首页 > 最新文献

地球科学最新文献

英文 中文
IF:
Extreme heat disproportionately exacerbates health issues by threatening fresh food supply
IF 30.7 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-23 DOI: 10.1038/s41558-024-02172-2
Yin Long, Yoshikuni Yoshida, Yuya Kajikawa
Record-breaking temperatures pose critical risks to the global food supply, particularly endangering fresh produce. Urgent enhancements in food safety measures, including re-evaluating the impact of food production, improving cold chain logistics and adapting dietary practices, are required to ensure the resilience of food systems and public health.
{"title":"Extreme heat disproportionately exacerbates health issues by threatening fresh food supply","authors":"Yin Long, Yoshikuni Yoshida, Yuya Kajikawa","doi":"10.1038/s41558-024-02172-2","DOIUrl":"https://doi.org/10.1038/s41558-024-02172-2","url":null,"abstract":"Record-breaking temperatures pose critical risks to the global food supply, particularly endangering fresh produce. Urgent enhancements in food safety measures, including re-evaluating the impact of food production, improving cold chain logistics and adapting dietary practices, are required to ensure the resilience of food systems and public health.","PeriodicalId":18974,"journal":{"name":"Nature Climate Change","volume":null,"pages":null},"PeriodicalIF":30.7,"publicationDate":"2024-10-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142487083","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Sediment Transport and Flood Risk: Impact of Newly Constructed Embankments on River Morphology and Flood Dynamics in Kathmandu, Nepal 沉积物迁移与洪水风险:新建堤坝对尼泊尔加德满都河流形态和洪水动态的影响
IF 5.4 1区 地球科学 Q2 ENVIRONMENTAL SCIENCES Pub Date : 2024-10-22 DOI: 10.1029/2024wr037742
Saraswati Thapa, Hugh D. Sinclair, Maggie J. Creed, Alistair G. L. Borthwick, C. Scott Watson, Manoranjan Muthusamy
Floodplain encroachment by embankments heightens flood risk. This is exacerbated by climate change and land-use modifications. This paper assesses the impact of embankments on sediment transport, channel geometry, conveyance capacity, and flood inundation of a reach of the Nakkhu River, Nepal. Using the CAESAR-Lisflood landscape evolution model based on a 2-m digital elevation model, we simulate four flood scenarios with and without embankments and sediment transport: a historical 25-year return period flood event used to design the embankments, 50-year, 100-year, and 1000-year return period flood events forecast using the Generalized Logistic Model (using data from 1992 to 2017). Our results indicate that flow confinement by embankments reduces inundation by 99% (from 22.5 to 0.3 ha) for the historical 25-year flood discharge of 42.23 <span data-altimg="/cms/asset/e8aa5bf6-5a8c-4281-ae9f-df9d782c62f2/wrcr27519-math-0001.png"></span><mjx-container ctxtmenu_counter="85" ctxtmenu_oldtabindex="1" jax="CHTML" role="application" sre-explorer- style="font-size: 103%; position: relative;" tabindex="0"><mjx-math aria-hidden="true" location="graphic/wrcr27519-math-0001.png"><mjx-semantics><mjx-mrow data-semantic-children="2,4" data-semantic-content="3" data-semantic- data-semantic-role="division" data-semantic-speech="normal m cubed divided by normal s" data-semantic-type="infixop"><mjx-msup data-semantic-children="0,1" data-semantic- data-semantic-parent="5" data-semantic-role="latinletter" data-semantic-type="superscript"><mjx-mi data-semantic-annotation="clearspeak:simple" data-semantic-font="normal" data-semantic- data-semantic-parent="2" data-semantic-role="latinletter" data-semantic-type="identifier"><mjx-c></mjx-c></mjx-mi><mjx-script style="vertical-align: 0.363em;"><mjx-mn data-semantic-annotation="clearspeak:simple" data-semantic-font="normal" data-semantic- data-semantic-parent="2" data-semantic-role="integer" data-semantic-type="number" size="s"><mjx-c></mjx-c></mjx-mn></mjx-script></mjx-msup><mjx-mo data-semantic- data-semantic-operator="infixop,/" data-semantic-parent="5" data-semantic-role="division" data-semantic-type="operator" rspace="1" space="1"><mjx-c></mjx-c></mjx-mo><mjx-mi data-semantic-annotation="clearspeak:simple" data-semantic-font="normal" data-semantic- data-semantic-parent="5" data-semantic-role="latinletter" data-semantic-type="identifier"><mjx-c></mjx-c></mjx-mi></mjx-mrow></mjx-semantics></mjx-math><mjx-assistive-mml display="inline" unselectable="on"><math altimg="urn:x-wiley:00431397:media:wrcr27519:wrcr27519-math-0001" display="inline" location="graphic/wrcr27519-math-0001.png" xmlns="http://www.w3.org/1998/Math/MathML"><semantics><mrow data-semantic-="" data-semantic-children="2,4" data-semantic-content="3" data-semantic-role="division" data-semantic-speech="normal m cubed divided by normal s" data-semantic-type="infixop"><msup data-semantic-="" data-semantic-children="0,1" data-semantic-parent="5" data-semantic-role=
堤坝对洪泛区的侵占加剧了洪水风险。气候变化和土地使用的改变加剧了这种情况。本文评估了堤坝对沉积物输运、河道几何形状、输送能力以及尼泊尔纳库河某河段洪水淹没的影响。利用基于 2 米数字高程模型的 CAESAR-Lisflood 景观演变模型,我们模拟了有堤防和无堤防以及泥沙输运的四种洪水情景:用于设计堤防的 25 年一遇历史洪水,利用广义逻辑模型预测的 50 年一遇、100 年一遇和 1000 年一遇洪水(使用 1992 年至 2017 年的数据)。我们的研究结果表明,对于历史上 25 年一遇的 42.23 m3/s${mathrm{m}}^{3}//mathrm{s}$的情况下,洪水淹没面积减少了 15%(从 28.8 公顷减少到 24.4 公顷);1000 年重现期洪水排放量为 95 m3/s${mathrm{m}}^{3}/mathrm{s}$(类似于 25 年最大中洪水)的情况下,洪水淹没面积减少了 15%(从 28.8 公顷减少到 24.4 公顷)。在考虑的所有洪水情景中,堤坝的存在都会使下游泥沙输移增加 32% 以上。与无沉积物情况相比,在有堤防的河道中,沉积物运移导致 25 年一遇的未来中期最大洪水的预测淹没面积增加了五倍。沉积作用导致的河道几何形状变化大大降低了河道的输送能力,增加了倾覆洪水的风险,尤其是在河道蜿蜒曲折或地势平坦的情况下。我们的研究结果表明,外侧蜿蜒处的泥沙侵蚀可能会促进下切,从而威胁堤坝的稳定性。建议在堤坝设计和洪泛区规划中考虑泥沙输移的影响。
{"title":"Sediment Transport and Flood Risk: Impact of Newly Constructed Embankments on River Morphology and Flood Dynamics in Kathmandu, Nepal","authors":"Saraswati Thapa, Hugh D. Sinclair, Maggie J. Creed, Alistair G. L. Borthwick, C. Scott Watson, Manoranjan Muthusamy","doi":"10.1029/2024wr037742","DOIUrl":"https://doi.org/10.1029/2024wr037742","url":null,"abstract":"Floodplain encroachment by embankments heightens flood risk. This is exacerbated by climate change and land-use modifications. This paper assesses the impact of embankments on sediment transport, channel geometry, conveyance capacity, and flood inundation of a reach of the Nakkhu River, Nepal. Using the CAESAR-Lisflood landscape evolution model based on a 2-m digital elevation model, we simulate four flood scenarios with and without embankments and sediment transport: a historical 25-year return period flood event used to design the embankments, 50-year, 100-year, and 1000-year return period flood events forecast using the Generalized Logistic Model (using data from 1992 to 2017). Our results indicate that flow confinement by embankments reduces inundation by 99% (from 22.5 to 0.3 ha) for the historical 25-year flood discharge of 42.23 &lt;span data-altimg=\"/cms/asset/e8aa5bf6-5a8c-4281-ae9f-df9d782c62f2/wrcr27519-math-0001.png\"&gt;&lt;/span&gt;&lt;mjx-container ctxtmenu_counter=\"85\" ctxtmenu_oldtabindex=\"1\" jax=\"CHTML\" role=\"application\" sre-explorer- style=\"font-size: 103%; position: relative;\" tabindex=\"0\"&gt;&lt;mjx-math aria-hidden=\"true\" location=\"graphic/wrcr27519-math-0001.png\"&gt;&lt;mjx-semantics&gt;&lt;mjx-mrow data-semantic-children=\"2,4\" data-semantic-content=\"3\" data-semantic- data-semantic-role=\"division\" data-semantic-speech=\"normal m cubed divided by normal s\" data-semantic-type=\"infixop\"&gt;&lt;mjx-msup data-semantic-children=\"0,1\" data-semantic- data-semantic-parent=\"5\" data-semantic-role=\"latinletter\" data-semantic-type=\"superscript\"&gt;&lt;mjx-mi data-semantic-annotation=\"clearspeak:simple\" data-semantic-font=\"normal\" data-semantic- data-semantic-parent=\"2\" data-semantic-role=\"latinletter\" data-semantic-type=\"identifier\"&gt;&lt;mjx-c&gt;&lt;/mjx-c&gt;&lt;/mjx-mi&gt;&lt;mjx-script style=\"vertical-align: 0.363em;\"&gt;&lt;mjx-mn data-semantic-annotation=\"clearspeak:simple\" data-semantic-font=\"normal\" data-semantic- data-semantic-parent=\"2\" data-semantic-role=\"integer\" data-semantic-type=\"number\" size=\"s\"&gt;&lt;mjx-c&gt;&lt;/mjx-c&gt;&lt;/mjx-mn&gt;&lt;/mjx-script&gt;&lt;/mjx-msup&gt;&lt;mjx-mo data-semantic- data-semantic-operator=\"infixop,/\" data-semantic-parent=\"5\" data-semantic-role=\"division\" data-semantic-type=\"operator\" rspace=\"1\" space=\"1\"&gt;&lt;mjx-c&gt;&lt;/mjx-c&gt;&lt;/mjx-mo&gt;&lt;mjx-mi data-semantic-annotation=\"clearspeak:simple\" data-semantic-font=\"normal\" data-semantic- data-semantic-parent=\"5\" data-semantic-role=\"latinletter\" data-semantic-type=\"identifier\"&gt;&lt;mjx-c&gt;&lt;/mjx-c&gt;&lt;/mjx-mi&gt;&lt;/mjx-mrow&gt;&lt;/mjx-semantics&gt;&lt;/mjx-math&gt;&lt;mjx-assistive-mml display=\"inline\" unselectable=\"on\"&gt;&lt;math altimg=\"urn:x-wiley:00431397:media:wrcr27519:wrcr27519-math-0001\" display=\"inline\" location=\"graphic/wrcr27519-math-0001.png\" xmlns=\"http://www.w3.org/1998/Math/MathML\"&gt;&lt;semantics&gt;&lt;mrow data-semantic-=\"\" data-semantic-children=\"2,4\" data-semantic-content=\"3\" data-semantic-role=\"division\" data-semantic-speech=\"normal m cubed divided by normal s\" data-semantic-type=\"infixop\"&gt;&lt;msup data-semantic-=\"\" data-semantic-children=\"0,1\" data-semantic-parent=\"5\" data-semantic-role=","PeriodicalId":23799,"journal":{"name":"Water Resources Research","volume":null,"pages":null},"PeriodicalIF":5.4,"publicationDate":"2024-10-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142486402","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Plant and Microbial Carbon Are Important Drivers of Free-Living Nitrogen Fixation in Tropical Forest Soils: A New Discovery of Carbon-Driven Nitrogen Input 植物碳和微生物碳是热带森林土壤自由固氮的重要驱动力:碳驱动氮输入的新发现
IF 5.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-10-22 DOI: 10.1029/2024gl111238
Meichen Xu, Linjie Fan, Andi Li, Qiyan Liu, Guangcan Yu, Senhao Wang, Baixin Zhang, Qing Ye, Jiangming Mo, Mianhai Zheng
Nitrogen (N) availability limits plant growth and soil carbon (C) sequestration in N-limited ecosystems, however, plant and soil C feedback on the free-living nitrogen fixation (FLNF) process is poorly understood. Moreover, whether this feedback is influenced by initial N availability in leguminous and non-leguminous forest soils has not been clarified. Here, we found that the addition of plant- and microbial-derived C significantly enhanced soil nitrogenase activity (13∼28%) and that microbial-derived C had a more positive impact. These positive effects were attributed to the direct C-energy supply (0.49∼0.84) rather than variations in soil microbial activity (−0.01∼0.21) and substrate resources (−0.45∼0.27). Long-term N addition did not inhibit FLNF. C addition promoted FLNF in soils of the two forests, but the response rate was higher in the leguminous forest soils. Our study reveals that increased soil C availability can drive FLNF in tropical forests, enhancing our understanding of the soil C-N coupling mechanism.
氮(N)的可用性限制了氮有限生态系统中植物的生长和土壤碳(C)的固存,然而,人们对植物和土壤碳对自由生活固氮(FLNF)过程的反馈作用知之甚少。此外,这种反馈是否受豆科植物和非豆科植物森林土壤中初始氮供应量的影响也尚未明确。在这里,我们发现添加植物和微生物源 C 能显著提高土壤氮酶活性(13∼28%),而微生物源 C 的影响更为积极。这些积极影响归因于直接的碳能量供应(0.49∼0.84),而不是土壤微生物活性(-0.01∼0.21)和基质资源(-0.45∼0.27)的变化。长期添加氮并不抑制FLNF。在两种森林土壤中,添加 C 都能促进 FLNF,但豆科森林土壤的响应率更高。我们的研究揭示了土壤碳供应量的增加可以驱动热带森林的FLNF,从而加深了我们对土壤C-N耦合机制的理解。
{"title":"Plant and Microbial Carbon Are Important Drivers of Free-Living Nitrogen Fixation in Tropical Forest Soils: A New Discovery of Carbon-Driven Nitrogen Input","authors":"Meichen Xu, Linjie Fan, Andi Li, Qiyan Liu, Guangcan Yu, Senhao Wang, Baixin Zhang, Qing Ye, Jiangming Mo, Mianhai Zheng","doi":"10.1029/2024gl111238","DOIUrl":"https://doi.org/10.1029/2024gl111238","url":null,"abstract":"Nitrogen (N) availability limits plant growth and soil carbon (C) sequestration in N-limited ecosystems, however, plant and soil C feedback on the free-living nitrogen fixation (FLNF) process is poorly understood. Moreover, whether this feedback is influenced by initial N availability in leguminous and non-leguminous forest soils has not been clarified. Here, we found that the addition of plant- and microbial-derived C significantly enhanced soil nitrogenase activity (13∼28%) and that microbial-derived C had a more positive impact. These positive effects were attributed to the direct C-energy supply (0.49∼0.84) rather than variations in soil microbial activity (−0.01∼0.21) and substrate resources (−0.45∼0.27). Long-term N addition did not inhibit FLNF. C addition promoted FLNF in soils of the two forests, but the response rate was higher in the leguminous forest soils. Our study reveals that increased soil C availability can drive FLNF in tropical forests, enhancing our understanding of the soil C-N coupling mechanism.","PeriodicalId":12523,"journal":{"name":"Geophysical Research Letters","volume":null,"pages":null},"PeriodicalIF":5.2,"publicationDate":"2024-10-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142486440","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Convectively Induced Secondary Circulations and Wind-Driven Heat Fluxes in the Surface Energy Balance Over Land 陆地地表能量平衡中对流诱发的次级环流和风驱动的热通量
IF 5.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-10-22 DOI: 10.1029/2024gl110565
Seth Colston, Ian N. Williams
Increased resolution has enabled kilometer-scale weather and climate models to partially resolve secondary circulations, including horizontal convective rolls (HCRs) and cold pool gust fronts. Although these circulations are ubiquitous in convective boundary layers over land, their impacts on the surface energy balance are largely unknown. Doppler lidar and surface observations were combined with DOE E3SM land model experiments, revealing increased surface winds (5 m/s) and heat fluxes (50 W/m2) in convergent branches of HCRs. Larger wind-driven flux responses (up to 150 W/m2) were found along gust fronts. Surface energy balance shifts to accommodate wind-driven fluxes, reducing ground heat conduction and longwave cooling. Our findings from the US Southern Great Plains are broadly relevant to modeling convective boundary layers. In particular, widely used subgrid wind gust parameterizations were found to be physically inconsistent with resolved secondary circulations and could worsen climate prediction biases at kilometer-scales.
分辨率的提高使得千米尺度的天气和气候模式能够部分解析次级环流,包括水平对流卷(HCR)和冷池阵风锋。虽然这些环流在陆地对流边界层中无处不在,但它们对地表能量平衡的影响在很大程度上是未知的。多普勒激光雷达和地表观测数据与 DOE E3SM 陆地模式实验相结合,揭示了在 HCR 的汇聚分支中增加的地表风(5 米/秒)和热通量(50 瓦/平方米)。在阵风前沿发现了更大的风驱动通量响应(高达 150 W/m2)。地表能量平衡为适应风驱动通量而改变,从而减少了地面热传导和长波冷却。我们在美国南部大平原的研究结果与对流边界层建模具有广泛的相关性。特别是,我们发现广泛使用的子网格阵风参数与解析的次级环流在物理上不一致,可能会加剧千米尺度的气候预测偏差。
{"title":"Convectively Induced Secondary Circulations and Wind-Driven Heat Fluxes in the Surface Energy Balance Over Land","authors":"Seth Colston, Ian N. Williams","doi":"10.1029/2024gl110565","DOIUrl":"https://doi.org/10.1029/2024gl110565","url":null,"abstract":"Increased resolution has enabled kilometer-scale weather and climate models to partially resolve secondary circulations, including horizontal convective rolls (HCRs) and cold pool gust fronts. Although these circulations are ubiquitous in convective boundary layers over land, their impacts on the surface energy balance are largely unknown. Doppler lidar and surface observations were combined with DOE E3SM land model experiments, revealing increased surface winds (5 m/s) and heat fluxes (50 W/m<sup>2</sup>) in convergent branches of HCRs. Larger wind-driven flux responses (up to 150 W/m<sup>2</sup>) were found along gust fronts. Surface energy balance shifts to accommodate wind-driven fluxes, reducing ground heat conduction and longwave cooling. Our findings from the US Southern Great Plains are broadly relevant to modeling convective boundary layers. In particular, widely used subgrid wind gust parameterizations were found to be physically inconsistent with resolved secondary circulations and could worsen climate prediction biases at kilometer-scales.","PeriodicalId":12523,"journal":{"name":"Geophysical Research Letters","volume":null,"pages":null},"PeriodicalIF":5.2,"publicationDate":"2024-10-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142486413","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Present-day crustal deformation based on an interpolated GPS velocity field in the collision zone of the Arabia-Eurasia tectonic plates 基于阿拉伯-欧亚大陆板块碰撞带全球定位系统插值速度场的现今地壳形变
IF 0.5 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-10-22 DOI: 10.1007/s11200-023-0740-5
Asghar Rastbood, Milad Salmanian, Masoud Mashhadi Hossainali

The oblique collision zone of Arabia-Eurasia is a seismically active region with complex crustal deformation patterns. While GPS measurements provide valuable data, their sparse distribution limits our understanding of the full extent of deformation. This study addresses this limitation by using a robust interpolation method for GPS velocity data in the collision zone. We utilized biharmonic splines to interpolate horizontal components of sparse GPS velocity data independently and in a coupled manner by altering Poisson ratio. This method is an effective means of interpolating sparse vector data in cases where deformation mechanics can be explained by elasticity principles. The interpolation process included fitting trends to the input data, calculating residuals, and analyzing them. The prediction process consisted of trend and spline fitting stages. We interpolate horizontal GPS velocities onto a standard geographic grid with a 30-minute interval, excluding data points with significant deviation. The data was partitioned into training and testing subsets, with the training set used for calibration and the testing set for evaluation of the interpolation method. Our analysis revealed an irregular spatial distribution of crustal movement. The northern component of the velocity field consistently points towards Eurasia and is greater than the eastern component. The amplitude of the northern component decreases from south to north and from west to east, indicating variations in deformation intensity. The eastern component exhibits a change in direction, moving westward in the western half of Iran and eastward in the eastern half, with a reversed trend in the north. This change in direction highlights the presence of solid blocks within the collision zone. Undeformed regions, major faults, convergence deformation, and compressing high-elevation regions are also observed in the collision zone. These findings provide a detailed picture of present-day crustal deformation in the Arabia-Eurasia collision zone, enhancing our understanding of the collision process.

阿拉伯-欧亚大陆斜向碰撞带是一个地震活跃地区,地壳变形模式复杂。虽然全球定位系统测量提供了宝贵的数据,但其稀疏的分布限制了我们对形变全部范围的了解。本研究通过对碰撞区的 GPS 速度数据采用稳健的内插法来解决这一局限性。我们利用双谐波曲线对稀疏的 GPS 速度数据的水平分量进行独立插值,并通过改变泊松比对其进行耦合插值。在变形力学可以用弹性原理解释的情况下,这种方法是对稀疏矢量数据进行插值的有效手段。插值过程包括对输入数据进行趋势拟合、计算残差和分析。预测过程包括趋势和样条拟合阶段。我们将全球定位系统的水平速度插值到标准地理网格上,间隔时间为 30 分钟,排除了有明显偏差的数据点。数据分为训练和测试子集,训练集用于校准,测试集用于评估插值方法。我们的分析表明,地壳运动的空间分布不规则。速度场的北部分量始终指向欧亚大陆,且大于东部分量。北部分量的振幅自南向北和自西向东逐渐减小,显示了变形强度的变化。东部分量的方向发生了变化,在伊朗的西半部向西移动,在东半部向东移动,在北部的趋势相反。这种方向的变化凸显了碰撞区内固体块的存在。在碰撞带还观察到未变形区域、主要断层、汇聚变形和压缩高海拔区域。这些发现提供了阿拉伯-欧亚大陆碰撞带当今地壳变形的详细情况,加深了我们对碰撞过程的了解。
{"title":"Present-day crustal deformation based on an interpolated GPS velocity field in the collision zone of the Arabia-Eurasia tectonic plates","authors":"Asghar Rastbood,&nbsp;Milad Salmanian,&nbsp;Masoud Mashhadi Hossainali","doi":"10.1007/s11200-023-0740-5","DOIUrl":"10.1007/s11200-023-0740-5","url":null,"abstract":"<div><p>The oblique collision zone of Arabia-Eurasia is a seismically active region with complex crustal deformation patterns. While GPS measurements provide valuable data, their sparse distribution limits our understanding of the full extent of deformation. This study addresses this limitation by using a robust interpolation method for GPS velocity data in the collision zone. We utilized biharmonic splines to interpolate horizontal components of sparse GPS velocity data independently and in a coupled manner by altering Poisson ratio. This method is an effective means of interpolating sparse vector data in cases where deformation mechanics can be explained by elasticity principles. The interpolation process included fitting trends to the input data, calculating residuals, and analyzing them. The prediction process consisted of trend and spline fitting stages. We interpolate horizontal GPS velocities onto a standard geographic grid with a 30-minute interval, excluding data points with significant deviation. The data was partitioned into training and testing subsets, with the training set used for calibration and the testing set for evaluation of the interpolation method. Our analysis revealed an irregular spatial distribution of crustal movement. The northern component of the velocity field consistently points towards Eurasia and is greater than the eastern component. The amplitude of the northern component decreases from south to north and from west to east, indicating variations in deformation intensity. The eastern component exhibits a change in direction, moving westward in the western half of Iran and eastward in the eastern half, with a reversed trend in the north. This change in direction highlights the presence of solid blocks within the collision zone. Undeformed regions, major faults, convergence deformation, and compressing high-elevation regions are also observed in the collision zone. These findings provide a detailed picture of present-day crustal deformation in the Arabia-Eurasia collision zone, enhancing our understanding of the collision process.</p></div>","PeriodicalId":22001,"journal":{"name":"Studia Geophysica et Geodaetica","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2024-10-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142453034","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Identification of chemically altered cut marks: an experimental approach from Geometrics Morphometrics 化学蚀刻痕迹的识别:《几何形态计量学》的实验方法
IF 2.1 2区 地球科学 Q1 ANTHROPOLOGY Pub Date : 2024-10-22 DOI: 10.1007/s12520-024-02091-5
David Rodríguez de la Fuente, Lloyd A. Courtenay, Darío Herranz-Rodrigo, Jose Yravedra, Antonio Pineda

Cut marks are striae accidentally produced by the contact made between the edge of a cutting tool and bone surfaces by anthropogenic activity, presenting evidence of hominin carcass processing and behaviour, butchery activities or diet. Post-depositional processes can cause the alteration (chemical or mechanical) of bones surfaces, changing their composition and causing the modification of bone surfaces. Previous research has addressed the problem of chemical alteration from a qualitative perspective, resulting in the loss of all diagnostic characteristics of the cut marks affected by these processes. Geometrics Morphometrics has led to great progress in the study of cut marks from a quantitative perspective and can be useful for the study of altered cut marks. In this study, an experiment was carried out in which 36 cut marks were reproduced and chemically altered. These marks were scanned and digitized before and after each phase of alteration. They were analyzed metrically as well as using Geometric Morphometrics, in order to study the evolution of modifications to cut mark morphology during the experiment. Results show clear morphological differences between the different phases of alteration with altered cut marks presenting a general tendency towards a decrease in both the width and depth over time. Research of this type opens up a new path for the study of the chemical alteration of cut marks, as well as other striae, through the application of Geometric Morphometrics.

切痕是人类活动中切削工具的边缘与骨骼表面接触而意外产生的条纹,是人类尸体加工和行为、屠宰活动或饮食的证据。沉积后过程可导致骨骼表面发生(化学或机械)改变,改变其成分并导致骨骼表面的改变。以往的研究都是从定性的角度来解决化学变化的问题,结果是受这些过程影响的切割痕迹丧失了所有的诊断特征。几何形态计量学在从定量角度研究切痕方面取得了巨大进步,可用于研究改变的切痕。在这项研究中,我们进行了一项实验,对 36 个切割痕迹进行了复制和化学改变。在每个改变阶段之前和之后,都对这些痕迹进行了扫描和数字化。为了研究实验过程中切割痕迹形态的变化情况,我们对这些痕迹进行了计量分析和几何形态计量学分析。结果显示,不同改造阶段的切痕形态差异明显,随着时间的推移,切痕的宽度和深度普遍呈下降趋势。此类研究为应用几何形态计量学研究切痕以及其他条纹的化学变化开辟了一条新路。
{"title":"Identification of chemically altered cut marks: an experimental approach from Geometrics Morphometrics","authors":"David Rodríguez de la Fuente,&nbsp;Lloyd A. Courtenay,&nbsp;Darío Herranz-Rodrigo,&nbsp;Jose Yravedra,&nbsp;Antonio Pineda","doi":"10.1007/s12520-024-02091-5","DOIUrl":"10.1007/s12520-024-02091-5","url":null,"abstract":"<div><p>Cut marks are striae accidentally produced by the contact made between the edge of a cutting tool and bone surfaces by anthropogenic activity, presenting evidence of hominin carcass processing and behaviour, butchery activities or diet. Post-depositional processes can cause the alteration (chemical or mechanical) of bones surfaces, changing their composition and causing the modification of bone surfaces. Previous research has addressed the problem of chemical alteration from a qualitative perspective, resulting in the loss of all diagnostic characteristics of the cut marks affected by these processes. Geometrics Morphometrics has led to great progress in the study of cut marks from a quantitative perspective and can be useful for the study of altered cut marks. In this study, an experiment was carried out in which 36 cut marks were reproduced and chemically altered. These marks were scanned and digitized before and after each phase of alteration. They were analyzed metrically as well as using Geometric Morphometrics, in order to study the evolution of modifications to cut mark morphology during the experiment. Results show clear morphological differences between the different phases of alteration with altered cut marks presenting a general tendency towards a decrease in both the width and depth over time. Research of this type opens up a new path for the study of the chemical alteration of cut marks, as well as other striae, through the application of Geometric Morphometrics.</p></div>","PeriodicalId":8214,"journal":{"name":"Archaeological and Anthropological Sciences","volume":null,"pages":null},"PeriodicalIF":2.1,"publicationDate":"2024-10-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s12520-024-02091-5.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142452896","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}
引用次数: 0
Exploring multiyear-to-decadal North Atlantic sea level predictability and prediction using machine learning 利用机器学习探索多年至十年北大西洋海平面的可预测性和预测性
IF 9 1区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2024-10-22 DOI: 10.1038/s41612-024-00802-2
Qinxue Gu, Liping Zhang, Liwei Jia, Thomas L. Delworth, Xiaosong Yang, Fanrong Zeng, William F. Cooke, Shouwei Li

Coastal communities face substantial risks from long-term sea level rise and decadal sea level variations, with the North Atlantic and U.S. East Coast being particularly vulnerable under changing climates. Employing a self-organizing map-based framework, we assess the North Atlantic sea level variability and predictability using 5000-year sea level anomalies (SLA) from two preindustrial control model simulations. Preferred transitions among patterns of variability are identified, revealing long-term predictability on decadal timescales related to shifts in Atlantic meridional overturning circulation phases. Combining this framework with model-analog techniques, we demonstrate prediction skill of large-scale SLA patterns and low-frequency coastal SLA variations comparable to that from initialized hindcasts. Moreover, additional short-term predictability is identified after the exclusion of low-frequency signals, which arises from slow gyre circulation adjustment triggered by the North Atlantic Oscillation-like stochastic variability. This study highlights the potential of machine learning to assess sources of predictability and to enable long-term climate prediction.

{"title":"Exploring multiyear-to-decadal North Atlantic sea level predictability and prediction using machine learning","authors":"Qinxue Gu, Liping Zhang, Liwei Jia, Thomas L. Delworth, Xiaosong Yang, Fanrong Zeng, William F. Cooke, Shouwei Li","doi":"10.1038/s41612-024-00802-2","DOIUrl":"https://doi.org/10.1038/s41612-024-00802-2","url":null,"abstract":"<p>Coastal communities face substantial risks from long-term sea level rise and decadal sea level variations, with the North Atlantic and U.S. East Coast being particularly vulnerable under changing climates. Employing a self-organizing map-based framework, we assess the North Atlantic sea level variability and predictability using 5000-year sea level anomalies (SLA) from two preindustrial control model simulations. Preferred transitions among patterns of variability are identified, revealing long-term predictability on decadal timescales related to shifts in Atlantic meridional overturning circulation phases. Combining this framework with model-analog techniques, we demonstrate prediction skill of large-scale SLA patterns and low-frequency coastal SLA variations comparable to that from initialized hindcasts. Moreover, additional short-term predictability is identified after the exclusion of low-frequency signals, which arises from slow gyre circulation adjustment triggered by the North Atlantic Oscillation-like stochastic variability. This study highlights the potential of machine learning to assess sources of predictability and to enable long-term climate prediction.</p>","PeriodicalId":19438,"journal":{"name":"npj Climate and Atmospheric Science","volume":null,"pages":null},"PeriodicalIF":9.0,"publicationDate":"2024-10-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142486756","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Madden Julian Oscillation Moves Faster as the Meridional Moisture Gradient Intensifies in a Warming World 在气候变暖的世界中,随着经向水分梯度的加剧,马登-朱利安涛动的移动速度也加快了
IF 5.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2024-10-22 DOI: 10.1029/2024gl110461
Panini Dasgupta, M. K. Roxy, SungHyun Nam, A. G. Prajeesh, J. S. Saranya, Chidong Zhang, Jian Ling, Daehyun Kim
The eastward-moving large-scale convective system associated with the Madden-Julian Oscillation (MJO) significantly impact global weather and climate. Recent decades have seen notable changes in the MJO's lifecycle due to non-uniform tropical ocean warming, with the roles of natural climate variability and anthropogenic influence still requiring quantification. This study examines observed and projected long-term changes in the MJO phase speed using four twentieth-century reanalyses and CMIP6 simulations. We find a substantial increase in MJO phase speed in three reanalyses during the twentieth century (0.6–1.2 m s⁻1 century⁻1) and further increase in MJO phase speed during the twenty-first century (0.3–1.5 m s⁻1 century⁻1), with notable multidecadal fluctuations. We attribute the overall acceleration of the MJO to the global warming-driven increase in the meridional moisture gradient around the warm pool while attributing the multidecadal variability in the MJO phase speed to changes in the zonal moisture gradient associated with the Pacific Decadal Oscillation.
{"title":"Madden Julian Oscillation Moves Faster as the Meridional Moisture Gradient Intensifies in a Warming World","authors":"Panini Dasgupta, M. K. Roxy, SungHyun Nam, A. G. Prajeesh, J. S. Saranya, Chidong Zhang, Jian Ling, Daehyun Kim","doi":"10.1029/2024gl110461","DOIUrl":"https://doi.org/10.1029/2024gl110461","url":null,"abstract":"The eastward-moving large-scale convective system associated with the Madden-Julian Oscillation (MJO) significantly impact global weather and climate. Recent decades have seen notable changes in the MJO's lifecycle due to non-uniform tropical ocean warming, with the roles of natural climate variability and anthropogenic influence still requiring quantification. This study examines observed and projected long-term changes in the MJO phase speed using four twentieth-century reanalyses and CMIP6 simulations. We find a substantial increase in MJO phase speed in three reanalyses during the twentieth century (0.6–1.2 m s⁻<sup>1</sup> century⁻<sup>1</sup>) and further increase in MJO phase speed during the twenty-first century (0.3–1.5 m s⁻<sup>1</sup> century⁻<sup>1</sup>), with notable multidecadal fluctuations. We attribute the overall acceleration of the MJO to the global warming-driven increase in the meridional moisture gradient around the warm pool while attributing the multidecadal variability in the MJO phase speed to changes in the zonal moisture gradient associated with the Pacific Decadal Oscillation.","PeriodicalId":12523,"journal":{"name":"Geophysical Research Letters","volume":null,"pages":null},"PeriodicalIF":5.2,"publicationDate":"2024-10-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142486463","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Seismic Evidence for Velocity Heterogeneity Along ∼40 Ma Old Oceanic Crustal Segment Formed at the Slow-Spreading Equatorial Mid-Atlantic Ridge From Full Waveform Inversion of Ocean Bottom Seismometer Data 从海底地震仪数据的全波形反演中获得在大西洋中脊缓慢扩张的赤道海域形成的 ∼40 Ma 旧大洋地壳段沿线速度异质性的地震证据
IF 3.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2024-10-22 DOI: 10.1029/2024jb029776
Peng Guo, Satish C. Singh
In slow spreading environments, oceanic crust is formed by a combination of magmatic and tectonic processes. Using full waveform inversion applied to active-source ocean bottom seismometer data, we reveal the presence of a strong lateral variability in the 40–48 Ma old oceanic crust formed at the slow-spreading Mid-Atlantic Ridge in the equatorial Atlantic Ocean. Over a 120 km-long section between the St Paul fracture zone (FZ) and the Romanche transform fault (TF), we observe four distinct 20–30 km long crustal segments. The segment affected by the St Paul FZ consists of three layers, an ∼2 km thick layer with a P-wave velocity <6 km/s, a 1.5 km thick middle crust with a velocity of 6–6.5 km/s, and an underlying layer where velocity is ∼7 km/s, representing the lower crust. The segment associated with an abyssal hill morphology contains a high velocity of ∼7 km/s at 2–2.5 km below the basement, indicating the presence of primitive gabbro or serpenized peridotite. The segment associated with a low basement morphology seems to have 5.5–6.5 km/s velocity starting near the basement extending down to ∼4 km depth, indicating chemically distinct crust. The segment close to the Romanche TF, a velocity 4.5–5 km/s near the seafloor increasing to 7 km/s at 4 km depth indicates a magmatic origin. The four distinct crustal segments have a good correlation with the overlying seafloor morphology. These observed strong crustal heterogeneities could result from alternate tectonic and magmatic processes along the ridge axis, possibly modulated by thermal and/or chemical variations in the mantle during their formation along the ridge segment.
在缓慢扩张的环境中,大洋地壳是由岩浆和构造过程共同形成的。通过对主动源海底地震仪数据进行全波形反演,我们揭示了在赤道大西洋缓慢扩张的大西洋中脊(Mid-Atlantic Ridge)形成的 40-48 Ma 大洋地壳中存在着强烈的横向变化。在圣保罗断裂带(FZ)和罗曼切转换断层(TF)之间 120 公里长的地段上,我们观察到四个不同的 20-30 公里长的地壳区段。受圣保罗断裂带影响的地段由三层组成,一层厚 2 千米,P 波速度为 6 千米/秒;一层厚 1.5 千米,速度为 6-6.5 千米/秒;另一层为下地壳,速度为 7 千米/秒。与深海山丘形态相关的地段在基底下 2-2.5 千米处有一个速度为每秒 7 千米的高速层,表明存在原始辉长岩或绢云橄榄岩。与低基底形态相关的地段似乎从基底附近开始有每秒 5.5-6.5 公里的速度,一直延伸到 4 公里深处,表明地壳的化学性质不同。靠近罗曼切 TF 的地段,靠近海底的速度为 4.5-5 千米/秒,在 4 千米深度处速度增至 7 千米/秒,表明地壳起源于岩浆。四个不同的地壳区段与上覆海底形态有很好的相关性。观察到的这些强烈的地壳异质性可能是沿海脊轴线交替的构造和岩浆过程造成的,可能在沿海脊段形成过程中受到地幔中热和/或化学变化的影响。
{"title":"Seismic Evidence for Velocity Heterogeneity Along ∼40 Ma Old Oceanic Crustal Segment Formed at the Slow-Spreading Equatorial Mid-Atlantic Ridge From Full Waveform Inversion of Ocean Bottom Seismometer Data","authors":"Peng Guo, Satish C. Singh","doi":"10.1029/2024jb029776","DOIUrl":"https://doi.org/10.1029/2024jb029776","url":null,"abstract":"In slow spreading environments, oceanic crust is formed by a combination of magmatic and tectonic processes. Using full waveform inversion applied to active-source ocean bottom seismometer data, we reveal the presence of a strong lateral variability in the 40–48 Ma old oceanic crust formed at the slow-spreading Mid-Atlantic Ridge in the equatorial Atlantic Ocean. Over a 120 km-long section between the St Paul fracture zone (FZ) and the Romanche transform fault (TF), we observe four distinct 20–30 km long crustal segments. The segment affected by the St Paul FZ consists of three layers, an ∼2 km thick layer with a P-wave velocity &lt;6 km/s, a 1.5 km thick middle crust with a velocity of 6–6.5 km/s, and an underlying layer where velocity is ∼7 km/s, representing the lower crust. The segment associated with an abyssal hill morphology contains a high velocity of ∼7 km/s at 2–2.5 km below the basement, indicating the presence of primitive gabbro or serpenized peridotite. The segment associated with a low basement morphology seems to have 5.5–6.5 km/s velocity starting near the basement extending down to ∼4 km depth, indicating chemically distinct crust. The segment close to the Romanche TF, a velocity 4.5–5 km/s near the seafloor increasing to 7 km/s at 4 km depth indicates a magmatic origin. The four distinct crustal segments have a good correlation with the overlying seafloor morphology. These observed strong crustal heterogeneities could result from alternate tectonic and magmatic processes along the ridge axis, possibly modulated by thermal and/or chemical variations in the mantle during their formation along the ridge segment.","PeriodicalId":15864,"journal":{"name":"Journal of Geophysical Research: Solid Earth","volume":null,"pages":null},"PeriodicalIF":3.9,"publicationDate":"2024-10-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142486407","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Human-bird interactions in the Levant during the Late Pleistocene to Early Holocene: Multi-scalar analysis of avifaunal remains 晚更新世至全新世早期黎凡特地区的人鸟互动:鸟类遗骸的多尺度分析
IF 2.1 2区 地球科学 Q1 ANTHROPOLOGY Pub Date : 2024-10-22 DOI: 10.1007/s12520-024-02090-6
Lisa Yeomans, Camilla Mazzucato

This paper describes analyses of avifauna from Levantine Late Pleistocene and Early Holocene sites at contrasting scales. We present avian osteological data at Shubayqa, in northeast Jordan, illustrating human-bird-environment interactions over 4000 years offering interpretation of environmental change on avifaunal communities and reorientation in the nature of multi-species relationships at a wetland environment. Comparisons to published avifaunal assemblages investigates bird-human relationships across a broader temporal and geographical span. During the Late Pleistocene and Early Holocene, some of our species gradually transitioned to agriculture. People hunted birds for subsistence but extensive evidence for the symbolic importance of birds suggests complex relationships between species. Avifaunal evidence, therefore, presents insights into two commonly suggested primary causes for the shift from hunter-foragers to agriculturalists – resource pressure and symbolic expression. In this paper, we investigate and try to clarify the relationship between humans and birds at this transitional period in human history, furthering discussions of the shift towards agriculture. We argue humans gradually modified the landscape but this was not a reactionary response to resource stress. Nevertheless, this resulted in the productivity of the landscape increasing and allowed further intensification. Feathers and talons of birds were used for millennia preceding the shift to agriculture and the increase in bird hunting towards the end of the Pleistocene cannot be explained by the increased role of birds in the symbolic realm. The evidence from the avifauna adds weight to the idea of ecological niche construction activities, as people invested in specific locations, increasing productivity of habitats, thus encouraging further investment within some environments.

本文介绍了对不同尺度的黎凡特晚更新世和全新世早期遗址鸟类的分析。我们展示了约旦东北部舒拜卡(Shubayqa)的鸟类骨学数据,说明了 4000 年来人类-鸟类-环境之间的相互作用,解释了鸟类群落的环境变化以及湿地环境中多物种关系性质的重新定位。通过与已发表的鸟类群落进行比较,研究鸟类与人类在更广阔的时间和地理跨度上的关系。在晚更新世和全新世早期,我们的一些物种逐渐向农业过渡。人们以捕猎鸟类为生,但有大量证据表明鸟类具有重要的象征意义,这表明物种之间存在着复杂的关系。因此,鸟类学证据为我们提供了从狩猎者向农业者转变的两个常见主要原因--资源压力和象征性表达--的见解。在本文中,我们调查并试图澄清在人类历史的这一过渡时期人类与鸟类之间的关系,从而进一步讨论向农业的转变。我们认为,人类逐渐改变了地貌,但这并不是对资源压力的反应。尽管如此,这还是提高了景观的生产力,并允许进一步集约化。鸟类的羽毛和爪子在向农业转变之前的几千年就已被使用,而更新世末期捕鸟活动的增加并不能用鸟类在象征领域中的作用增强来解释。鸟类的证据增加了生态位构建活动这一观点的分量,因为人们在特定地点投资,提高了栖息地的生产力,从而鼓励了在某些环境中的进一步投资。
{"title":"Human-bird interactions in the Levant during the Late Pleistocene to Early Holocene: Multi-scalar analysis of avifaunal remains","authors":"Lisa Yeomans,&nbsp;Camilla Mazzucato","doi":"10.1007/s12520-024-02090-6","DOIUrl":"10.1007/s12520-024-02090-6","url":null,"abstract":"<div><p>This paper describes analyses of avifauna from Levantine Late Pleistocene and Early Holocene sites at contrasting scales. We present avian osteological data at Shubayqa, in northeast Jordan, illustrating human-bird-environment interactions over 4000 years offering interpretation of environmental change on avifaunal communities and reorientation in the nature of multi-species relationships at a wetland environment. Comparisons to published avifaunal assemblages investigates bird-human relationships across a broader temporal and geographical span. During the Late Pleistocene and Early Holocene, some of our species gradually transitioned to agriculture. People hunted birds for subsistence but extensive evidence for the symbolic importance of birds suggests complex relationships between species. Avifaunal evidence, therefore, presents insights into two commonly suggested primary causes for the shift from hunter-foragers to agriculturalists – resource pressure and symbolic expression. In this paper, we investigate and try to clarify the relationship between humans and birds at this transitional period in human history, furthering discussions of the shift towards agriculture. We argue humans gradually modified the landscape but this was not a reactionary response to resource stress. Nevertheless, this resulted in the productivity of the landscape increasing and allowed further intensification. Feathers and talons of birds were used for millennia preceding the shift to agriculture and the increase in bird hunting towards the end of the Pleistocene cannot be explained by the increased role of birds in the symbolic realm. The evidence from the avifauna adds weight to the idea of ecological niche construction activities, as people invested in specific locations, increasing productivity of habitats, thus encouraging further investment within some environments.</p></div>","PeriodicalId":8214,"journal":{"name":"Archaeological and Anthropological Sciences","volume":null,"pages":null},"PeriodicalIF":2.1,"publicationDate":"2024-10-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s12520-024-02090-6.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142453123","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}
引用次数: 0
期刊
全部 Geobiology Appl. Clay Sci. Geochim. Cosmochim. Acta J. Hydrol. Org. Geochem. Carbon Balance Manage. Contrib. Mineral. Petrol. Int. J. Biometeorol. IZV-PHYS SOLID EART+ J. Atmos. Chem. Acta Oceanolog. Sin. Acta Geophys. ACTA GEOL POL ACTA PETROL SIN ACTA GEOL SIN-ENGL AAPG Bull. Acta Geochimica Adv. Atmos. Sci. Adv. Meteorol. Am. J. Phys. Anthropol. Am. J. Sci. Am. Mineral. Annu. Rev. Earth Planet. Sci. Appl. Geochem. Aquat. Geochem. Ann. Glaciol. Archaeol. Anthropol. Sci. ARCHAEOMETRY ARCT ANTARCT ALP RES Asia-Pac. J. Atmos. Sci. ATMOSPHERE-BASEL Atmos. Res. Aust. J. Earth Sci. Atmos. Chem. Phys. Atmos. Meas. Tech. Basin Res. Big Earth Data BIOGEOSCIENCES Boundary Layer Meteorol. BOREAS Braz. J. Geol. B GEOSCI CAN GEOTECH J Bull. Seismol. Soc. Am. Can. Mineral. Bull. Am. Meteorol. Soc. Can. J. Earth Sci. Carbonates Evaporites Chem. Geol. Clim. Dyn. Clay Miner. Clays Clay Miner. Clim. Past CLIM RES Comput. Geosci. DEEP-SEA RES PT II Dokl. Earth Sci. Earth Surf. Processes Landforms EARTH PLANETS SPACE Earth Sci. Res. J. Econ. Geol. Earth Planet. Sci. Lett. Earth Sci. Rev. Eng. Geol. ELEMENTS Eur. J. Mineral. Front. Earth Sci. Geo-Mar. Lett. GEOFLUIDS Geophys. J. Int. Geophys. Res. Lett. Geocarto Int. Geog. Anal. GEOL CARPATH GEOL Q Gems Gemol. Geol. Mag. GEOCHEM PERSPECT LET Geosynth. Int. Geofis. Int. Geostand. Geoanal. Res. GEOLOGY Geosci. J. Geochem. J. Geochem. Trans. Geosci. Front. Geol. Ore Deposits Global Biogeochem. Cycles Gondwana Res. Geochem. Int. Geol. J. Geophys. Prospect. Geosci. Model Dev. GEOL BELG GROUNDWATER Hydrogeol. J. Hydrol. Earth Syst. Sci. Hydrol. Processes Int. J. Climatol. Int. J. Earth Sci.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1