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Diversity and connectivity of deep-sea Amphipoda of the Bering Sea and the Aleutian Trench revealed with DNA barcoding 白令海和阿留申海沟深海两栖动物的多样性和连通性
IF 4.1 3区 地球科学 Q1 OCEANOGRAPHY Pub Date : 2025-12-19 DOI: 10.1016/j.pocean.2025.103655
Anna M. Jażdżewska, Anne Helene S. Tandberg, Wiktor Leszczyński
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引用次数: 0
Ecological and spatial factors shaping abyssal and hadal peracarid crustacean communities in the eastern Aleutian Trench (NE Pacific) 东太平洋阿留申海沟深层和浅层甲壳类群落形成的生态和空间因素
IF 4.1 3区 地球科学 Q1 OCEANOGRAPHY Pub Date : 2025-12-19 DOI: 10.1016/j.pocean.2025.103651
Davide Di Franco, Stefanie Kaiser, Andreas Kelch, Mathis Preikschardt, Magdalena Błażewicz, Nils Brenke, Sarah Gerken, Kamila Głuchowska, Karen Jeskulke, Henry Knauber, Katharina Kohlenbach, Anne Helene S. Tandberg, Anna Jażdżewska, Angelika Brandt
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引用次数: 0
Monthly and seasonal variations in ocean near-surface gradients around Santo Antão Island: A 20-year MODIS-aqua study 圣安托<e:1>岛附近海洋近表面梯度的月和季节变化:20年MODIS-aqua研究
IF 4.1 3区 地球科学 Q1 OCEANOGRAPHY Pub Date : 2025-12-18 DOI: 10.1016/j.pocean.2025.103654
Cassandra Santos-Pacheco, Issah N. Suleiman, Tiago Da Rosa Serpa, Miguel Figueiredo, Ana Martins
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引用次数: 0
Ice melt season in the Kara Sea: Size-fractionated primary production and chlorophyll-a, evolution of the subsurface chlorophyll maximum layer and its contribution to total water column values 喀拉海融冰季节:初级生产和叶绿素-a的大小分异、次表层叶绿素最大层的演变及其对总水柱值的贡献
IF 3.6 3区 地球科学 Q1 OCEANOGRAPHY Pub Date : 2025-12-18 DOI: 10.1016/j.pocean.2025.103652
Andrey B. Demidov , Tatiana A. Belevich , Anna V. Kostyleva , Valentina M. Sergeeva , Alexander A. Polukhin , Vladimir A. Artemiev , Andrey A. Nedospasov , Dragosh I. Migali , Mikhail V. Flint
The characteristics of phytoplankton variability during spring sea ice retreat are poorly understood at the regional scale. To address this gap, three cruises were conducted in the Kara Sea from late June to early August during sea ice retreat. The present study focused on the variability of primary production (PP), chlorophyll-a (Chl-a) concentration of total and size-fractionated phytoplankton, the evolution of the subsurface Chl-a maximum layer (SCML), and its contribution to the total water column PP (IPPtot) and integrated photosynthetic layer Chl-a (Chlph). During the study period, the ice-edge phytoplankton bloom was characterised by high values of IPPtot and Chlph (up to 1352 mgC m−2 d–1 and 151.53 mg m−2, respectively) and a dominance of microphytoplankton (>20 µm) in the water column (88 % of IPPtot and 77 % of Chlph on average) and in the SCML (52 % of PP and 64 % of Chl-a on average). The role of nano- (3 – 20 µm) and picophytoplankton (<3 µm) increased with sea ice retreat. During the melt season, micro-, nano- and picophytoplankton contributed on average 50, 14 and 36 % to IPPtot and 60, 15 and 25 % to Chlph, respectively. PP and Chl-a associated with the SCML contributed 32 % to IPPtot and 76 % to Chlph. The rapid decline in IPPtot during sea ice retreat suggests that Arctic warming, sea ice loss, and the significant increase in total PP due to newly exposed open water areas may not be accompanied by an increase in photosynthetic activity in the Arctic Ocean. During the ice melt season in the Kara Sea ∼1/3 of IPPtot and 3/4 of Chlph are concentrated in the SCML, emphasizing its importance in the seasonal trophic balance and in the development of PP algorithms.
在区域尺度上,对春季海冰退缩过程中浮游植物的变异特征了解甚少。为了填补这一空白,从6月下旬到8月初海冰消退期间,在喀拉海进行了三次巡航。本研究主要研究了总分异浮游植物初级生产量(PP)、叶绿素-a (Chl-a)浓度的变异性、次表层最大叶绿素层(SCML)的演化及其对总水柱PP (IPPtot)和综合光合层Chl-a (Chlph)的贡献。在研究期间,冰边浮游植物爆发的特征是高IPPtot和Chlph值(分别高达1352 mgC m - 2 d-1和151.53 mg m - 2),并且在水柱(平均占IPPtot的88%和Chlph的77%)和SCML(平均占PP的52%和Chl-a的64%)中占主导地位的微型浮游植物(>20µm)。纳米(3 ~ 20µm)和浮游植物(<3µm)的作用随着海冰的退缩而增强。在融化期,微浮游、纳米浮游和浮游植物对IPPtot的平均贡献率分别为50%、14%和36%,对Chlph的平均贡献率分别为60%、15%和25%。与SCML相关的PP和Chl-a分别占IPPtot的32%和Chlph的76%。海冰退缩期间IPPtot的快速下降表明,北极变暖、海冰消失以及由于新暴露的开放水域而导致的总PP的显著增加可能并不伴随着北冰洋光合活性的增加。在喀拉海的融冰季节,约1/3的IPPtot和3/4的Chlph集中在SCML中,强调了SCML在季节性营养平衡和PP算法发展中的重要性。
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引用次数: 0
Influence of the Kuroshio Current on the benthic communities in the southern seas of Korea 黑潮对朝鲜南部海域底栖生物群落的影响
IF 4.1 3区 地球科学 Q1 OCEANOGRAPHY Pub Date : 2025-12-18 DOI: 10.1016/j.pocean.2025.103658
Sang Lyeol Kim, Hyung-Gon Lee, Kyung-Hee Oh, Kongtae Ra, Ok Hwan Yu
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引用次数: 0
Halocline as an environmental barrier for the larvae of Arctic marine benthic invertebrates 盐跃层作为北极海洋底栖无脊椎动物幼体的环境屏障
IF 4.1 3区 地球科学 Q1 OCEANOGRAPHY Pub Date : 2025-12-14 DOI: 10.1016/j.pocean.2025.103649
Patuła Weronika, Ronowicz Marta, Kukliński Piotr, Weydmann-Zwolicka Agata
Many marine benthic invertebrates possess a pelagic larval life stage (meroplankton) that is highly sensitive to environmental changes, influencing their spatial distribution, survival, and settlement. This study was conducted on the adjacent shelf and in Kongsfjorden, a high-Arctic fjord system in Svalbard, where the Kongsfjorden Transect (KT), influenced by Arctic and Atlantic oceanic regimes, shows strong variability in physico-chemical conditions. Consequently, changes in environmental conditions, including the depth of the halocline, can act as a physical barrier for organisms, affecting local biodiversity. We, investigated meroplankton vertical distribution in relation to the halocline, and hypothesized that the salinity gradient acts as a barrier for larvae, influencing their movements, distribution and diversity. We identified 25 meroplankton morphotypes along the KT, with Bivalvia veligers as the dominant taxon. Taxonomic assemblages differed significantly between above (AH) and below (BH) the halocline. More abundant Echinodermata larvae characterized the AH assemblage, which remained compositionally similar throughout the studied transect. In contrast, Polychaeta larvae were characteristic of the BH assemblage with greater spatial variability, consistent with decreasing temperature, salinity, and chlorophyll a concentration, towards the inner part of the fjord. By integrating detailed morphotype analysis with hydrographic data, we showed that the halocline is a barrier for meroplankton larvae, defining their vertical distribution, abundance, and taxonomic composition; we also present the indicator taxa of the AH and BH assemblages. Our results emphasize the role of the salinity gradient in shaping larval communities and support their potential role as early indicators of environmental change in the Arctic fjords.
许多海洋底栖无脊椎动物都有一个对环境变化高度敏感的浮游生物幼虫阶段,影响它们的空间分布、生存和定居。这项研究是在邻近的大陆架和斯瓦尔巴群岛的高北极峡湾系统Kongsfjorden进行的,其中Kongsfjorden样带(KT)受北极和大西洋制度的影响,在物理化学条件上表现出强烈的变化。因此,环境条件的变化,包括盐跃层的深度,可以作为生物的物理屏障,影响当地的生物多样性。我们研究了浮游生物与盐跃层的垂直分布,并假设盐度梯度对幼虫起屏障作用,影响它们的运动、分布和多样性。结果表明,沿KT段共鉴定出25种浮游生物形态,以双壳壳浮游生物为优势分类群。在盐跃层上方(AH)和下方(BH)之间的分类组合差异显著。更丰富的棘皮虫幼虫具有AH组合的特征,在整个研究样带中其组成保持相似。多毛藻幼虫则以BH组合为特征,具有较大的空间变异性,与峡湾内部温度、盐度和叶绿素a浓度的降低一致。结合详细的形态分析和水文数据,我们发现盐跃层是浮游生物幼虫的屏障,定义了浮游生物幼虫的垂直分布、丰度和分类组成;并给出了AH和BH组合的指示分类群。我们的研究结果强调了盐度梯度在塑造幼虫群落中的作用,并支持它们作为北极峡湾环境变化早期指标的潜在作用。
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引用次数: 0
No discovery without exploration: Deep-sea sampling across the Pacific reveals a three new genus of Typhlotanaidae (Crustacea: Tanaidacea) 没有探索就没有发现:横跨太平洋的深海采样揭示了三种新的斑藻属(甲壳纲:斑藻科)
IF 4.1 3区 地球科学 Q1 OCEANOGRAPHY Pub Date : 2025-12-12 DOI: 10.1016/j.pocean.2025.103644
Marta Gellert, Magdalena Błażewicz, Chee Kong Chim, Graham J. Bird
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引用次数: 0
Variability of near-inertial internal wave energy in the Kuroshio extension from CPIES array observations CPIES阵列观测黑潮扩展中近惯性内波能量的变率
IF 3.6 3区 地球科学 Q1 OCEANOGRAPHY Pub Date : 2025-12-11 DOI: 10.1016/j.pocean.2025.103650
Y.R. Mu , Y.S. Xu , J.H. Park
Near-inertial internal waves (NIIWs) play a central role in ocean mixing and energy transfer, and understanding their local variability is essential for quantifying ocean energetics. This study investigates the local drivers of NIIW variability in the Kuroshio Extension System Study (KESS) region using observations from a Current-and Pressure-sensor-equipped Inverted Echo Sounder (CPIES) array deployed over a 600 km by 600 km area, assuming negligible net NIIW flux. We developed an empirical model to quantify the contributions of wind-induced near-inertial energy flux (WNEF), mixed layer depth (MLD), and relative vorticity (ζ), which have dominant influences on NIIW variability, accounting for 39 %, 41 %, and 20 % of the variability, respectively. WNEF and MLD positively correlate with NIIW energy, while ζ shows a negative correlation. These findings highlight the significance of local processes in modulating NIIW energy and improving our understanding of ocean mixing dynamics by transitioning from qualitative to quantitative analysis.
近惯性内波(NIIWs)在海洋混合和能量传递中起着核心作用,了解其局部变率对海洋能量学的量化至关重要。本文研究了黑潮延伸系统研究(KESS)区域NIIW变率的局部驱动因素,利用部署在600 km × 600 km区域的配备电流和压力传感器的反向回声测深仪(CPIES)阵列的观测数据,假设净NIIW通量可以忽略不计。我们建立了一个经验模型来量化风致近惯性能量通量(WNEF)、混合层深度(MLD)和相对涡度(ζ)对NIIW变率的贡献,它们对NIIW变率的影响占主导地位,分别占39%、41%和20%。WNEF和MLD与NIIW能量呈正相关,ζ呈负相关。这些发现强调了局部过程在调节NIIW能量方面的重要性,并通过从定性分析过渡到定量分析来提高我们对海洋混合动力学的理解。
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引用次数: 0
Fine-scale hydrodynamic variability at Majuro Atoll, Republic of the Marshall islands. Part I: Flow variability 马绍尔群岛共和国马朱罗环礁的精细尺度水动力变率。第一部分:流动可变性
IF 3.6 3区 地球科学 Q1 OCEANOGRAPHY Pub Date : 2025-12-11 DOI: 10.1016/j.pocean.2025.103648
Yan Jia , Weifeng (Gordon) Zhang , Steven J. Lentz , Nathaniel R. Mollica , Gonzalo Pérez-Rosales , Anne L. Cohen
Majuro, a coral atoll in the Central Pacific, consists of rim reefs and low-lying islands surrounding a lagoon 40 km long, 10 km wide, and averaging 35 m deep. The lagoon is connected to the open ocean through shallow reef flats along the northwestern and western rims, and a 40 m deep channel in the northern rim. Spatiotemporal variability of lagoon hydrodynamics is characterized with a 15-year (2009–2023) simulation of a high-resolution ocean-wave coupled model. In winter, strong northeasterly winds generate high waves that approach the atoll from the northeast, breaking on the reef flats to the northwest of the lagoon, and driving strong flow across the reef flats into the lagoon. The wave- and wind-driven flows together forms a counterclockwise vortex pattern over the entire water column in the western lagoon, leading to a strong barotropic outflow through the deep channel. The lagoon circulation in winter is thus laterally sheared. In summer with weaker northeasterly winds, the wave-driven overflow across the northwestern reef flats weakens. In fall, episodic westerly winds drive open ocean water across the western reef flat into the lagoon. The weak winds in summer and fall allow the development of vertically sheared flows in the lagoon, with surface flows generally aligned with winds and subsurface flows opposing winds. This study demonstrates that lagoon circulation, varying over the scale of O(100 m-10 km), differ drastically from that in the surrounding ocean, can directly affect coral reef communities, and is thus critical for effective marine resource management.
Plain language summary.
Majuro Atoll, Republic of Marshall Islands, is located in the Central Pacific and is made up of rim reefs and islands surrounding lagoon of 40 km long and 10 km wide. The lagoon is separated from the open ocean by shallow rim reefs on its north and west sides and an island chain on its south and east sides. The deep part of the lagoon is connected to the open ocean by a 40-m deep channel in the north. This work uses a high-resolution computer model to simulate flows and temperature conditions in 2009–2023 and study how the lagoon flow conditions change in space and time. The model shows that the lagoon flows are influenced not only by winds throughout the year but also by high waves approaching the atoll from the northeast. As the waves break on the north shore of the atoll, they push a significant amount of water into the lagoon. Some of the lagoon water then flow out into the open ocean through the deep channel. Circulation in the lagoon changes dramatically with the winds. All these flow changes in the lagoon cause the lagoon environment to differ significantly from the open ocean. Such fine-scale changes in lagoon conditions likely affect coral health, influence their responses to climate change, and provide key information for effective coral reef conservation and protection.
马朱罗是太平洋中部的一个环礁,由环礁和低洼岛屿组成,周围是一个长40公里,宽10公里,平均深35米的泻湖。泻湖通过西北和西部边缘的浅礁滩与开阔的海洋相连,北部边缘有一条40米深的通道。利用高分辨率海波耦合模式的15年(2009-2023)模拟分析了泻湖水动力的时空变化特征。在冬季,强烈的东北风产生的巨浪从东北方向接近环礁,在礁滩上打破到泻湖的西北部,并推动强烈的水流穿过礁滩进入泻湖。波浪和风驱动的水流共同在西部泻湖的整个水柱上形成逆时针的漩涡模式,导致强烈的正压性流出通过深通道。因此,冬季的泻湖环流被横向剪切。在夏季,东北风减弱,西北礁滩的波浪溢出减弱。秋天,断断续续的西风将开阔的海水吹过西部礁滩,注入泻湖。夏季和秋季的弱风使泻湖的垂直剪切流得以发展,表面流通常与风一致,而地下流则与风相反。这项研究表明,在0 (100 m-10 km)尺度上变化的泻湖环流与周围海洋的环流有很大不同,可以直接影响珊瑚礁群落,因此对有效的海洋资源管理至关重要。简单的语言总结。马绍尔群岛共和国马朱罗环礁位于太平洋中部,由环礁和岛屿组成,周围有40公里长,10公里宽的泻湖。泻湖与开阔的海洋被北部和西部的浅海礁和南部和东部的岛链隔开。泻湖的深处通过北部一条40米深的通道与开阔的海洋相连。这项工作使用高分辨率的计算机模型来模拟2009-2023年的流量和温度条件,并研究泻湖流量条件在空间和时间上的变化。该模型表明,泻湖的流量不仅受到全年风的影响,而且还受到从东北方向接近环礁的大浪的影响。当波浪在环礁的北岸破碎时,它们将大量的水推入泻湖。一些泻湖的水然后通过深通道流入开阔的海洋。泻湖的环流随着风的变化而急剧变化。所有这些在泻湖的流量变化导致泻湖的环境明显不同于开放的海洋。泻湖条件的这种细微变化可能影响珊瑚健康,影响它们对气候变化的反应,并为有效的珊瑚礁养护和保护提供关键信息。
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引用次数: 0
Does an arctic circumpolar distribution exist for deep-sea sponges? Unravelling the systematics of Stylocordyla borealis (Porifera: Demospongiae) through integrative taxonomy 深海海绵存在北极绕极分布吗?用综合分类学揭示北方styloordyla borealis (Porifera: Demospongiae)的系统
IF 4.1 3区 地球科学 Q1 OCEANOGRAPHY Pub Date : 2025-12-11 DOI: 10.1016/j.pocean.2025.103646
Franziska I. Theising, Ute Hentschel, Kathrin Busch, Angelika Brandt, Francisca Carvalho, Joana R. Xavier, Andreu Santín Muriel
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引用次数: 0
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Progress in Oceanography
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