Lucy R. Roberts, Isabel J. Bishop, Jennifer K. Adams
The open collection “Aquatic transitions: Tracking the nature and trajectories of anthropogenically forced change in freshwater and coastal ecosystems” stems from a session of the same name at the ASLO (Association for the Sciences of Limnology and Oceanography) Aquatic Sciences Meeting 2017 in Honolulu, Hawai'i. The five papers gathered here reflect the focus of the special session on long-term ecosystem research and monitoring (LTERM), and collectively make use of monitoring data, palaeolimnology, and historical and documentary records to explore the timing, extent, and causes of human-related impacts on aquatic ecosystems. Collectively, they demonstrate that because timescales of ecological change often extend beyond contemporary monitoring, LTERM plays a crucial role in supporting evidence-based conservation. In this introduction, we reflect on the role that LTERM has had in each of the ecosystems studied, and discuss the opportunities for LTERM work to inform future conservation.
“水生过渡:追踪淡水和沿海生态系统人为强迫变化的性质和轨迹”这一公开合集源于2017年在夏威夷檀香山举行的ASLO(湖沼学和海洋学科学协会)水生科学会议的同名会议。这五篇论文反映了长期生态系统研究和监测(LTERM)特别会议的重点,并共同利用监测数据、古湖泊学、历史和文献记录来探讨人类对水生生态系统影响的时间、程度和原因。总的来说,他们表明,由于生态变化的时间尺度往往超出当代监测,LTERM在支持基于证据的保护方面发挥着至关重要的作用。在这篇引言中,我们反思了LTERM在研究的每个生态系统中的作用,并讨论了LTERM工作为未来保护提供信息的机会。作者将英国布罗德斯国家公园(Broads National Park) Thurne Broads的记录作为一个试验台,利用历史记录作为一种低成本和有效的方法来确定欧盟水框架指令的前人为参考条件,并为未来的地点管理提供信息。他们强调了在多压力源环境中长期监测的潜在局限性,并建议将历史记录和古湖泊学研究结合起来进行更可靠的重建。
{"title":"Anthropogenically forced change in aquatic ecosystems: Reflections on the use of monitoring, archival and palaeolimnological data to inform conservation","authors":"Lucy R. Roberts, Isabel J. Bishop, Jennifer K. Adams","doi":"10.1002/geo2.89","DOIUrl":"10.1002/geo2.89","url":null,"abstract":"<p>The open collection “Aquatic transitions: Tracking the nature and trajectories of anthropogenically forced change in freshwater and coastal ecosystems” stems from a session of the same name at the ASLO (Association for the Sciences of Limnology and Oceanography) Aquatic Sciences Meeting 2017 in Honolulu, Hawai'i. The five papers gathered here reflect the focus of the special session on long-term ecosystem research and monitoring (LTERM), and collectively make use of monitoring data, palaeolimnology, and historical and documentary records to explore the timing, extent, and causes of human-related impacts on aquatic ecosystems. Collectively, they demonstrate that because timescales of ecological change often extend beyond contemporary monitoring, LTERM plays a crucial role in supporting evidence-based conservation. In this introduction, we reflect on the role that LTERM has had in each of the ecosystems studied, and discuss the opportunities for LTERM work to inform future conservation.</p>","PeriodicalId":44089,"journal":{"name":"Geo-Geography and Environment","volume":"7 1","pages":""},"PeriodicalIF":2.2,"publicationDate":"2020-05-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/geo2.89","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"48490625","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Charlotte L. Briddon, Suzanne McGowan, Sarah E. Metcalfe, Virginia Panizzo, Jack Lacey, Stefan Engels, Melanie Leng, Keely Mills, Muhammad Shafiq, Mushrifah Idris
Rapid development and climate change in southeast Asia is placing unprecedented pressures on freshwater ecosystems, but long term records of the ecological consequences are rare. Here we examine one basin of Tasik Chini (Malaysia), a UNESCO-designated flood pulse wetland, where human disturbances (dam installation, iron ore mining, oil palm and rubber cultivation) have escalated since the 1980s. Diatom analysis and organic matter geochemistry (δ13Corg and C/N ratios) were applied to a sediment sequence to infer ecological changes in the basin since c. 1900 CE. As the Tasik Chini wetland is a rare ecosystem with an unknown diatom ecology, contemporary diatom habitats (plant surfaces, mud surfaces, rocks, plankton) were sampled from across the lake to help interpret the sedimentary record. Habitat specificity of diatoms was not strongly defined and, although planktonic and benthic groupings were distinctive, there was no difference in assemblages among the benthic habitat surfaces. An increase in the proportion of benthic diatom taxa suggests that a substantial decrease in water level occurred between c. 1938 and 1995 CE, initiated by a decline in rainfall (supported by regional meteorological data), which increased the hydrological isolation of the sub-basin. Changes in the diatom assemblages were most marked after 1995 CE when the Chini dam was installed. After this time both δ13Corg and C/N decreased, suggesting an increase in autochthonous production relative to allochthonous river flood pulse inputs. Oil palm plantations and mining continued to expand after c. 1995 CE and we speculate that inputs of pollutants from these activities may have contributed to the marked ecological change. Together, our work shows that this sub-basin of Tasik Chini has been particularly sensitive to, and impacted by, a combination of human and climatically induced changes due to its hydrologically isolated position.
{"title":"Diatoms in a sediment core from a flood pulse wetland in Malaysia record strong responses to human impacts and hydro-climate over the past 150 years","authors":"Charlotte L. Briddon, Suzanne McGowan, Sarah E. Metcalfe, Virginia Panizzo, Jack Lacey, Stefan Engels, Melanie Leng, Keely Mills, Muhammad Shafiq, Mushrifah Idris","doi":"10.1002/geo2.90","DOIUrl":"10.1002/geo2.90","url":null,"abstract":"<p>Rapid development and climate change in southeast Asia is placing unprecedented pressures on freshwater ecosystems, but long term records of the ecological consequences are rare. Here we examine one basin of Tasik Chini (Malaysia), a UNESCO-designated flood pulse wetland, where human disturbances (dam installation, iron ore mining, oil palm and rubber cultivation) have escalated since the 1980s. Diatom analysis and organic matter geochemistry (δ<sup>13</sup>C<sub>org</sub> and C/N ratios) were applied to a sediment sequence to infer ecological changes in the basin since <i>c.</i> 1900 CE. As the Tasik Chini wetland is a rare ecosystem with an unknown diatom ecology, contemporary diatom habitats (plant surfaces, mud surfaces, rocks, plankton) were sampled from across the lake to help interpret the sedimentary record. Habitat specificity of diatoms was not strongly defined and, although planktonic and benthic groupings were distinctive, there was no difference in assemblages among the benthic habitat surfaces. An increase in the proportion of benthic diatom taxa suggests that a substantial decrease in water level occurred between <i>c.</i> 1938 and 1995 CE, initiated by a decline in rainfall (supported by regional meteorological data), which increased the hydrological isolation of the sub-basin. Changes in the diatom assemblages were most marked after 1995 CE when the Chini dam was installed. After this time both δ<sup>13</sup>C<sub>org</sub> and C/N decreased, suggesting an increase in autochthonous production relative to allochthonous river flood pulse inputs. Oil palm plantations and mining continued to expand after <i>c.</i> 1995 CE and we speculate that inputs of pollutants from these activities may have contributed to the marked ecological change. Together, our work shows that this sub-basin of Tasik Chini has been particularly sensitive to, and impacted by, a combination of human and climatically induced changes due to its hydrologically isolated position.</p>","PeriodicalId":44089,"journal":{"name":"Geo-Geography and Environment","volume":"7 1","pages":""},"PeriodicalIF":2.2,"publicationDate":"2020-05-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/geo2.90","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45395662","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Charles Travis, Francis Ludlow, Al Matthews, Kevin Lougheed, Kieran Rankin, Bernard Allaire, Robert Legg, Patrick Hayes, Richard Breen, John Nicholls, Lydia Towns, Poul Holm
As a feature of the Fish Revolution (1400–1700), the early modern “invention” of the Grand Banks in literary and cartographical documents facilitated a massive and unprecedented extraction of cod from the waters of the north Atlantic and created the Cod/Sack trade Triangle. This overlapped with the southern Atlantic Slave, Sugar, and Tobacco Triangle to capitalise modern European and North American societies. In 1719, Pierre de Charlevoix claimed that the Grand Banks was “properly a mountain, hid under water,” and noted its cod population “seems to equal that of the grains of sand which cover this bank.” However, two centuries later in 1992, in the face of the collapse of the fishery, and fearing its extinction, a moratorium was placed on five centuries of harvesting Grand Banks cod. The invention and mining of its waters serves as a bellwether for the massive resource extractions of modernity that drive the current leviathan and “wicked problem” of global warming. The digital environmental humanities narrative of this study is parsed together from 83 pieces of Grand Banks charting from 1504 to 1833, which are juxtaposed through Humanities GIS applications with English and French cod-catch records kept between 1675 and 1831, letters regarding Cabot's 1497 voyage, Shakespeare's The Tempest (1611) and scientific essays by De Brahms (1772) and Franklin (1786).
作为鱼类革命(1400-1700年)的一个特点,文学和制图文献中关于大浅滩的早期现代“发明”促进了从北大西洋水域大规模和前所未有的鳕鱼开采,并创造了鳕鱼/袋贸易三角。这与南大西洋奴隶、糖和烟草三角重叠,使现代欧洲和北美社会资本化。1719年,皮埃尔·德·沙勒瓦(Pierre de Charlevoix)声称大浅滩“实际上是一座隐藏在水下的山”,并指出它的鳕鱼数量“似乎与覆盖在这片海岸上的沙粒数量相当”。然而,两个世纪后的1992年,面对渔业的崩溃,以及对其灭绝的担忧,人们暂停了五个世纪以来捕捞大浅滩鳕鱼的活动。这一水域的发明和开采为现代社会大规模的资源开采提供了一个风向标,这些资源开采推动了当前的利维坦和全球变暖的“邪恶问题”。本研究的数字环境人文叙述从1504年至1833年的83份大滩图表中分析出来,通过人文地理信息系统应用将其与1675年至1831年间保存的英语和法语鳕鱼捕捞记录、卡博特1497年航行的信件、莎士比亚的《暴风雨》(1611年)以及德·勃拉姆斯(1772年)和富兰克林(1786年)的科学论文并列。
{"title":"Inventing the Grand Banks: A deep chart","authors":"Charles Travis, Francis Ludlow, Al Matthews, Kevin Lougheed, Kieran Rankin, Bernard Allaire, Robert Legg, Patrick Hayes, Richard Breen, John Nicholls, Lydia Towns, Poul Holm","doi":"10.1002/geo2.85","DOIUrl":"https://doi.org/10.1002/geo2.85","url":null,"abstract":"<p>As a feature of the Fish Revolution (1400–1700), the early modern “invention” of the Grand Banks in literary and cartographical documents facilitated a massive and unprecedented extraction of cod from the waters of the north Atlantic and created the Cod/Sack trade Triangle. This overlapped with the southern Atlantic Slave, Sugar, and Tobacco Triangle to capitalise modern European and North American societies. In 1719, Pierre de Charlevoix claimed that the Grand Banks was “properly a mountain, hid under water,” and noted its cod population “seems to equal that of the grains of sand which cover this bank.” However, two centuries later in 1992, in the face of the collapse of the fishery, and fearing its extinction, a moratorium was placed on five centuries of harvesting Grand Banks cod. The invention and mining of its waters serves as a bellwether for the massive resource extractions of modernity that drive the current leviathan and “wicked problem” of global warming. The digital environmental humanities narrative of this study is parsed together from 83 pieces of Grand Banks charting from 1504 to 1833, which are juxtaposed through Humanities GIS applications with English and French cod-catch records kept between 1675 and 1831, letters regarding Cabot's 1497 voyage, Shakespeare's <i>The Tempest</i> (1611) and scientific essays by De Brahms (1772) and Franklin (1786).</p>","PeriodicalId":44089,"journal":{"name":"Geo-Geography and Environment","volume":"7 1","pages":""},"PeriodicalIF":2.2,"publicationDate":"2020-03-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/geo2.85","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"91888065","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
This paper explores the geographical distribution of independent and do-it-yourself information and communication technology maintenance and repair (INDIY ICT M&R) activity around the world. It examines a large set of Google Analytics data pertaining to users of free, open-source online repair manuals provided by iFixit, a US-based organisation that develops the free manuals, sells tools and components, and also engages in technical education and policy advocacy. The paper draws on three years of available user data (2016–2018). Over this time period the total user base of iFixit's manuals grew from over 1.3 million users to more than 4.1 million users across the planet. However, counter to what might be expected, the global distribution of iFixit users does not systematically co-vary with internet access rates or with the population size of locations. The results reported here, while partial, are valuable in that they demonstrate both a globally distributed phenomenon and high-resolution location patterns of INDIY ICT M&R activity. Mapping the extent and spatial patterning of such activity is a jumping off point for the kinds of qualitative analyses needed to elucidate the how's, the why's, and the meanings of the observed uneven distribution patterns. More broadly, the results suggest fruitful directions for deeper analyses and research into both pragmatic questions about ICT maintenance and repair (such as their social, economic, and environmental significance), as well as more speculative questions about how and why the fates of ICT within and between production, use, and discard stand in for dreams of technological futurity and nightmares of social and environmental breakdown.
{"title":"Planet of fixers? Mapping the middle grounds of independent and do-it-yourself information and communication technology maintenance and repair","authors":"Josh Lepawsky","doi":"10.1002/geo2.86","DOIUrl":"https://doi.org/10.1002/geo2.86","url":null,"abstract":"<p>This paper explores the geographical distribution of independent and do-it-yourself information and communication technology maintenance and repair (INDIY ICT M&R) activity around the world. It examines a large set of Google Analytics data pertaining to users of free, open-source online repair manuals provided by iFixit, a US-based organisation that develops the free manuals, sells tools and components, and also engages in technical education and policy advocacy. The paper draws on three years of available user data (2016–2018). Over this time period the total user base of iFixit's manuals grew from over 1.3 million users to more than 4.1 million users across the planet. However, counter to what might be expected, the global distribution of iFixit users does not systematically co-vary with internet access rates or with the population size of locations. The results reported here, while partial, are valuable in that they demonstrate both a globally distributed phenomenon and high-resolution location patterns of INDIY ICT M&R activity. Mapping the extent and spatial patterning of such activity is a jumping off point for the kinds of qualitative analyses needed to elucidate the how's, the why's, and the meanings of the observed uneven distribution patterns. More broadly, the results suggest fruitful directions for deeper analyses and research into both pragmatic questions about ICT maintenance and repair (such as their social, economic, and environmental significance), as well as more speculative questions about how and why the fates of ICT within and between production, use, and discard stand in for dreams of technological futurity and nightmares of social and environmental breakdown.</p>","PeriodicalId":44089,"journal":{"name":"Geo-Geography and Environment","volume":"7 1","pages":""},"PeriodicalIF":2.2,"publicationDate":"2020-02-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/geo2.86","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"91830065","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Exploration of the underwater landscape in Lithuanian waters, in the eastern part of the Baltic Sea, allowed identification of trees stumps in growth position, peat sediments, and traces of people that were living in the now flooded landscape. The exploration has been concentrated on localisation of the former Early Holocene coasts. Based on new data about sediment layers of the Preboreal‒Atlantis I, palynological and dendrohronological analysis, identified vegetation species, and dating of wood and peat samples by radiocarbon methods the Baltic Sea water level dynamics during the stages Yoldia Sea‒Early Litorina Sea could be identified. There are traces of the eroded coasts of the Yoldia Sea at a depth of 39–43 m, which were also observed at depths of 44 and 47 m. During the Ancylus Lake transgression, the RF-I lagoons and small lakes with the peat layer and the surrounding forests were submerged. The water level could have even risen to 10–9 m below present sea level. The water drop during the Ancylus Lake regression is evidenced by a peat layer dated to 9,150–8,520 cal BP, and similar radiocarbon dating of an oak stump. The changes of the species composition of trees are indicative of the noticeable climate changes during the period 11,410–7,900 cal BP. Litorina transgression is marked by a tree stump found at a depth of 14.5 m dated to 7,900–7,660 cal BP. The preference of the Early Holocene population to the coastal zone is evidenced by poles driven into the seabed (one was dated to 9,510–9,460 cal BP) that were detected at a depth of 11 m and the T-shaped antler axes dated to the Early Neolithic, washed ashore from the Litorina Sea coastal Stone Age settlements.
对波罗的海东部立陶宛水域水下景观的探索,使人们能够识别生长位置的树桩、泥炭沉积物,以及生活在现在被淹没的景观中的人的痕迹。勘探主要集中在早期全新世前海岸的定位上。根据preborealatlantis I沉积层的新资料、孢粉学和树木年代学分析、已鉴定的植被种类以及放射性碳测年法测定的木材和泥炭样品,可以确定约尔迪亚海-早期利托里纳海阶段波罗的海的水位动态。在39-43米的深度有约尔迪亚海海岸被侵蚀的痕迹,在44和47米的深度也有观察到。在安丘勒斯湖海侵期间,含泥炭层的RF-I泻湖和小湖泊及其周围的森林被淹没。水位甚至可能上升到比现在的海平面低10-9米。在安丘勒斯湖回归期间的水滴由泥炭层和橡树树桩的放射性碳定年法证明,泥炭层的年代为9,150-8,520 cal BP。树木种类组成的变化反映了11410 ~ 7900 cal BP期间明显的气候变化。Litorina海侵的标志是在14.5 m深度发现的树桩,其年代为7,900-7,660 cal BP。全新世早期种群对沿海地区的偏好可以通过以下证据得到证明:在11米深的海底发现了插入海底的极点(其中一个极点的年代为9,510-9,460 cal BP),以及从Litorina海沿海石器时代定居点冲上岸的t形鹿角轴,这些极点可以追溯到新石器时代早期。
{"title":"The eastern shores of the Baltic Sea in the Early Holocene according to natural and cultural relict data","authors":"Vladas Žulkus, Algirdas Girininkas","doi":"10.1002/geo2.87","DOIUrl":"https://doi.org/10.1002/geo2.87","url":null,"abstract":"<p>Exploration of the underwater landscape in Lithuanian waters, in the eastern part of the Baltic Sea, allowed identification of trees stumps in growth position, peat sediments, and traces of people that were living in the now flooded landscape. The exploration has been concentrated on localisation of the former Early Holocene coasts. Based on new data about sediment layers of the Preboreal‒Atlantis I, palynological and dendrohronological analysis, identified vegetation species, and dating of wood and peat samples by radiocarbon methods the Baltic Sea water level dynamics during the stages Yoldia Sea‒Early Litorina Sea could be identified. There are traces of the eroded coasts of the Yoldia Sea at a depth of 39–43 m, which were also observed at depths of 44 and 47 m. During the Ancylus Lake transgression, the RF-I lagoons and small lakes with the peat layer and the surrounding forests were submerged. The water level could have even risen to 10–9 m below present sea level. The water drop during the Ancylus Lake regression is evidenced by a peat layer dated to 9,150–8,520 cal BP, and similar radiocarbon dating of an oak stump. The changes of the species composition of trees are indicative of the noticeable climate changes during the period 11,410–7,900 cal BP. Litorina transgression is marked by a tree stump found at a depth of 14.5 m dated to 7,900–7,660 cal BP. The preference of the Early Holocene population to the coastal zone is evidenced by poles driven into the seabed (one was dated to 9,510–9,460 cal BP) that were detected at a depth of 11 m and the T-shaped antler axes dated to the Early Neolithic, washed ashore from the Litorina Sea coastal Stone Age settlements.</p>","PeriodicalId":44089,"journal":{"name":"Geo-Geography and Environment","volume":"7 1","pages":""},"PeriodicalIF":2.2,"publicationDate":"2020-02-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/geo2.87","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"91830068","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
L. Roberts, C. Sayer, D. Hoare, M. Tomlinson, J. Holmes, D. Horne, Andrea Kelly
The effective management and restoration of aquatic ecosystems rely on the establishment of “reference conditions,” defined as the conditions expected in theabsence of anthropogenic impacts, and require a thorough understanding of thenatural variability within a system. However, at least in Europe, most systematicsurveys post‐date the onset of human‐induced pressures on aquatic ecosystems,and thus fail to capture earlier degradation to water chemistry and flora and fauna,which were already advanced. Paleolimnological methods can be used to assess arange of anthropogenic stressors, but variability within a system is often smoothedto give long‐term patterns. Here, we compile monitoring, documentary, and archival records from a range of sources to extend our understanding of centennial‐scale lake ecosystem change and recovery from increasing salinity. We use a casestudy of the Thurne Broads shallow lake coastal wetland system (Broads NationalPark, UK), which has been subjected to multiple pressures of anthropogenic landdrainage and North Sea storm surges (primarily in 1938 and 1953 CE) that haveinfluenced salinity. Although there are still periods with significant data gaps andthe interactions with eutrophication remain unclear, we demonstrate that historicaldata sources can be used in combination to observe seasonal patterns and extendknowledge on past salinity change and macrophyte community structure back tothe 1800s. A demonstrable change in the ecosystem is observed after the sea floodof 1938 CE, when salinity levels in parts of the Thurne Broads were close, orequivalent, to seawater. With the added anthropogenic pressures of the late 1900s,the system has failed to fully recover. Future management, whilst balancing theneeds of multiple users, should focus on the current large seasonal fluctuations insalinity and the vulnerability of the system to future large salinity increases.
{"title":"The role of monitoring, documentary and archival records for coastal shallow lake management","authors":"L. Roberts, C. Sayer, D. Hoare, M. Tomlinson, J. Holmes, D. Horne, Andrea Kelly","doi":"10.1002/GEO2.83","DOIUrl":"https://doi.org/10.1002/GEO2.83","url":null,"abstract":"The effective management and restoration of aquatic ecosystems rely on the establishment of “reference conditions,” defined as the conditions expected in theabsence of anthropogenic impacts, and require a thorough understanding of thenatural variability within a system. However, at least in Europe, most systematicsurveys post‐date the onset of human‐induced pressures on aquatic ecosystems,and thus fail to capture earlier degradation to water chemistry and flora and fauna,which were already advanced. Paleolimnological methods can be used to assess arange of anthropogenic stressors, but variability within a system is often smoothedto give long‐term patterns. Here, we compile monitoring, documentary, and archival records from a range of sources to extend our understanding of centennial‐scale lake ecosystem change and recovery from increasing salinity. We use a casestudy of the Thurne Broads shallow lake coastal wetland system (Broads NationalPark, UK), which has been subjected to multiple pressures of anthropogenic landdrainage and North Sea storm surges (primarily in 1938 and 1953 CE) that haveinfluenced salinity. Although there are still periods with significant data gaps andthe interactions with eutrophication remain unclear, we demonstrate that historicaldata sources can be used in combination to observe seasonal patterns and extendknowledge on past salinity change and macrophyte community structure back tothe 1800s. A demonstrable change in the ecosystem is observed after the sea floodof 1938 CE, when salinity levels in parts of the Thurne Broads were close, orequivalent, to seawater. With the added anthropogenic pressures of the late 1900s,the system has failed to fully recover. Future management, whilst balancing theneeds of multiple users, should focus on the current large seasonal fluctuations insalinity and the vulnerability of the system to future large salinity increases.","PeriodicalId":44089,"journal":{"name":"Geo-Geography and Environment","volume":"15 11-12","pages":""},"PeriodicalIF":2.2,"publicationDate":"2019-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/GEO2.83","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"51001266","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
I. Bishop, H. Bennion, C. Sayer, Ian R. Patmore, Handong Yang
In the absence of long ‐ term monitoring records, paleoecology can be used to extend knowledge of species and community ecology into the past. The rare and declining aquatic plant Najas flexilis is a priority species for conservation across Europe, and is an ideal candidate for paleoecological study; not only are historical records of the plant sparse, but its seeds are commonly found and well preserved in lake sediment cores. In this study, we investigate the timing and causes of decline at two UK sites at which N. flexilis has recently become extinct: Esthwaite Water (England) and Loch of Craiglush (Scotland). For both sites, multiple paleoecological indicators and available historical biological records and monitoring data are compared to numbers of N. flexilis seeds enumerated in dated sediment cores representing the last 150 years. At Esthwaite Water, N. flexili s seeds were found in abundance in association with indicators of a clear, oligo ‐ mesotrophic, mildly alkaline lake. Eutrophication led to the disappearance of N. flexilis in the 1980s. By contrast, far fewer N. flexilis seeds were found in a core from Loch of Craiglush, and the current period of N. flexilis absence was found to be one of several over the last 100 years. Species represented in cores taken from Loch of Craiglush were indicative of slightly more acidic conditions than Esthwaite Water. Given that N. flexilis favours circumneutral to alkaline conditions, it is possible that Loch of Craiglush has not always been favourable for the plant. These findings have important implications for future conservation efforts, particularly at Esthwaite Water where they suggest that recent failed attempts to reintroduce the species may have been premature. More generally, this study demonstrates the value of paleoecological techniques as a means to provide the long ‐ term context that is often missing from conservation planning and management.
在缺乏长期监测记录的情况下,古生态学可以用来将物种和群落生态学的知识扩展到过去。珍稀濒危水生植物挠性纳哈斯(Najas flexilis)是欧洲各国优先保护的物种,也是古生态研究的理想候选者;不仅这种植物的历史记录很少,而且它的种子在湖泊沉积物岩心中也很常见并保存得很好。在这项研究中,我们调查了两个英国地点的下降时间和原因,在这两个地点,flexilis最近已经灭绝:Esthwaite Water(英格兰)和Loch of Craiglush(苏格兰)。在这两个地点,我们将多个古生态指标和现有的历史生物记录和监测数据与150年来沉积物岩心中所列举的弹性草种子数量进行了比较。在Esthwaite水域,柔皮草种子的丰度与一个清澈、低中营养、轻度碱性湖泊的指标相关。富营养化导致柔僵菌在20世纪80年代消失。相比之下,在克雷格卢什湖的一个岩心中发现的柔僵草种子要少得多,而且目前的柔僵草缺失期是过去100年里的几次缺失期之一。克雷格鲁什湖岩心中所代表的物种表明酸性条件略高于埃斯韦特水。考虑到N. flexilis喜欢环中性的碱性条件,克雷格鲁什湖可能并不总是对这种植物有利。这些发现对未来的保护工作具有重要意义,特别是在埃斯韦特水域,它们表明最近重新引入该物种的失败尝试可能为时过早。更广泛地说,这项研究证明了古生态技术作为一种提供长期背景的手段的价值,而这在保护规划和管理中往往是缺失的。
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