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Impacts of flooding on agricultural practices in Bunkure Local Government Area, Kano State, Nigeria 洪水对尼日利亚卡诺州邦库尔地方政府地区农业生产的影响
Pub Date : 2026-01-01 DOI: 10.1016/j.eve.2026.100110
Inuwa Sani Sani, Adi Wibowo
Flooding has become one of the key environmental issues that have impacted agricultural productivity in northern Nigeria. This study examines the impacts of recurrent flooding on agricultural practices in Bunkure Local Government Area, Kano State, integrating multi-year satellite-derived Land Use/Land Cover (LULC) analysis, Digital Elevation Model (DEM) terrain assessment, and household survey data. The LULC classifications (2019–2023) based on Landsat data show the presence of considerable Spatio temporal changes in agricultural land, vegetation, bare land and water bodies, which are highly affected by seasonal floods. Terrain analysis also indicates that hydromorphic lowlands in the southern and central parts of the LGA are highly prone to inundation, resulting in prolonged waterlogging of farmlands. The outcomes of the surveys conducted on 346 farmers affirm the prevalence of the effects such as delayed growth of crops, untimely death of crops, changed planting time and low quality of harvests. The findings align with recent studies showing increasing flood frequency and rainfall intensity across northern Nigeria linked to climate variability. In general, flooding has led to massive loss of crops, soil erosion and economic distress particularly to smallholders and vulnerable farmers. The combined spatial and socio-economic analysis indicates evidence that there are changes in the agricultural land availability and productivity in response to the annual floods. The research recommends that flood resistant crop varieties, better drainage systems, and land-use planning should be adopted in minimizing the exposure of farmlands to flooding. Enhancing the early warning system and incorporating local knowledge in line with the contemporary farming practices will boost resiliency in the communities. The study provides context-related observations to enable policy intervention in the case of sustainable agricultural and disaster-risk management in flood-prone rural LGAs.
洪水已经成为影响尼日利亚北部农业生产力的关键环境问题之一。本研究综合了多年卫星土地利用/土地覆盖(LULC)分析、数字高程模型(DEM)地形评估和住户调查数据,研究了卡诺州邦库尔地方政府地区经常性洪水对农业生产的影响。基于Landsat数据的lucc分类(2019-2023年)显示,受季节性洪水影响较大的农用地、植被、裸地和水体存在较大的时空变化。地形分析还表明,LGA南部和中部的水形低地极易被淹没,导致农田涝渍时间延长。对346名农民进行的调查结果证实,诸如作物生长延迟、作物过早死亡、种植时间改变和收成质量低下等影响普遍存在。这些发现与最近的研究结果一致,这些研究表明,尼日利亚北部洪水频率和降雨强度的增加与气候变化有关。总的来说,洪水造成了大量的作物损失、土壤侵蚀和经济困境,特别是对小农和脆弱的农民。综合空间和社会经济分析表明,农业用地可利用性和生产力在响应年度洪水时发生了变化。该研究建议,应该采用抗洪作物品种、更好的排水系统和土地利用规划,以尽量减少农田遭受洪水的风险。加强早期预警系统,结合符合当代农业实践的当地知识,将提高社区的复原力。该研究提供了与环境相关的观察结果,以便在易发洪水的农村地方政府可持续农业和灾害风险管理的情况下进行政策干预。
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引用次数: 0
Heavy metal contamination in water and sediment of a tropical urbanizing landscape: Insights from Akkulam–Veli Lake, southwest coast, India 热带城市化景观中水和沉积物中的重金属污染:来自印度西南海岸阿库拉姆-维利湖的见解
Pub Date : 2026-01-01 DOI: 10.1016/j.eve.2026.100112
Arsha , Pooja Pradeep , S.G. Dhanil Dev , E. Shaji , P.K. Krishna Prasad , S. Swetha , S. Arya , V. Deepchand , Mohammed Noohu Nazeer
A comprehensive hydrogeological investigation was conducted to evaluate heavy metal contamination in water and sediments of the Akkulam–Veli Lake system, a rapidly urbanizing coastal landscape in Thiruvananthapuram, Kerala, southwest India. Decadal land use/land cover (LULC) analysis (2014–2023) over a 7.05 km2 area revealed extensive urban expansion, with built-up areas increasing sharply at the expense of vegetation and wetlands, reflecting intense anthropogenic pressure. Water and sediment samples were analyzed for physicochemical parameters and heavy metals using Microwave Plasma Atomic Emission Spectroscopy and Atomic Absorption Spectrophotometry, integrated with GIS-based spatial analysis. Sediments exhibited elevated concentrations of Zn (up to 285 mg/kg), Ni (113 mg/kg), Cu (74 mg/kg), Pb (66–260 mg/kg), Cd (1.14–8.21 mg/kg), Fe (255–1755 mg/kg), and Cr (86–241 mg/kg), with lead exceeding permissible limits by up to 6.5 times. Water samples showed Zn concentrations up to 5.6 mg/L, Cd up to 0.24 mg/L, Fe up to 0.37 mg/L, and Cr up to 0.09 mg/L, frequently surpassing drinking-water standards. Pollution indices identified severe contamination hotspots near Parvathy Puthanaar and Kochuveli, closely associated with unplanned urban development, dredging activities, and untreated effluent discharge. Comparison with earlier studies (2012–2014) indicates a marked escalation in heavy metal concentrations, particularly Pb, Cd, and Cr, highlighting intensifying anthropogenic influence. The findings underscore the need for continuous monitoring, stricter regulation of urban discharges, and future studies integrating seasonal variability, contaminant source apportionment, and ecological risk assessment to support sustainable management of tropical urban lake systems.
本文对印度西南部喀拉拉邦蒂鲁凡南得普拉姆(Thiruvananthapuram)快速城市化的沿海景观Akkulam-Veli湖系统的水和沉积物中的重金属污染进行了全面的水文地质调查。2014-2023年7.05 km2区域的年代际土地利用/土地覆盖(LULC)分析显示,城市扩张范围广泛,建成区急剧增加,植被和湿地受到损害,反映出强烈的人为压力。采用微波等离子体原子发射光谱法和原子吸收分光光度法,结合基于gis的空间分析技术,对水和沉积物样品的理化参数和重金属进行了分析。沉积物中Zn(高达285 mg/kg)、Ni (113 mg/kg)、Cu (74 mg/kg)、Pb (66 ~ 260 mg/kg)、Cd (1.14 ~ 8.21 mg/kg)、Fe (255 ~ 1755 mg/kg)、Cr (86 ~ 241 mg/kg)的浓度均有所升高,其中铅的浓度最高超标6.5倍。水样中锌含量高达5.6 mg/L,镉含量高达0.24 mg/L,铁含量高达0.37 mg/L,铬含量高达0.09 mg/L,经常超过饮用水标准。污染指数确定了Parvathy Puthanaar和Kochuveli附近的严重污染热点,与无计划的城市发展、疏浚活动和未经处理的污水排放密切相关。与早期研究(2012-2014)相比,重金属浓度显著上升,尤其是Pb、Cd和Cr,凸显了人为影响的加剧。研究结果强调,需要对城市排放进行持续监测和更严格的监管,并在未来的研究中整合季节变化、污染源分配和生态风险评估,以支持热带城市湖泊系统的可持续管理。
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引用次数: 0
Investigating size-asymmetric feeding among tyrannosaurids using tooth marks on a metatarsal from the Judith River Formation, Montana, USA 利用在美国蒙大拿州朱迪思河地层发现的跖骨上的牙印来研究暴龙的大小不对称摄食
Pub Date : 2026-01-01 DOI: 10.1016/j.eve.2026.100107
Josephine Nielsen , Denver Fowler , Taia Wyenberg-Henzler , Aase Roland Jacobsen , Christof Pearce
The Judith River Formation in Montana, USA, is a key Campanian-aged sedimentary package, with a rich fossil assemblage, including multiple tyrannosaurid taxa. This study documents BDM 124, a partial left metatarsal II exhibiting multiple tooth marks consistent with tyrannosaurid feeding activity. Using the Category-Modifier (CM) classification system and high-resolution 3D surface scanning, 16 distinct marks were systematically characterized. Morphometric analyses and Non-metric Multidimensional Scaling (NMDS) revealed grouping patterns suggestive of size-asymmetric feeding behavior. The small size and spacing of the marks indicate that they were produced by a small tyrannosaurid, most likely scavenging on the carcass of a significantly larger conspecific or closely related taxon. The absence of healing, mark placement on the metatarsal, and their morphology collectively suggest late-stage carcass consumption. The study contributes a new data point to our understanding of trophic dynamics and interactions among Late Cretaceous tyrannosaurids, highlighting the value of systematic methodologies for interpreting tooth marks.
美国蒙大拿州朱迪思河组是坎帕尼亚期重要的沉积包系,化石组合丰富,包括多个暴龙类群。本研究记录了BDM 124,一个局部左跖II,显示出与暴龙进食活动一致的多齿印。利用CM分类系统和高分辨率三维表面扫描,系统表征了16个明显的标记。形态计量学分析和非度量多维尺度(NMDS)揭示了提示尺寸不对称摄食行为的分组模式。这些标记的小尺寸和间距表明,它们是由一只小型暴龙留下的,很可能是在一个明显更大的同种或密切相关的分类单元的尸体上觅食。愈合的缺失,跖骨上的标记,以及它们的形态都表明尸体是在后期被消耗的。该研究为我们了解晚白垩世暴龙之间的营养动力学和相互作用提供了新的数据点,突出了系统方法解释牙印的价值。
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引用次数: 0
Source terranes, humid-weathering diagenesis, and fluvial deposition in the cretaceous Garoua Basin: Implications for correlation with the upper Benue (Bima) system Garoua盆地白垩系烃源体、湿风化成岩作用和河流沉积:与上贝努埃(Bima)体系的对比意义
Pub Date : 2026-01-01 DOI: 10.1016/j.eve.2026.100109
Hermann Nyochembeng Akateh , Olugbenga A. Boboye , Edwin Ayuk Ndip , Shivanjali Sharma , Darshan Halari , Andre Mbabi Bitchong , Raoul Gake Belle
The Cretaceous Garoua Rift Basin, an eastern extension of the Upper Benue Basin in West Africa, preserves a fluvial succession essential for understanding the syn-rift sediment deposition of the West and Central African Rift System (WCARS). This study provides a comprehensive analysis of the clastic fill of the basin, combining grain size statistics, thin section petrology, heavy-mineral analysis, X-ray diffraction, and scanning electron microscopy to elucidate the provenance, diagenesis, and depositional processes. The results reveal that the sediments consist primarily of medium-to coarse-grained, moderately to moderately well-sorted, arkose to subarkose, characterized by approximately leptokurtic and near-symmetrical grain size distributions. These textural attributes indicate deposition by bedload-dominated, braided to low-sinuosity fluvial systems under high-energy conditions. The signatures of provenance, characterised by a framework dominated by quartz, feldspar and a group of heavy minerals abundant in zircon, tourmaline and rutile (ZTR) alongside prominent garnet and staurolite (GZi = 23–59 %), clearly indicate a source from nearly granitoid and gneissic basement rock throughout Pan-African. Diagenesis was primarily influenced by humid-weathering processes, as evidenced by the high kaolinite content of feldspar (up to 43 wt%) and widespread hematite cementation, which together governed the development of the reservoir quality. The striking similarity in composition, texture, and diagenetic overprint between the Garoua Succession and the upper Bima Member of the Nigerian Benue Trough confirm their stratigraphic equivalence. This correlation defines a coherent Cretaceous river system within the Yola-Garoua rift arm, providing an improved model for source-to-basin dynamics and reservoir characterisation in humid climate rift basins.
白垩纪Garoua裂谷盆地是西非上贝努埃盆地的东部延伸,保留了对了解西非和中非裂谷系(WCARS)同裂谷沉积至关重要的河流演替。结合粒度统计、薄片岩石学、重矿物分析、x射线衍射、扫描电镜等综合分析盆地碎屑充填物,阐明物源、成岩作用和沉积过程。结果表明,沉积物主要由中~粗粒、中等~中等分选良好、粗粒~次粗粒组成,粒度分布呈近似细峰状,接近对称;这些结构属性表明,在高能条件下,沉积以层状物为主,编织成低弯曲度的河流体系。物源特征以石英、长石为主,以锆石、电气石和金红石(ZTR)为主的一组重矿物为特征,并伴有显著的石榴石和橄榄石(GZi = 23 - 59%),表明其物源来自泛非洲地区的近花岗质和片麻岩基岩。成岩作用主要受湿风化作用的影响,长石高岭石含量高(高达43%),赤铁矿胶结作用广泛存在,两者共同决定了储层质量的发展。Garoua演替与尼日利亚Benue海槽上Bima段在组成、结构和成岩叠印上的惊人相似性证实了它们的地层等效性。这种对比定义了Yola-Garoua裂谷臂内连贯的白垩纪河流系统,为湿润气候裂谷盆地的源-盆地动力学和储层特征提供了改进的模型。
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引用次数: 0
Enhancing paleoclimate reconstructions in the late Aptian North-Northeast Brazil using clay mineralogy 利用粘土矿物学加强阿普tian晚期巴西东北北部古气候重建
Pub Date : 2026-01-01 DOI: 10.1016/j.eve.2026.100111
Victor Matheus Joaquim Salgado-Campos , Luiz Carlos Bertolino , Leonardo Borghi , Aristóteles de Moraes Rios-Netto , Bruno Cesar Araújo , Danielle Cardoso de Souza , Laís de Oliveira Ferreira , Fabia Emanuela Rafaloski Bobco , Jéssica de Souza Gabi Barcellos , Ismar de Souza Carvalho
Paleoclimate changes are commonly analyzed on three distinct scales: small-scale (20–500 kyr), linked to Milankovitch cycles; medium-scale events (∼30 Myr), associated with sea-level changes and tectonic activity; and large-scale (∼300 Myr), related to icehouse-greenhouse transitions. Different methods are used in paleoclimatology, with clay mineralogy emerging as a particularly effective tool. This study presents an approach to understanding late Aptian paleoclimate variations in North-Northeastern Brazil using clay mineralogy. To achieve this, fifty-two mudrock samples from the late Aptian Codó and Itapecuru formations were analyzed in the Parnaíba Basin (Northeastern Brazil) using clay and bulk mineralogy, major element chemical analysis, and scanning electron microscopy. These new data were integrated with a compiled dataset and evaluated using climofunctions to reconstruct paleoprecipitation and paleotemperature conditions, which were subsequently compared with patterns observed in modern lacustrine environments. Three paleoclimate stages were identified in North-Northeastern Brazil during the late Aptian, characterized by four distinct clay mineral assemblages. From the older to the younger stages, the first one indicates paleoprecipitation values ranging from 800 to 1000 mm/yr and paleotemperatures of approximately 15 °C. The second stage indicates paleoprecipitation values of up to 200 mm/yr and paleotemperature values of approximately 22 °C. The third stage suggests paleoprecipitation values between 600 and 800 mm/yr and paleotemperature conditions of approximately 20 °C. These paleoclimate stages indicate an aridification followed by a humidification process during the late Aptian in North-Northeastern Brazil. The latter humidification is likely linked to the Gondwana break-up and the potential onset of Oceanic Anoxic Event 1b, which marks the transition from the Aptian to the Albian. This study contributes to the use of clay minerals in reconstructing past climates and enhances our understanding of late Aptian climate changes in North-Northeastern Brazil.
古气候变化通常在三个不同的尺度上进行分析:小尺度(20-500 kyr),与米兰科维奇旋回有关;与海平面变化和构造活动有关的中等尺度事件(~ 30 Myr);大尺度(~ 300 Myr),与冰-温室过渡有关。在古气候学中使用了不同的方法,粘土矿物学是一种特别有效的工具。本研究提出了一种利用粘土矿物学来理解巴西东北北部晚阿普提古气候变化的方法。为了实现这一目标,研究人员在Parnaíba盆地(巴西东北部)对来自晚Aptian Codó和Itapecuru地层的52个泥岩样本进行了粘土和大块矿物学、主要元素化学分析和扫描电子显微镜分析。将这些新数据与已编制的数据集相结合,利用气候函数进行评估,重建古降水和古温度条件,并将其与现代湖泊环境的模式进行比较。巴西东北部北部在阿普tian晚期确定了3个古气候阶段,其特征是4种不同的粘土矿物组合。从较老阶段到较年轻阶段,第一个阶段表明古降水值在800 ~ 1000 mm/yr之间,古温度约为15℃。第二阶段表明古降水量高达200 mm/yr,古温度值约为22°C。第三阶段表明古降水值在600 ~ 800 mm/yr之间,古温度条件约为20℃。这些古气候阶段表明,在巴西东北部北部的阿普tian晚期,一个干旱化之后是一个湿化过程。后者的湿化可能与冈瓦纳破裂和海洋缺氧事件1b的潜在开始有关,这标志着从阿普tian到Albian的过渡。该研究有助于利用粘土矿物重建过去的气候,并提高我们对巴西东北北部阿普提亚晚期气候变化的认识。
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引用次数: 0
Microbiome dynamics following coral transplantation and nursery culture in the Brazilian reef builder Mussismilia harttii 珊瑚移植和苗圃培养后的微生物组动力学在巴西珊瑚礁建造者Mussismilia harttii
Pub Date : 2026-01-01 DOI: 10.1016/j.eve.2026.100106
Tooba Varasteh , Reza Amir Ahmadi , Michele S. Lima , Georgia C. Atella , Claudia Omachi , Ana Carolina Vicente , Camila S. Oliveira , Carlos D. Pérez , Cristiane C. Thompson , Paula B. Gomes , Fabiano L. Thompson
Coral reefs, vital ecosystems that support diverse marine life, are increasingly facing threats from anthropogenic activities and environmental changes. In this study, we analyzed the site-specific effects of coral translocation on coral holobiont microbiomes. Polyps of Mussismilia harttii were transplanted from one reef location (Japaratinga, Alagoas, Brazil; JP) to another (Porto de Galinhas, Pernambuco; PG) 95.6 km away. JP is characterized by higher coral abundance and larger colony size indices than PG. Because the study design includes only two geographically distinct sites, interpretations are restricted to these locations. This study tested the hypothesis that donor-reef origin influences site- and time-associated longitudinal microbiome trajectories. The microbiome of transplanted JP corals differed after 1 month at PG, consistent with short-term compositional adjustment to local conditions rather than an inference of physiological stress; alpha-diversity differences were also detected and are reported descriptively without attributing environmental causation. After this period, transplanted corals demonstrated an increase in putative symbiont-associated genera (e.g., Ruegeria, Labrenzia, and Paracoccus) according to 16S rRNA amplicon analysis with multiple-comparison control (q < 0.05). The PG seawater showed an enrichment of taxa commonly associated with nutrient-enriched or impacted coastal waters (e.g., Nitrospira, Desulfovibrio, Escherichia, and Arcobacter), providing environmental context for the distinct coral-associated microbiome patterns observed at this site. At 15 months, microbiomes of transplanted JP corals were more similar to JP controls than to PG controls. These results suggest a partial, site-specific donor-origin microbiome signature and support incorporating longitudinal microbiome monitoring into translocation assessments for restoration.
珊瑚礁作为支持多种海洋生物的重要生态系统,正日益面临来自人为活动和环境变化的威胁。在这项研究中,我们分析了珊瑚迁移对珊瑚全息生物微生物组的位点特异性影响。哈氏Mussismilia hartii的珊瑚虫从一个珊瑚礁位置(Japaratinga, Alagoas, Brazil; JP)移植到95.6公里外的另一个珊瑚礁位置(Porto de Galinhas, Pernambuco; PG)。与PG相比,JP具有更高的珊瑚丰度和更大的群落大小指数。由于研究设计仅包括两个地理上不同的地点,因此解释仅限于这些地点。这项研究测试了供体-珊瑚礁起源影响地点和时间相关的纵向微生物群轨迹的假设。移植的JP珊瑚在PG 1个月后的微生物组有所不同,这与当地条件下的短期成分调整相一致,而不是生理应激的推断;α -多样性差异也被发现,并被描述性地报道,而没有归因于环境的原因。在此之后,根据16S rRNA扩增子分析和多重比较对照(q < 0.05),移植珊瑚显示出推定的共生相关属(如Ruegeria, Labrenzia和副球菌)的增加。PG海水显示出与营养丰富或受影响的沿海水域相关的分类群(如硝化螺旋菌、脱硫弧菌、埃希氏菌和Arcobacter)的富集,为该地点观察到的独特的珊瑚相关微生物群模式提供了环境背景。在15个月时,移植的JP珊瑚的微生物组与JP对照组比PG对照组更相似。这些结果表明了局部的、特定地点的供体来源微生物组特征,并支持将纵向微生物组监测纳入恢复易位评估中。
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引用次数: 0
Early Danian paleotemperature records from Neuquén Basin-Argentina: Applications of the ostracod Sr/Ca paleothermometer 阿根廷neuquacimen盆地早大年世古地温记录:介形虫Sr/Ca古地温计的应用
Pub Date : 2026-01-01 DOI: 10.1016/j.eve.2026.100113
Marlone H.H. Bom , Karlos G.D. Kochhann , Rodrigo do Monte Guerra , Daiane Ceolin , Guilherme Krahl , Luciana R.C. Duarte , Mírian L.A.F. Pacheco , Thorsten Bauersachs , Luiz Frederico Rodrigues , Flavia Callefo , Franciele Agnesa Trentin , Douglas Galante , Telma Musso , Lorenz Schwark , Andrea Concheyro , Gerson Fauth
The early Danian is marked by a recovery in marine and terrestrial ecosystems after the Cretaceous-Paleogene mass extinction. Both sea surface temperature (SST) and bottom water temperature (BWT) reconstructions are essential for a better understanding of paleoclimatic developments occurring at this critical time interval. Paleotemperature reconstructions based on ostracods are an excellent alternative for studies in regions where benthic foraminifera are scarce or absent. In this context, we present a paleotemperature reconstruction of the Cerro Azul Section, Neuquén Basin, Argentina, based on the ostracod Henryhowella (Wichmannella) meridionalis (Bertels, 1974). Trace element/calcium ratios (El/Ca) were determined on well preserved specimens using two different analytical techniques: (i) oxidative cleaning followed by acid digestion (measured with ICP OES), and (ii) laser ablation (measured with LA-ICP-MS). Our results show that El/Ca ratios of ornamented species are more effectively quantified using acid digestion. Although some intervals show high values of the Al/Ca ratio, which could suggest the presence of remaining clay and/or organic contaminants. Low values of both Fe/Ca and Mn/Ca ratios indicate efficient cleaning regarding oxyhydroxides. As the incorporation of Mg and Sr into inorganic calcite is a thermodynamic process, we mapped the distribution of both trace elements on ostracod valves in nanoscale using Synchrotron-based X-ray fluorescence (nannoXRF). Our results show that Sr/Ca has a negligible correlation with Al/Ca, and Sr appears to be more homogeneously distributed compared to Mg in Henryhowella (Wichmannella) meridionalis valves. Therefore, we opted to apply the Sr/Ca ratio as a paleothermometer in the studied Danian ostracods, consisting in the first ostracod-based BWT record for the Paleogene. Our results indicate stable BWT values throughout the studied interval at the Cerro Azul Section, ranging between 5.1 and 8.8 °C (oxidative cleaning), and 7 to 13 °C (laser ablation). BWTs show the expected offset (colder temperatures) to TEXH86 and stable oxygen isotope (δ18O)-derived SSTs, which ranged from 28.3 to 31.8 °C, with TEXH86 depicting a 2.5 °C warming between calcareous nannofossil zones AP0 and AP1a. The present study demonstrates the potential of using the elemental composition of ostracod valves as a new tool for reconstructing past deep ocean temperature variations.
大年世早期标志着白垩纪-古近纪大灭绝后海洋和陆地生态系统的恢复。海表温度(SST)和底水温(BWT)的重建对于更好地理解发生在这一关键时间间隔的古气候发展至关重要。在底栖有孔虫稀少或缺乏的地区,基于介形类的古地温重建是一个很好的选择。在此背景下,我们以介形虫Henryhowella (Wichmannella) meridionalis (Bertels, 1974)为基础,对阿根廷neuqun盆地Cerro Azul剖面进行了古温度重建。使用两种不同的分析技术(i)氧化清洗后酸消解(ICP OES测量)和(ii)激光烧蚀(LA-ICP-MS测量)对保存良好的标本进行了微量元素/钙比(El/Ca)的测定。结果表明,利用酸消化法可以更有效地量化装饰植物的El/Ca比值。虽然有些区间显示出较高的Al/Ca比值,这可能表明存在剩余的粘土和/或有机污染物。Fe/Ca和Mn/Ca比值均较低,表明对氢氧化物的清洗效果较好。由于镁和锶在无机方解石中的结合是一个热力学过程,我们利用同步辐射x射线荧光(nannoXRF)在纳米尺度上绘制了这两种微量元素在介形虫阀上的分布。我们的研究结果表明,Sr/Ca与Al/Ca的相关性可以忽略不计,与Mg相比,Sr在Henryhowella (Wichmannella) meridionalis阀中的分布更为均匀。因此,我们选择将Sr/Ca比值作为研究对象的古温度表,这是古近系首次基于介形虫的BWT记录。我们的结果表明,在Cerro Azul剖面的整个研究区间内,BWT值稳定,范围在5.1至8.8°C(氧化清洗)和7至13°C(激光烧蚀)之间。BWTs显示了对TEXH86和稳定氧同位素(δ18O)衍生海温的预期偏移(较冷的温度),范围在28.3 ~ 31.8°C之间,TEXH86描述了钙质纳米化石带AP0和AP1a之间2.5°C的升温。本研究证明了利用介形虫壳的元素组成作为重建过去深海温度变化的新工具的潜力。
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引用次数: 0
Flood susceptibility mapping in the tropical river basinof central Kerala, India, using Analytic Hierarchy Process (AHP) and geospatial techniques 基于层次分析法和地理空间技术的印度喀拉拉邦中部热带河流流域洪水易感性制图
Pub Date : 2026-01-01 DOI: 10.1016/j.eve.2026.100105
Ajayakumar Appukuttan , Kavya S. Kutty , Rajesh Reghunath , Vineetha P
Floods remain one of the most severe hydro-meteorological hazards globally, often exacerbated by rapid land-use change, geomorphic alterations, and intense rainfall in tropical regions. The Karuvannur River Basin (KRB) in central Kerala, India, has experienced frequent flood events, yet a systematic, geospatially integrated flood susceptibility assessment has been lacking. This study applies the Analytic Hierarchy Process (AHP) coupled with Geographic Information System (GIS) techniques to develop a flood susceptibility map that captures the spatial variability of flood-prone zones based on geomorphological, hydrological, and land surface parameters. A total of nine environmental variables, including slope, drainage density, land use/land cover (LULC), soil texture, and the Topographic Wetness Index (TWI), were derived from SRTM DEM, Landsat 9 OLI, Survey of India toposheets, and ancillary soil data. Model validation was carried out using National Remote Sensing Centre (NRSC) flood inundation data, and the predictive performance was evaluated using the Receiver Operating Characteristic (ROC) curve. The model achieved a high Area Under the Curve (AUC) value of 0.945, indicating excellent predictive accuracy. The AHP consistency ratio was 0.02, confirming the logical consistency of the assigned weights. The results indicate that approximately 570.38 km2 (54.9 % of the basin) fall under high and very high flood susceptibility zones, predominantly in the central and western floodplains. The study provides critical spatial insights for flood risk mitigation, landscape resilience planning, and geomorphologically informed infrastructure development, offering a replicable model for flood-prone tropical river basins.
洪水仍然是全球最严重的水文气象灾害之一,往往因土地利用的快速变化、地貌的改变和热带地区的强降雨而加剧。印度喀拉拉邦中部的Karuvannur河流域(KRB)经历了频繁的洪水事件,但缺乏系统的、地理空间一体化的洪水易感性评估。本研究应用层次分析法(AHP)和地理信息系统(GIS)技术,根据地貌、水文和地表参数,绘制洪水易发区空间变异性的洪水易发区地图。基于SRTM DEM、Landsat 9 OLI、Survey of India toposheets和辅助土壤数据,共获得9个环境变量,包括坡度、排水密度、土地利用/土地覆盖(LULC)、土壤质地和地形湿度指数(TWI)。利用国家遥感中心(NRSC)洪水淹没数据对模型进行验证,并利用受试者工作特征(ROC)曲线对模型的预测性能进行评价。该模型的曲线下面积(AUC)为0.945,预测精度较高。AHP一致性比为0.02,证实了所分配权重的逻辑一致性。结果表明:流域高、极高易发区面积约为570.38 km2(54.9%),主要分布在中西部洪泛平原;该研究为洪水风险缓解、景观恢复力规划和地貌信息基础设施开发提供了重要的空间见解,为洪水易发的热带河流流域提供了可复制的模型。
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引用次数: 0
Effectiveness and scalability of coastal nature-based solutions under climate impact drivers: A systematic review 气候影响驱动因素下沿海自然解决方案的有效性和可扩展性:系统综述
Pub Date : 2026-01-01 DOI: 10.1016/j.eve.2026.100108
Pradeep Marula Siddappanavara , Anushiya Jeganathan , P Jayashree
Nature-based Solutions (NbS) are increasingly promoted to enhance coastal resilience to climate change, yet most evaluations focus on biophysical outcomes while overlooking the project-level processes that influence long-term effectiveness and scalability. This study applies an implementation-based analytical framework to assess how coastal NbS implementation processes engaged with multiple Climate Impact Drivers (CIDs), including sea-level rise, ocean warming, storm intensity, precipitation variability, and ocean acidification.
A structured qualitative review of 117 coastal NbS studies was conducted, of which 35 were CID-relevant and only 14 contained sufficient process-level information for detailed analysis. Eight key Implementation Components (ICs)—baseline assessment, stakeholder engagement, comparative analysis, economic analysis, performance indicators, monitoring, adaptive management, scalability and replicability—were identified and analysed using Jaccard similarity indices to quantify their co-occurrence. These ICs are related to implementation planning, governance, monitoring, learning, and scalability. The ICs were further mapped to the International Union for Conservation of Nature (IUCN) Global Standard for NbS to evaluate their conceptual alignment with recognised quality criteria.
Results show that foundational and measurement ICs such as baseline assessment, monitoring, and performance indicators dominate current NbS practice, whereas learning-orientated and enabling processes—particularly comparative analysis, adaptive management, stakeholder engagement, and economic assessment—are weakly integrated. This structural imbalance limits cross-site learning, adaptive capacity, and scalability under interacting climate pressures. NbS interventions exhibiting more complete process architectures demonstrate greater alignment with IUCN criteria related to governance, feasibility, and long-term sustainability.
The study demonstrates that scalability is an emergent property of implementation-process completeness rather than a function of ecosystem type or intervention outcomes. This study establishes a quantitative-conceptual framework that integrates CIDs, ICs, and NbS Standard, offering a transferable methodology for identifying implementation deficiencies and enhancing the design of resilient, policy-relevant coastal NbS.
基于自然的解决方案(NbS)越来越多地被推广以增强沿海地区对气候变化的适应能力,但大多数评估都侧重于生物物理结果,而忽视了影响长期有效性和可扩展性的项目级过程。本研究采用基于实施的分析框架来评估沿海国家统计局实施过程如何与多种气候影响驱动因素(cid)相结合,包括海平面上升、海洋变暖、风暴强度、降水变率和海洋酸化。对117项沿海国家统计局研究进行了结构化的定性审查,其中35项与cid相关,只有14项包含足够的过程级信息以进行详细分析。八个关键实施组件(ic)——基线评估、利益相关者参与、比较分析、经济分析、绩效指标、监测、适应性管理、可扩展性和可复制性——被确定并使用Jaccard相似性指数进行分析,以量化它们的共存性。这些ic与实现计划、治理、监视、学习和可伸缩性相关。这些国家进一步被映射到国际自然保护联盟(IUCN)的国家统计局全球标准,以评估其概念与公认的质量标准的一致性。结果表明,基础ic和测量ic,如基线评估、监测和绩效指标,主导着当前的国家统计局实践,而以学习为导向和使能过程(特别是比较分析、适应性管理、利益相关者参与和经济评估)的整合程度较弱。这种结构不平衡限制了在相互作用的气候压力下的跨站点学习、适应能力和可扩展性。NbS干预措施展示了更完整的流程架构,与IUCN有关治理、可行性和长期可持续性的标准更一致。研究表明,可扩展性是实现过程完备性的一个紧急属性,而不是生态系统类型或干预结果的函数。本研究建立了一个量化概念框架,整合了CIDs、ic和NbS标准,为识别实施缺陷和加强弹性、政策相关的沿海NbS设计提供了一种可转移的方法。
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引用次数: 0
Groundwater quality assessments of phreatic and deeper aquifers of the eastern Palghat, Kerala, Southern India 印度南部喀拉拉邦帕尔加特东部深层含水层的地下水质量评估
Pub Date : 2025-12-24 DOI: 10.1016/j.eve.2025.100104
K.V. Sarath , E. Shaji , M. Thirumurugan , S.G. Dhanil Dev , G. Indu , Ashitha , Keerthana
Identification and management of groundwater quality is crucial for maintaining the resources of over-exploited areas in the rain shadow region of the hard rock aquifer, which is essential for sustainable development. This research aims to identify water quality analysis for drinking and agricultural harvest in the crystalline aquifer, located in the eastern Palghat, Kerala, southern India. A groundwater compatibility study was conducted by analysing in situ parameters, major cations, anions, macronutrients, and fluorine in groundwater. Irrigational water quality parameters like Soluble Sodium Percentage (SSP), Sodium Adsorption Ratio (SAR), and Kelly's Ratio (KR), Permeability Index (PI) and Magnesium Hazard were obtained from 48 samples, 24 from excavated wells and 24 from tube wells (TW) in the exact location. The Water Quality Index (WQI) and irrigation water quality (IWQ) index are utilised due to their high importance in identifying the quality of water resources for irrigation and drinking purposes. Groundwater is the essential source for domestic, agricultural, and industrial purposes in the eastern Palghat, Kerala, southern India. This paper presents geochemical analyses of groundwater collected from phreatic and deeper aquifers of the area. Groundwater quality analyses show a considerable difference in the groundwater chemistry of phreatic and deeper aquifers. Excess fluoride is noted in a few samples. Rainwater harvesting, nanotechnology-based filters and awareness programs are recommended for reliable groundwater management in the study area.
地下水质量的识别和管理对维持硬岩含水层雨影区过度开发地区的资源至关重要,对可持续发展至关重要。本研究旨在确定位于印度南部喀拉拉邦帕尔加特东部的结晶含水层的饮用水和农业收获水质分析。通过分析地下水中的原位参数、主要阳离子、阴离子、常量营养素和氟,进行了地下水相容性研究。选取48个样品,其中开挖井24个,管井24个,获得了灌溉水的可溶性钠含量(SSP)、钠吸附比(SAR)、凯利比(KR)、渗透率指数(PI)、镁危害等水质参数。使用水质指数(WQI)和灌溉水质指数(IWQ)是因为它们在确定用于灌溉和饮用的水资源质量方面非常重要。地下水是印度南部喀拉拉邦东部帕尔加特地区家庭、农业和工业的重要水源。本文介绍了从该地区的深层和深层含水层收集的地下水的地球化学分析。地下水水质分析表明,深层含水层和深层含水层的地下水化学成分有相当大的差异。在一些样品中发现了过量的氟化物。雨水收集、基于纳米技术的过滤器和意识项目被推荐用于研究区域可靠的地下水管理。
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Evolving Earth
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