prolonged diel forays into the OMZ. Metabolic suppression likely limits active, daytime foraging at depth in the core of the OMZ, but confers an energetic advantage over competitors that must remain in warm, oxygenated surface waters. Moreover, the capacity for metabolic suppression provides habitat flexibility as OMZs expand as a result of climate change.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
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    Unbekannt
    In:  EPIC3ICES/PICES 6th Zooplankton Production Symposium, Bergen, Norway, 2016-05-09-2016-05-13
    Publikationsdatum: 2024-05-13
    Beschreibung: The copepod Calanus finmarchicus is a dominant zooplankter in the north Atlantic and is spreading northward into the Arctic due to ocean warming. The copepods life is characterized by diel vertical migration as well as a seasonal cycle with overwintering in deep waters. Although both phenome have been studied for more than a century, the exact factors controlling these rhythms are still unclear. Molecular techniques have precisely described genetic clockworks in several, mostly terrestrial species and there is clear evidence that clock genes are not only involved in the regulation of diel 24h rhythms, but can also play an important role in the synchronisation (entrainment) of the seasonal cycle. We present first records of clock gene expression in Calanus finmarchicus from Kongsfjorden, Svalbard and compare gene activity between specimen in the early and late phase of overwintering. Copepods were sampled from overwintering depth (〉220 m) in September 2014 when day length was about 10 hours and during polar night in January 2015. The results show clear 24h oscillations in most genes for September, whereas gene expression is generally lower and almost completely arrhythmic during the polar night. The results strongly point towards the existence of a light-entrained genetic clock in Calanus finmarchicus. As the regulators of seasonal timing in this species are still unclear, understanding the mechanism of the clock could help assessing the adaptability of this boreal species to the strongly fluctuating light conditions at high latitudes. This could be crucial in predicting future seasonal mismatches and ecosystem consequences.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
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    Unbekannt
    In:  EPIC3Time and Light: Novel Concepts and Models in Sensory and Chronobiology, Vienna, Austria, 2016-05-08-2016-05-10
    Publikationsdatum: 2024-05-13
    Beschreibung: The copepod Calanus finmarchicus plays a crucial role in the north Atlantic food web, channelling energy from phytoplankton primary production to higher trophic levels including commercially important fish stocks like herring and cod. The copepod species is spreading northward into the Arctic due to ocean warming. The activity phase of C. finmarchicus in spring/summer is characterized by diel vertical migration, meaning that the animals migrate to surface waters around sunset to feed, and back to deeper layers around sunrise to hide from visual predators. This rhythmic vertical migration behaviour is characteristic for zooplankton communities all around the world. At the end of the activity phase in autumn, C. finmarchicus enters an overwintering mode and inactively dwell in deep waters until next spring when it starts a new generation cycle. Although both rhythms (diel and seasonal) have been studied for more than a century, the exact factors controlling them are still unclear. Molecular techniques have precisely described genetic clockworks in numerous species and there is clear evidence that clock genes are not only involved in the regulation of diel 24h rhythms, but also in the entrainment of the seasonal cycle. We present first records of clock gene expression in Calanus finmarchicus from a high Arctic fjord in Svalbard at 79°N and compare gene activity between specimen in the early and late phase of overwintering. Copepods were sampled from overwintering depth (〉220 m) in September 2014 when surface photoperiod was about 10 hours and during polar night in January 2015 when no light was present. Samples were analysed by quantitative real-time PCR (qRT-PCR) using custom designed Taqman® low-density array cards. The results show clear 24h oscillations in most genes for September, whereas gene expression is almost completely arrhythmic during the polar night in January. It furthermore appears that in September most of the investigated clock genes show distinct expressions patterns, which often match pattern previously observed in other (model) species. For example, expression of period (1 & 2) is highest around sunset (per1) or early night (per2) whereas activity of clock sharply increases around sunrise and peaks in the afternoon. Expression of cryptochrome 1 is highest around midnight while expression of cryptochrome 2 shows patterns similar to those of the period genes. The results strongly point towards the existence of a light-entrained genetic clock in Calanus finmarchicus that becomes arrhythmic during the constant darkness of the polar night. Our work presents an example on how the vast mechanistic knowledge about endogenous timekeeping gained from model organisms can be transferred to field studies on non-model species of high ecological relevance.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
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    Unbekannt
    INTER-RESEARCH
    In:  EPIC3Marine Ecology-Progress Series, INTER-RESEARCH, 603, pp. 79-92, ISSN: 0171-8630
    Publikationsdatum: 2024-05-13
    Beschreibung: Changing environmental conditions cause poleward distribution shifts in many marine organisms including the northern Atlantic key zooplankton species Calanus finmarchicus. The copepod has diel cycles of vertical migration and feeding, a seasonal life cycle with diapause in winter and a functioning circadian clock. Endogenous clock mechanisms control various aspects of rhythmic life and are heavily influenced by environmental light conditions. Here we explore how the extreme seasonal change in photoperiod (day length) in a high Arctic fjord affects circadian clock functioning as well as diel and seasonal cycles in C. finmarchicus. Expression of clock genes was measured in the active life phase at the end of midnight sun, in early diapause when photoperiod was ~12 h, and in late diapause during the polar night. While the clock maintained diel rhythmicity under extremely long photoperiods, it became arrhythmic during diapause. This was probably not due to a lack of light but was related to the physiological state of diapause. Seasonal expression analyses of 35 genes show distinct patterns for each investigated life phase. C. finmarchicus is able to maintain diel clock rhythmicity at photoperiods close to 24 h, and it is discussed how this may be related to the nature of the marine environment. The work also evaluates the potential negative consequences of rigid clock-based seasonal timing in a polar environment exposed to climate change and with high interannual variability.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
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    Unbekannt
    CELL PRESS
    In:  EPIC3Current Biology, CELL PRESS, 27(14), pp. 2194-2201, ISSN: 0960-9822
    Publikationsdatum: 2024-05-13
    Beschreibung: Biological clocks are a ubiquitous ancient and adaptive mechanism enabling organisms to anticipate environmental cycles and to regulate behavioral and physiological processes accordingly [1]. Although terrestrial circadian clocks are well understood, knowledge of clocks in marine organisms is still very limited [2–5]. This is particularly true for abundant species displaying large-scale rhythms like diel vertical migration (DVM) that contribute significantly to shaping their respective ecosystems [6]. Here we describe exogenous cycles and endogenous rhythms associated with DVM of the ecologically important and highly abundant planktic copepod Calanus finmarchicus. In the laboratory, C. finmarchicus shows circadian rhythms of DVM, metabolism, and most core circadian clock genes (clock, period1, period2, timeless, cryptochrome2, and clockwork orange). Most of these genes also cycle in animals assessed in the wild, though expression is less rhythmic at depth (50–140 m) relative to shallow-caught animals (0–50 m). Further, peak expressions of clock genes generally occurred at either sunset or sunrise, coinciding with peak migration times. Including one of the first field investigations of clock genes in a marine species [5, 7], this study couples clock gene measurements with laboratory and field data on DVM. While the mechanistic connection remains elusive, our results imply a high degree of causality between clock gene expression and one of the planet’s largest daily migrations of biomass. We thus suggest that circadian clocks increase zooplankton fitness by optimizing the temporal trade-off between feeding and predator avoidance, especially when environmental drivers are weak or absent [8].
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    Publikationsdatum: 2024-05-13
    Beschreibung: Ocean warming and acidification are two important environmental drivers affecting marine organisms. Organisms living at high latitudes might be especially threatened in near future, as current environmental changes are larger and occur faster. Therefore, we investigated the effect of hypercapnia on thermal tolerance and physiological performance of sub-Arctic Mytilus edulis from the White Sea. Mussels were exposed (2 weeks) to 390 µatm (control) and 1,120 µatm CO2 (year 2100) before respiration rate (MO2), anaerobic metabolite (succinate) level, haemolymph acid-base status, and intracellular pH (pHi) were determined during acute warming (10-28°C, 3°C over night). In normocapnic mussels, warming induced MO2 to rise exponentially until it levelled off beyond a breakpoint temperature of 20.5°C. Concurrently, haemolymph PCO2 rose significantly 〉19°C followed by a decrease in PO2 indicating the pejus temperature (TP, onset of thermal limitation). Succinate started to accumulate at 28°C under normocapnia defining the critical temperature (TC). pHi was maintained during warming until it dropped at 28°C, in line with the concomitant transition to anaerobiosis. At acclimation temperature, CO2 had only a minor impact. During warming, MO2 was stimulated by CO2 resulting in an elevated breakpoint of 25.8°C. Nevertheless, alterations in haemolymph gases (〉16°C) and the concomitant changes of pHi and succinate level (25°C) occurred at lower temperature under hypercapnia versus normocapnia indicating a downward shift of both thermal limits TP and TC by CO2. Compared to temperate conspecifics, sub-Arctic mussels showed an enhanced thermal sensitivity, exacerbated further by hypercapnia, indicating their potential vulnerability to environmental changes projected for 2100.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev , info:eu-repo/semantics/article
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    facet.materialart.
    Unbekannt
    Springer
    In:  EPIC3Polar Night Marine Ecology_ Life and Light in the Dead of Night, Advances in Polar Ecology, Switzerland, Springer, pp. 217-240, ISBN: 978-3-030-33208-2
    Publikationsdatum: 2024-05-13
    Beschreibung: Biological clocks are universal to all living organisms on Earth. Their ubiquity is testament to their importance to life: from cells to organs and from the simplest cyanobacteria to plants and primates, they are central to orchestrating life on this planet. Biological clocks are usually set by the day–night cycle, so what happens in polar regions during the Polar Night or Polar Day when there are periods of 24! hours of darkness or light? How would a biological clock function without a timekeeper!cycle? This chapter details evidence that biological clocks are central to structuring daily and seasonal activities in organisms at high latitudes. Importantly, despite a strongly reduced or absent day–night cycle, biological clocks in the Polar Night still appear to be regulated by background illumination. Here we explore evidence for highly cyclic activity, from behaviour patterns to clock gene expression, in copepods, krill and bivalves. The ultimate goal will be to understand the role of endogenous clocks in driving important daily and seasonal life cycle functions and to determine scope for plasticity in a rapidly changing environment.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Inbook , peerRev
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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