Marie-Elodie Perga, Thorsten Dittmar, Damien Bouffard, Emma Kritzberg
{"title":"The elephant in the conference room: reducing the carbon footprint of aquatic science meetings","authors":"Marie-Elodie Perga, Thorsten Dittmar, Damien Bouffard, Emma Kritzberg","doi":"10.1002/lol2.10402","DOIUrl":"10.1002/lol2.10402","url":null,"abstract":"<p>The ASLO community is firmly committed to a sustainable future, and themes of the past conferences often infer a link between aquatic systems evolution and climate change. At the latest Aquatic Sciences Meeting (ASM) in 2023, climate change and carbon-centered topics were salient themes, making up to 50% of all contributions (Fig. 1). Many keynotes were remarked on for their willingness to engage toward actions and solutions and go beyond the sole report of dangers and threats posed by climate change and other overpassed planetary limits.</p><p>Taking part in international scientific conferences such as ASM makes an integrated component of our academic life. Expectations from scientific conferences are to provide an opportunity to stay informed about the latest developments, disseminate one's own research, discuss perspectives and ideas, and get inspired. Scientific conferences also foster a sense of belonging to a community and offer a social context in which to expand research networks. In line with this, academic incentives and travel support are high and on the rise (Bojica et al. <span>2022</span>). Yet, scientific conferencing also generates significant CO<sub>2</sub> emissions at the Worldwide scale. Eighty percent of the carbon footprint of international conferences is made up of air travel, with a lower estimate of roughly 1 tCO<sub>2−e</sub> (metric tons of carbon dioxide equivalent, that is, the number of metric tons of CO<sub>2</sub> emissions with the same global warming potential as one metric ton of another greenhouse gas) emitted per attendee for transportation (Klower et al. <span>2020</span>; Tao et al. <span>2021</span>). If half of the 8 million worldwide academics were to take part annually in an international conference (Sarabipour et al. <span>2021</span>), transporting academics to international conferences would generate a back-of-the-envelope estimate of 4 MtCO<sub>2−e</sub>, rivaling with annual emissions of countries such as Niger, Nicaragua, or Latvia (Crippa et al. <span>2022</span>).</p><p>Meeting the Paris Agreement to contain warming to the 1.5°C target requires that the emissions per capita fall down to 2.3 tCO<sub>2−e</sub> by 2030 (Gore <span>2021</span>), while, due to their hypermobile lifestyle, the sole professional travel-related annual emissions for academics can easily reach 6 tCO<sub>2−e</sub> per capita (Ciers et al. <span>2019</span>). The significance of the carbon footprint of scientific conferences has led individual academics and scientific societies to question the current model for conferencing (Malcolm <span>2008</span>; Achten et al. <span>2013</span>; Arsenault et al. <span>2019</span>; Klower et al. <span>2020</span>; Tao et al. <span>2021</span>). Despite extending beyond our immediate community, this issue holds particular significance for us within the ASLO community, as we travel the World and generate such greenhouse emissions specifically to meet and devise climate-related matters a","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":"9 5","pages":"499-505"},"PeriodicalIF":5.1,"publicationDate":"2024-05-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/lol2.10402","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140910593","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
M. Lindhart, M. A. Daly, H. Walker, I. B. Arzeno-Soltero, J. Z. Yin, T. W. Bell, S. G. Monismith, G. Pawlak, J. J. Leichter
{"title":"Short wave attenuation by a kelp forest canopy","authors":"M. Lindhart, M. A. Daly, H. Walker, I. B. Arzeno-Soltero, J. Z. Yin, T. W. Bell, S. G. Monismith, G. Pawlak, J. J. Leichter","doi":"10.1002/lol2.10401","DOIUrl":"10.1002/lol2.10401","url":null,"abstract":"<p>Giant kelp (<i>Macrocystis pyrifera</i>) forests are common along the California coast. Attached on the rocky bottom at depths of approximately 5–25 m, the kelp, when mature, spans the water column and develops dense, buoyant canopies that interact with waves and currents. We present two novel results based on observations of surface gravity waves in a kelp forest in Point Loma, California. First, we report short wave (1–3 s) attenuation in kelp, quantified by an exponential decay coefficient <span></span><math>\u0000 <mrow>\u0000 <mi>α</mi>\u0000 <mo>∼</mo>\u0000 <mi>O</mi>\u0000 <mfenced>\u0000 <mrow>\u0000 <msup>\u0000 <mn>10</mn>\u0000 <mrow>\u0000 <mo>−</mo>\u0000 <mn>3</mn>\u0000 </mrow>\u0000 </msup>\u0000 <msup>\u0000 <mi>m</mi>\u0000 <mrow>\u0000 <mo>−</mo>\u0000 <mn>1</mn>\u0000 </mrow>\u0000 </msup>\u0000 </mrow>\u0000 </mfenced>\u0000 </mrow></math>—comparable to the dampening effect of sea ice. Second, we identify seasonal and tidal changes in attenuation, peaking mid-summer with maximum kelp cover, and during low tide when a greater proportion of the fronds are at the surface. Thus, the naturally occurring surface canopies of kelp forests can act as temporally varying, high-frequency filters of wave energy.</p>","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":"9 4","pages":"478-486"},"PeriodicalIF":5.1,"publicationDate":"2024-05-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/lol2.10401","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140907310","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Patrick K. Thomas, Marrit Jacob, Esteban Acevedo-Trejos, Helmut Hillebrand, Maren Striebel
{"title":"Species richness and intraspecific variation interactively shape marine diatom community functioning","authors":"Patrick K. Thomas, Marrit Jacob, Esteban Acevedo-Trejos, Helmut Hillebrand, Maren Striebel","doi":"10.1002/lol2.10398","DOIUrl":"10.1002/lol2.10398","url":null,"abstract":"<p>Biodiversity generally increases productivity in ecosystems; however, this is mediated by the specific functional traits that come with biodiversity loss or gain and how these traits interact with environmental conditions. Most biodiversity studies evaluate the effects of species richness alone, despite our increasing understanding that intraspecific diversity can have equally strong impacts. Here, we manipulate both species richness and intraspecific richness (i.e., number of distinct strains) in marine diatom communities to explicitly test the relative importance of species and strain richness for biomass and trait diversity in six distinct temperature/nutrient environments. We show that species and strain richness both have significant effects on biomass and growth rates, but more importantly, they interact with each other, indicating that cross-species diversity effects depend on within-species diversity and vice versa. This intertwined relationship thus calls for more integrative approaches quantifying the relative importance of distinct biodiversity components and environmental context on ecosystem functioning.</p>","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":"9 5","pages":"612-623"},"PeriodicalIF":5.1,"publicationDate":"2024-05-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/lol2.10398","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140895389","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Assessing N2 fixation flux and its controlling factors in the (sub)tropical western North Pacific through high-resolution observations","authors":"Xinran Yu, Zuozhu Wen, Ruotong Jiang, Jin-Yu Terence Yang, Zhimian Cao, Haizheng Hong, Yuntao Zhou, Dalin Shi","doi":"10.1002/lol2.10404","DOIUrl":"10.1002/lol2.10404","url":null,"abstract":"<p>The (sub)tropical western North Pacific is potentially an area of intense nitrogen (N<sub>2</sub>) fixation in the global ocean, despite limited understanding of the flux and controlling factors. We conducted high-resolution observations from 2016 to 2021 in this region and used machine learning algorithms to simulate N<sub>2</sub> fixation flux. Models estimated an N<sub>2</sub> fixation flux from 5.72 to 6.45 Tg N yr<sup>−1</sup>, with strong seasonal variation and peak rates in summer. The western North Pacific Subtropical Gyre and the Kuroshio Current contributed more to N<sub>2</sub> fixation flux than did the adjacent areas. Models suggested that sea surface temperature, photosynthetically available radiation, and nutrient supply were most strongly correlated with seasonal and spatial variations in N<sub>2</sub> fixation. This study provides an improved estimation of N<sub>2</sub> fixation in the western North Pacific and advances our understanding of its role in ocean productivity.</p>","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":"9 6","pages":"716-724"},"PeriodicalIF":5.1,"publicationDate":"2024-05-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/lol2.10404","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140821777","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Qualitative and quantitative changes in phenology of chlorophyll a concentrations during the transition from eutrophy to oligotrophy","authors":"Dietmar Straile, Karl-Otto Rothhaupt","doi":"10.1002/lol2.10403","DOIUrl":"10.1002/lol2.10403","url":null,"abstract":"<p>The PEG (Plankton Ecology Group) model predicts differences in phenology between eutrophic and oligotrophic lakes regarding the occurrence, timing and magnitude of annual chlorophyll maxima and minima. While these predictions have been tested between lakes, hardly any tests exist using long-term data. We test these predictions using chlorophyll time-series (1980–2019) from Lake Constance in which trophic status shifted from eutrophic to oligotrophic conditions. We show that oligotrophication subsequently resulted in reduction of the summer and spring blooms, and finally the loss of the clear-water phase. In contrast to the PEG model the spring bloom was not delayed, but advanced with oligotrophication. Warming modified the seasonal patterns via advancing clear-water timing. Oligotrophication did not only influence phenologies, but also the importance of independent variables driving phenologies. Thus, the decline of nutrients was the dominant factor in shaping the seasonal patterns of chlorophyll in Lake Constance during the last four decades.</p>","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":"9 4","pages":"354-363"},"PeriodicalIF":5.1,"publicationDate":"2024-05-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/lol2.10403","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140821562","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Giulia Gionchetta, Rebeca Arias-Real, Pilar Hurtado, Helmut Bürgmann, Cayetano Gutiérrez-Cánovas
{"title":"Key bacterial groups maintain stream multifunctionality in response to episodic drying","authors":"Giulia Gionchetta, Rebeca Arias-Real, Pilar Hurtado, Helmut Bürgmann, Cayetano Gutiérrez-Cánovas","doi":"10.1002/lol2.10400","DOIUrl":"10.1002/lol2.10400","url":null,"abstract":"<p>Microbial biodiversity is fundamental to maintain ecosystem functioning in seasonally variable ecosystems. However, it remains unclear how alterations in water availability caused by episodic drying compromise the ability of stream microbes to maintain multiple functions simultaneously (e.g., primary production and carbon cycling). Using data from 32 streams, we investigated how the phenology of annual drying influences stream sediment microbial biodiversity and their capacity to sustain multifunctionality. Our results showed that stream multifunctionality and most bacteria did not respond to changes in drying phenology. Only two bacterial groups, the drying-resistant Sphingobacteriia and the drying-sensitive Acidobacteria_Gp7, exhibited positive associations with multifunctionality; whereas, bacterial diversity showed a negative correlation with functions. Among these biodiversity aspects, Sphingobacteriia showed the strongest capacity to maintain multifunctionality at low and moderate performance levels. Our findings will help to better understand the mechanisms through which biodiversity sustains the functioning of seasonally variable streams and their responses to global change.</p>","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":"9 3","pages":"286-295"},"PeriodicalIF":7.8,"publicationDate":"2024-04-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/lol2.10400","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140817626","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Camilla Liénart, Alan Fournioux, Andrius Garbaras, Arnaud Lheureux, Hugues Blanchet, Nicolas Briant, Stanislas F. Dubois, Aline Gangnery, Anne Grouhel Pellouin, Pauline Le Monier, Xavier De Montaudouin, Nicolas Savoye
{"title":"Bivalve tissues as a recorder of multidecadal global anthropogenic and climate-mediated change in coastal areas","authors":"Camilla Liénart, Alan Fournioux, Andrius Garbaras, Arnaud Lheureux, Hugues Blanchet, Nicolas Briant, Stanislas F. Dubois, Aline Gangnery, Anne Grouhel Pellouin, Pauline Le Monier, Xavier De Montaudouin, Nicolas Savoye","doi":"10.1002/lol2.10399","DOIUrl":"10.1002/lol2.10399","url":null,"abstract":"<p>Recent rapid changes in climate and environmental conditions have significantly impacted coastal ecosystem functioning. However, the complex interplay between global and local effects makes it challenging to pinpoint the primary drivers. In a multi-ecosystem study, we analyzed pluri-decadal trends of bivalve-δ<sup>13</sup>C as recorder of global environmental changes. These trends were correlated with large-scale natural and anthropogenic climate proxies to identify whether coastal biota responded to global effects. Our findings revealed decreasing bivalve-δ<sup>13</sup>C trends in all sea regions, mainly linked with increased temperature and atmospheric-CO<sub>2</sub> concentrations, the later generating a decrease in atmospheric-CO<sub>2</sub> δ<sup>13</sup>C values (Suess effect) because of fossil-fuel burning. After removing the Suess effect from bivalve-δ<sup>13</sup>C trends, ongoing global climate variability continues to affect most ecosystems, possibly intensified by combined, interacting regional or local effects. These results highlight the need to consider large-scale effects to fully understand ecosystem and food web responses to the multiple effects of global change.</p>","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":"9 5","pages":"653-666"},"PeriodicalIF":5.1,"publicationDate":"2024-04-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/lol2.10399","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140651543","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Whales and cephalopods in a deep-sea arms race","authors":"Henk-Jan Hoving, Fleur Visser","doi":"10.1002/lol2.10391","DOIUrl":"10.1002/lol2.10391","url":null,"abstract":"<p>The pelagic deep sea is an enormous three-dimensional space that poses unique selective pressures. In absence of sun light, the dominant forms of communication are bioluminescence and sound. Diverse, abundant taxa inhabit the pelagic deep sea (water column >200 m). These taxa range from microplankton to meganekton, which may aggregate and migrate, resulting in a dynamic system with patches of high biomass—and rich hunting grounds for oceanic predators.</p><p>Toothed whales are mammalian top predators that occur in all oceans. Many of these, including beaked and sperm whales, hunt for deep-sea cephalopods, in particular squids (Clarke <span>2006</span>) (Fig. 1). They have evolved a range of morphological, physiological, and behavioral traits enabling prolonged breath-hold dives to 100 or 1000s of meters (Kooyman <span>2009</span>). Deep-diving toothed whales (i.e., odontocetes routinely foraging deeper than 200 m) are efficient, often generalist predators, daily capturing hundreds of prey (Visser et al. <span>2021</span>). Most cephalopods are fast-growing, relatively short-lived predators with a single reproductive cycle followed by death (semelparity), a life history adaptation that is possibly driven by a massive increase in predation pressure subsequent to the evolutionary loss of the external shell (Amodio et al. <span>2019</span>). Their size and high gonadal investment makes them nutritious prey (Boyle and Rodhouse <span>2005</span>).</p><p>The evolution of cephalopod avoidance strategies is strongly rooted in their response to predominantly visual predators. Cephalopods have co-existed with their main predators, fishes, for 530 million years (Jaitly et al. <span>2022</span>). The much more recent entry of mammals into the marine realm and ensuing evolution of predatory toothed whale echolocation (34 million years ago), created strongly different selective pressures on cephalopod adaptive strategies to avoid predation—this time by acoustic predators. The resulting evolutionary arms race in predator–prey adaptations has shaped the cephalopods and toothed whales into the organisms roaming our modern oceans. Their interactions, however, remain unobserved, and unknown. Have pelagic cephalopods succeeded in eluding large, warm-blooded predators geared for long-range detection of prey? Which traits drive the deep-sea arms race between toothed whales and cephalopods?</p><p>Here, we combine the current knowledge on deep-diving toothed whale predators and their cephalopod prey (focused on oegopsid squids) to reconstruct their sequence of predatory interactions, from search to selection and capture. In the light of current ecological concepts, we form four testable hypotheses supported by research approaches, advancing to a scientific framework that will help understand the selective pressures shaping deep-sea predator–prey systems.</p><p>Cephalopods can sense vibrations using a system analogous to the lateral line system of fishes, and rely o","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":"9 3","pages":"165-171"},"PeriodicalIF":7.8,"publicationDate":"2024-04-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/lol2.10391","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140642642","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Harshith Bachimanchi, Matthew I. M. Pinder, Chloé Robert, Pierre De Wit, Jonathan Havenhand, Alexandra Kinnby, Daniel Midtvedt, Erik Selander, Giovanni Volpe
{"title":"Deep-learning-powered data analysis in plankton ecology","authors":"Harshith Bachimanchi, Matthew I. M. Pinder, Chloé Robert, Pierre De Wit, Jonathan Havenhand, Alexandra Kinnby, Daniel Midtvedt, Erik Selander, Giovanni Volpe","doi":"10.1002/lol2.10392","DOIUrl":"10.1002/lol2.10392","url":null,"abstract":"<p>The implementation of deep learning algorithms has brought new perspectives to plankton ecology. Emerging as an alternative approach to established methods, deep learning offers objective schemes to investigate plankton organisms in diverse environments. We provide an overview of deep-learning-based methods including detection and classification of phytoplankton and zooplankton images, foraging and swimming behavior analysis, and finally ecological modeling. Deep learning has the potential to speed up the analysis and reduce the human experimental bias, thus enabling data acquisition at relevant temporal and spatial scales with improved reproducibility. We also discuss shortcomings and show how deep learning architectures have evolved to mitigate imprecise readouts. Finally, we suggest opportunities where deep learning is particularly likely to catalyze plankton research. The examples are accompanied by detailed tutorials and code samples that allow readers to apply the methods described in this review to their own data.</p>","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":"9 4","pages":"324-339"},"PeriodicalIF":5.1,"publicationDate":"2024-04-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/lol2.10392","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140620483","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Recent warming of the Kuroshio Current has promoted offshore sediment transport in the Yellow Sea","authors":"Yong Shi, Xiaomei Xu, Tao Liu, Guang Yang, Shengjing Liu, Jixuan Lyu, Shuo Zhang, Hui Sheng, Jianhua Gao","doi":"10.1002/lol2.10396","DOIUrl":"10.1002/lol2.10396","url":null,"abstract":"<p>As cross-shelf gradients of most properties are typically much steeper than those in the alongshore direction, transport across isobaths tends to be inhibited, particularly at oceanic fronts where cross-shelf gradients are markedly pronounced. Consequently, variations in cross-shelf gradients may exert a significant influence on offshore transport; however, this influence is not yet well understood. This study employs reconstructed daily suspended sediment concentration (SSC) data from the Yellow Sea's offshore region to investigate the dynamics of offshore transport. Our analysis on an interannual scale shows that offshore SSC correlates more with temperature gradients at the oceanic front than with winter storms, despite the latter's vital role in causing frontal instability. The observed increase in offshore transport over the past two decades is likely connected to Kuroshio Current warming, which has strengthened the horizontal density gradient at the oceanic front, driving the strengthened offshore transport of coastal sediments during instability episodes.</p>","PeriodicalId":18128,"journal":{"name":"Limnology and Oceanography Letters","volume":"9 4","pages":"452-460"},"PeriodicalIF":5.1,"publicationDate":"2024-04-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/lol2.10396","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140620190","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}