2018年2月27日 星期二

理論提出植物根部的效率變高以及獨自運作的能力增加使它們能擴散至全世界


理論提出植物根部的效率變高以及獨自運作的能力增加使它們能擴散至全世界
Morgan Kelly
一項關於植物演化的新理論提出4億年來驅使植物擴散至全世界的因素,或許不是地表之上我們能輕易看見的特徵,而是位在地底的適應構造讓植物能更有效率地獨自運作。
根據普林斯頓大學和北京中國科學院的研究人員於221日發表在期刊《科學》(Nature)的研究,當植物從它們最初發源、營養豐富的赤道地區往南北擴張時,它們的根尖變得更細且根系分布範圍也變得更廣,有助於植物從越發貧瘠的土壤中探求重要養分。
此外,隨著植物往環境變化越來越難以預測的地區擴張(像是乾燥的沙漠),它們生長時對共生真菌――即「菌根菌」(mycorrhiza)――的依存程度也越來越低。菌根菌會寄居在植物根部並幫助宿主吸收植物必須的養分――氮和磷。
研究通訊作者Lars Hedin教授是普林斯頓大學環境學院生態學暨演化生物學系的主任,同時也是該校生物學的名譽教授。Hedin表示這項發現重新探討植物演化時如何適應新環境。他說科學家過去討論這項問題時著重於植物地面上的特徵,尤其是葉子的性質和植物進行光合作用時吸收陽光的效率。
反之,Hedin表示他和同事首度發現植物的根部直徑和對真菌的依賴程度――或者是缺乏真菌的程度,這兩項性質是各個生物相(biome)中的植物群集最為一致的特徵。所謂的生物相是由許多特定動植物組成的大型群集,像是沙漠、溫帶森林或者莽原生物相。
「隨著時間經過植物能逐漸征服全球必定有它們的秘訣。」Hedin表示,「我們的目標是要解開並了解這些策略,而我們的發現對植物演化提供了一個新的通用理論。殘酷的適者生存遊戲一直以來在地下悄悄上演著,我們有幸能當上有史以來首批解開這場遊戲背後科學法則的人。」
「這項研究對植物界的保育和管理工作來說具有很大的意義。」Hedin接著說明,「研究提供了某些隱藏在『地下』的法則指出哪些植物可以生存下來並散佈出去。當我們正需要放諸四海皆準的規則來建立氣候模型並深入了解生物圈時,這項研究提供了一個關於植物演化的通用觀點。」
研究第一作者,Hedin研究團隊的普林斯頓研究生Mingzhen Lu表示,如果一種植物忍受特定環境的能力確實取決於根部的性質,當我們要保育瀕危物種或者推測植物可能會如何適應氣候變遷時,這些發現便相當有價值。
「在實際用途上,這項發現可以使我們簡單扼要地表達一種植物獲取養分的策略。」Lu表示,「瞭解植物獲取養分的基本策略有助於我們找出保護它們的方法,或者讓我們得知在哪些情況下它們會存活下來還是邁向滅亡。」
愛達荷大學自然資源學院的院長Kurt Pregitzer表示,在這個物種流動高度頻繁的世界中,入侵種對生物多樣性造成的威脅越加增長,而研究成果在對抗入侵種時或許相當有用。
「入侵種可以大範圍地取代原生植物並在全球造成重大的經濟損失。」Pregitzer表示,「這項研究或許可以開拓新的科學研究方向,讓我們更加瞭解入侵種植物的根系是如何幫助這些外來物種淘汰掉原生物種。」
Pregitzer表示這篇發表於《自然》(Nature)的研究的獨到之處在於規模及精心設計的研究方法。他說:「這是首度有研究的範圍涵蓋如此多樣的陸域環境。結果顯示植物根部演化出的策略僅能在同一科、屬或種身上看到。這些根部特徵或許能讓植物在自然情況下競爭激烈的生態系中成功立足。」
研究人員花費兩年時間仔細研究一座關於根部特徵的資料庫,其內容之多為世上獨有,包含的369個物種分別來自七種生物相:沙漠、草原、地中海型、寒帶、溫帶、亞熱帶和熱帶。
資料由最後一位共同通訊作者,中國科學院地理科學與資源研究所Dali Guo教授的實驗室在長達十年的時間中逐步匯整而成。第一作者Zeqing MaGuo教授實驗室的研究人員;共同作者Xiangliang Xu則和Guo教授任職於同一單位。論文其他共同作者包括英國曼徹斯特大學的生態學教授,研究植物根部的專家Richard Bardgett;賓州州立大學木本植物生理學的教授David Eissenstat;以及明尼蘇達大學的研究人員M. Luke McCormack
就植物用來搜索養分的根尖來說,研究人員發現熱帶和亞熱帶生物相中植物根尖的最小直徑呈現出最大的分布範圍,從小於0.25釐米到1厘米以上都有。研究人員稱呼這些根部較粗的植物採用的策略為「保守型」。它們和地球最早的陸地植物相似,依賴在暖濕的熱帶亞熱帶土壤中常見的土壤真菌來提供養分。研究人員認為它們採用保守策略的原因是常年處於濕熱環境、富含養分的土壤對植物來說是「一成不變的」。
另一方面,在以土壤貧瘠、冬季酷寒或/和降雨稀少為環境特色的生物相中,植物細部根尖的直徑則落在相對狹隘的範圍中,這在「反覆無常」的環境中來說是較為理想的。舉例來說,研究中生活在沙漠和草原的植物種類根部直徑皆小於0.25釐米。在這些生物相中,植物的根尖往更細的方向演化,如此它們才能將耗費的每一分碳都用來更有效率地探索土壤,同時它們對共生真菌的依賴程度也比較低。
Lu表示研究人員所用的大量資料使他們能以前所未有的詳細程度來探討植物根部的演化過程。「由於資料不足的關係,植物生態系統在地下的樣貌一直未被好好研究。」他表示,「因此,在地下進行的事物受到什麼法則掌管,我們仍然所知甚少。」
Hedin補充:「迄今,所有研究學者在試著去瞭解組織管理植物的構造時都相當自然地著眼在地表以上能看到的特徵。但我們的發現卻違背了地表以上理論――這確實令人感到十分驚訝。」
Pregitzer表示研究顯示根和葉是依循著不同路徑來演化。他說植物生態學家已知葉片的型態和構造對一種植物能否成功來說至關重要,但是「我們並不瞭解呈現出龐大多樣性的植物根系是否也有同樣作用。」
「有趣的是,過去我們不太瞭解植物的根部是如何演化來幫助它們在原本的棲地成功生長。」Pregitzer表示,「現在我們知道葉片和根部會對演化過程中不同的選擇性壓力產生回應,這讓我們可以開始更深入瞭解根部的型態和功能,如何促成我們現今在地球上可以見到如此千變萬化的植物。」
Hedin表示這項發現也和另一個由普林斯頓大學的研究人員探討出的概念相符,其認為植物並非是被動地由環境產生出來的特徵,而是可以主動適應並形塑它們所處的環境。在2015年發表在《自然植物》(Nature Plants )Hedin為主要作者的論文中,他們認為生態系之所以呈現出各式各樣的形貌,是因為植物運作的方式不僅可以圖利它們自身,也決定了它們所處棲地的生產力和成份。
Hedin表示:「從演化的時間尺度來看,植物就像是會主動探索出最佳策略來保衛自己以存活下來。」他和Lu將此觀點運用到由中國科學院的共同研究人員所彙整而成的資料庫當中。
「我們從植物學的觀點來看,瞭解到他們獨有的全球資料庫可以應用在演化相關的問題。」Hedin表示,「這項完美的合作將新概念跟歷經多年辛勤的野外工作結合而產生如此漂亮的成果,缺少任何一方都無法達成。」

Theory suggests root efficiency, independence drove global spread of flora
A new theory of plant evolution suggests that the 400 million-year drive of flora across the globe may not have been propelled by the above-ground traits we can see easily, but by underground adaptations that allowed plants to become more efficient and independent.
As plant species spread north and south from their nutrient-rich tropical beginnings, the fine tips of their roots became narrower and more widespread to help them explore increasingly poor soil for vital nutrients, according to a Feb. 21 study in the journal Nature led by researchers from Princeton University and the Chinese Academy of Sciences (CAS) in Beijing.
In addition, as plants spread into unpredictable environments such as arid deserts they grew less dependent on the symbiotic fungi — or mycorrhiza — that colonize roots and help host plants obtain the essential plant nutrients nitrogen and phosphorous.
The findings reconsider how plants adapted to new environments as they evolved, said corresponding author Lars Hedin, the George M. Moffett Professor of Biology and chair and professor of ecology and evolutionary biology and the Princeton Environmental Institute. Scientists have in the past focused on above-ground characteristics, primarily leaf traits and the efficiency with which plants absorb sunlight for photosynthesis, he said.
Instead, Hedin said, he and his colleagues have found for the first time that root diameter and reliance on fungi — or the lack thereof — are the traits that most consistently characterize the plant community across entire biomes, which are large distinct communities of animals and plants such as a desert, temperate forest or savanna.
“These are the secret strategies that plants have used over time to take over the world,” Hedin said. “Our goal was to unlock the understanding of those strategies, and our findings offer a new global theory for plant evolution. Hidden underground there has been a tremendous game of survival-of-the-fittest and we are fortunate to have the first-ever view of the science of that game.
“This work has major implications for conservation and our stewardship of the plant world,” Hedin continued. “It provides some of the hidden, below-ground rules by which plants survive and spread. It’s a global view of plant evolution at a time when global rules are essential for building climate models and understanding the biosphere.”
Mingzhen Lu, first Princeton author and a graduate student in Hedin’s research group, said that if root traits do in fact determine a plant’s ability to withstand a particular environment, these findings could be valuable in conserving endangered species or projecting how plants might adapt to climate change.
“Our findings simplify how we can practically characterize a plant’s strategy for obtaining nutrients,” Lu said. “Knowing their underlying nutrient strategy will help us know how to preserve them, or know the conditions under which they could or could not survive.”
Kurt Pregitzer, the Thomas Reveley Professor and dean of the College of Natural Resources at the University of Idaho, said this work could be especially useful in combating invasive species, which, in a highly mobile world, increasingly threaten biodiversity. Pregitzer is familiar with the research but had no role in it.
“Invasive species cause widespread displacement of native plants and tremendous economic impacts across the globe,” Pregitzer said. “This study may open entirely new lines of scientific investigation that help us better understand how invasive-plant root systems help these exotic species outcompete native plants.”
The Nature paper is unique for its scale and careful application of scientific methods, Pregitzer said. “This study is the first conducted across a wide range of terrestrial environments and it demonstrates that plant species have evolved root strategies that are conserved within corresponding families, genera and species,” he said. “These root traits likely facilitate plant success in highly competitive natural ecosystems.”
The researchers spent two years examining a uniquely large database of root traits consisting of 369 species from seven biomes: desert, grassland, Mediterranean, boreal, temperate, subtropical and tropical.
These data were compiled over the course of a decade in the lab of late co-corresponding author Dali Guo, a professor at CAS’ Institute of Geographic Sciences and Natural Resources Research. First author Zeqing Ma is a research associate in Guo’s lab and co-author Xiangliang Xu is a colleague of Guo’s. The paper’s co-authors also included root experts Richard Bardgett, professor of ecology at the University of Manchester in the U.K.; David Eissenstat, professor of woody plant physiology at Pennsylvania State University; and M. Luke McCormack, a research associate at the University of Minnesota.
The researchers found that plants in tropical and subtropical biomes exhibited the largest diameter range for the finest root tips that forage for nutrients, from less than 0.25 millimeters up to 1 millimeter. These thicker-rooted plants employ what the authors call a “conservative” strategy — similar to that of Earth’s earliest land plants — that relies on the soil fungi prevalent in wet, warm tropical and subtropical soils to provide nutrients. The researchers refer to nutrient-rich soil in consistently sultry environs as “predictable.”
Meanwhile, fine-root diameters in “unpredictable” biomes characterized by poor soil, cold winters and/or infrequent precipitation fall within a narrower range ideal for that environment. For instance, the desert and grassland species studied all had root diameters of less than 0.25 millimeters. Root tips in these biomes evolved to be thinner so they could more efficiently explore soil for every unit of carbon the plant expends, and they have less dependence on symbiotic fungi.
The extensive data the researchers used allowed them to explore the evolution of plant roots to an extent never before possible, Lu said. “Below-ground plant ecology has been understudied, limited by a paucity of data,” he said. “Because of that, the governing rule of what’s going on below ground has been very poorly known.”
“Thus far,” Hedin added, “everybody has quite naturally tried to understand how plants are organized by looking at above-ground traits. But our findings do not follow the above-ground theories — that was a surprise.”
The study reveals that root and leaf evolution have followed different paths, Pregitzer said. Plant ecologists have known that the form and function of leaves are essential to a plant species’ success, but “we did not understand if this was true across the tremendous diversity of plant root systems,” he said.
“Interestingly, little was known about how plant roots have evolved to facilitate success in their native habitats,” Pregitzer said. “Now we know that leaves and roots have responded to different evolutionary selective pressures, and we can start building a better understanding of how root form and function drive plant success within the tremendous biological diversity we see on Earth.”
The findings align with ideas explored at Princeton that suggest that plants — rather than being passive features of their environment — have actively adapted to and shaped their environments, Hedin said. He was senior author of a 2015 paper in Nature Plants that suggested that ecosystems take their various forms because plants behave in ways that not only benefit themselves but also determine the productivity and composition of their habitats.
“Over evolutionary time, it’s as if plants have actively explored the best strategies to safeguard their own survival,” Hedin said. He and Lu brought this perspective to the database put together by their colleagues at CAS.
“We understood from a plant perspective how to bring evolutionary questions to their unique global dataset,” Hedin said. “It was this great collaboration where we combined new ideas with years of painstaking fieldwork to produce this great result. It couldn’t have happened without both sides.”
原始論文:Zeqing Ma, Dali Guo, Xingliang Xu, Mingzhen Lu, Richard D. Bardgett, David M. Eissenstat, M. Luke McCormack, Lars O. Hedin. Evolutionary history resolves global organization of root functional traitsNature, 2018; DOI: 10.1038/nature25783
引用自:Princeton University. "Theory suggests root efficiency, independence drove global spread of flora."

2018年2月14日 星期三

恐龍或許是被接連兩下重擊打倒在地的


恐龍或許是被接連兩下重擊打倒在地的
By Jim Barlow
恐龍到底是被什麼事物消滅的?這項爭議仍然存在。
奧勒岡大學進行的新研究發現6600萬年前沿著深海洋脊發生了跟重力相關的擾動現象,其指出撞擊墨西哥猶加敦半島的巨大隕石可能引發全世界的火山噴出岩漿。這兩次接踵而來的重創或許決定了發生在恐龍身上的噩運。
「我們找到的證據顯示大滅絕事件期間,有段之前未辨識出來的全球火山活動高峰期。」之前在奧勒岡大學就讀博士學位的Joseph Byrnes表示。
這項由Byrnes和奧勒岡大學地球科學系的教授Leif Karlstrom進行的研究於27日刊登於《科學進展》(Science Advances)。這份研究詳細描繪了保存在中洋脊(板塊構造在海底的邊界)的火山活動紀錄,證據則來自於從海床上方測到的重力強度變化。
這項奧勒岡大學的研究由美國國家科學基金會資助。Karlstrom表示研究指出在希克蘇魯伯撞擊事件之後全球火山活動有加劇的現象,包括印度德干高原的噴發量也有所提升。位在印度中西部的德干高原是由一段歷時長久的大型火山噴發事件形成,其噴濺出來的熔岩層層堆積達到數千公尺厚,使德干高原成為地球最大型的火山地貌之一。
在恐龍滅絕的爭論中,德干高原地區曾屢次居於要角又退居幕後。科學家知道如此大規模的罕見火山噴發事件對地球氣候造成的擾動足以釀成重大災難,當它們發生時通常會跟大滅絕事件有所關聯。大型火山噴發事件會噴出大量灰燼和氣體至大氣當中,僅有少數植物能生存下來,進而破壞食物鏈造成動物滅絕。
自從在1980年代發現今日墨西哥的希克蘇魯伯附近曾遭到隕石撞擊的證據之後,科學家就一直在爭論殲滅所有非鳥類恐龍的滅絕事件的罪魁禍首到底是誰――隕石還是德干高原噴發事件。
日趨進步的定年方法顯示德干高原的火山在隕石撞擊之前就已經相當活躍。Karlstrom表示隕石撞擊產生傳遍全球的地震波,或許有助於加速這些噴發事件進行。
「我們的成果顯示這些分布在整個地球,極度稀有且破壞性十足的事件彼此之間互有關連。」Karlstrom表示,「隕石撞擊可能影響了正在進行的火山噴發活動,因而對恐龍造成了接連兩下重創。」
2015年加州大學柏克萊分校的研究人員提出這兩個事件可能有關而加強了此種說法。包括Karlstrom的該團隊認為隕石產生的強力地震波撼動了整個地球,或許能影響遠方的火山活動。
Karlstrom表示就像平常由構造活動產生的地震有時候會讓水井和溪流的流量增加,他們的研究認為震波產生的晃動可以使德干高原下方地函儲存的岩漿釋放出來,而在當地造成最具規模的火山爆發。
奧勒岡大學進行的這項新發現將震波引起噴發的發生範圍從印度拓展至全世界的海盆。
現為明尼蘇達大學博士後研究員的Byrnes從公開取用的資料庫分析全球自由空間重力、海底地形和板塊擴張速率的資料。
在他的分析當中,他以一百萬年為區間來劃分海床年代,建構出的紀錄可以回推至1億年前。他發現大約6600萬年前,自由空間重力的數據出現異常的頻率有所增加,顯示沿著古代洋脊發生的海底岩漿活動此時出現了短暫的高峰期。
自由空間重力異常是指重力加速度的變化量,計算單位是相當微小的毫伽。地球重力比較強的地方會聚集更多海水,運用衛星測量便能偵測到此種變化。Byrnes發現在隕石撞擊過後的首個100萬年之內形成的海床,其自由空間重力發生了520毫伽的異常變化。

A one-two punch may have helped deck the dinosaurs
The debate goes on: What killed off the dinosaurs?
New University of Oregon research has identified gravity-related fluctuations dating to 66 million years ago along deep ocean ridges that point to a “one-two punch” from the big meteor that struck off Mexico’s Yucatan peninsula, possibly triggering a worldwide release of volcanic magma that could have helped seal the dinosaurs' fate.
"We found evidence for a previously unknown period of globally heighted volcanic activity during the mass-extinction event," said former UO doctoral student Joseph Byrnes.
The study by Byrnes and Leif Karlstrom, a professor in the UO’s Department of Earth Sciences, was published Feb. 7 in Science Advances. It details a record of volcanism preserved along the mid-ocean ridges, which mark the oceanic boundaries of tectonic plates. The evidence comes from changes in the strength of gravity above the seafloor.
The findings of the UO's National Science Foundation-supported study, Karlstrom said, point to a pulse of accelerated worldwide volcanic activity that includes enhanced eruptions at India's Deccan Traps after the Chicxulub impact. The Deccan Traps, in west-central India, formed during a period of massive eruptions that poured out layers of molten rock thousands of feet deep, creating one of the largest volcanic features on Earth.
The Deccan Traps region has been in and out of the dinosaur debate. Rare volcanic events at such a scale are known to cause catastrophic disturbances to Earth's climate, and, when they occur, they are often linked to mass extinctions. Huge volcanic events can eject so much ash and gas into the atmosphere that few plants survive, disrupting the food chain and causing animals to go extinct.
Since evidence of the meteor strike near present-day ChicxulubMexico, surfaced in the 1980s, scientists have debated whether the meteor or the Deccan Traps eruptions drove the extinction event that killed off all nonavian dinosaurs.
Progressively improving dating methods indicate that the Deccan Traps volcanoes already were active when the meteor struck. Resulting seismic waves moving through the planet from the meteor strike, Karlstrom said, probably fueled an acceleration of those eruptions.
"Our work suggests a connection between these exceedingly rare and catastrophic events, distributed over the entire planet," Karlstrom said. "The meteorite's impact may have influenced volcanic eruptions that were already going on, making for a one-two punch."
That idea gained strength in 2015 when researchers at the University of California, Berkeley, proposed that the two events might be connected. That team, which included Karlstrom, suggested that the meteorite may have modulated distant volcanism by generating powerful seismic waves that produced shaking worldwide.
Similar to the impacts that normal tectonic earthquakes sometimes have on wells and streams, Karlstrom said, the study proposed that seismic shaking liberated magma stored in the mantle beneath the Deccan Traps and caused the largest eruptions there.
The new findings at the UO extend this eruption-triggering in India to ocean basins worldwide.
Byrnes, now a postdoctoral researcher at the University of Minnesota, analyzed publicly available global data sets on free-air gravity, ocean floor topography and tectonic spreading rates.
In his analyses, he divided the seafloor into 1-million-year-old groupings, constructing a record back to 100 million years ago. At about 66 million years, he found evidence for a "short-lived pulse of marine magmatism" along ancient ocean ridges. This pulse is suggested by a spike in the rate of the occurrence of free-air gravity anomalies seen in the data set.
Free-air gravity anomalies, measured in tiny increments call milligals, account for variations in gravitational acceleration, found from satellite measurements of additional seawater collecting where the Earth's gravity is stronger. Byrnes found changes in free-air gravity anomalies of between five and 20 milligals associated with seafloor created in the first million years after the meteor.
原始論文:Joseph S. Byrnes, Leif Karlstrom. Anomalous K-Pg–aged seafloor attributed to impact-induced mid-ocean ridge magmatismScience Advances, 2018; 4 (2): eaao2994 DOI: 10.1126/sciadv.aao2994
引用自:University of Oregon. "A one-two punch may have helped deck the dinosaurs.”


2018年2月9日 星期五

古代多峇火山的爆發並未在東非造成火山冬天


原文網址:https://uanews.arizona.edu/story/no-volcanic-winter-east-africa-ancient-toba-eruption
古代多峇火山的爆發並未在東非造成火山冬天
亞利桑那州立大學的地質學家表示,74000年前的超級火山爆發並未在東非引發造成人類數目減少的嚴重環境破壞。
根據亞利桑那州立大學的地質學家所述,大約74000年前發生在蘇門答臘的多峇超級火山爆發並未在東非造成長達6年的「火山冬天」,故該地區的人口也沒有因此而急速下降。
這項新發現駁斥了多峇巨災理論(Toba catastrophe hypothesis)。該理論認為火山噴發和後續效應使東非陷入了數年的酷寒,造成嚴重的生態浩劫。
「這是首度有研究提供直接證據顯示噴發不久之前和之後的植被狀況,進而指出多峇火山爆發對植被的影響。」主要作者,亞利桑那州立大學地質科學系的博士候選人Chad L. Yost表示。「對於東非的植被生長狀況來說,多峇火山爆發並未造成顯著的負面衝擊。」
利用沖刷至湖泊然後堆積在湖底的植物部件,研究人員可以重建某個地區過往的生態系樣貌。Yost和同事研究的微小植物碎屑保存於馬拉威湖的兩根沉積物岩芯當中,這座湖泊長約570公里,是東非大裂谷最南端的湖泊。
之前的研究曾在馬拉威湖的岩芯當中找到來自於多峇火山爆發的物質,它們可以指出噴發時間並讓Yost和同事得以追溯多峇火山爆發之前100年和之後200年間發生的事物。研究團隊在這300年區間中,平均每隔8.5年便分析一個代表性樣品。
「結果相當令人驚訝。」Yost表示。「基於多峇火山爆發的規模,你可能會預料有嚴重的冷化現象發生――但我們卻沒有看到。」
Yost和他的同事並未看到低海拔的植被在噴發過後有顯著變化,但團隊確實發現噴發剛結束時,某些山區植物有消失的跡象。他說噴發造成的冷化可能對不耐寒的植物造成了損害。
Yost表示如果此區域在多峇火山噴發之後歷經了長達數年的嚴重冷化,則岩芯呈現的證據應該會指出該區域各海拔的植被都經歷了大規模死亡。
多峇巨災理論中的一部份認為該次噴發造成人類數目大幅減少。
「我們知道當時馬拉威湖周遭的50公里以內有解剖學上的現代人生活著,」Yost表示。「人類或許可以搬遷到其他棲地或者低海拔地區,多峇火山爆發造成的冷化效應對這些地方只有些微影響或者根本沒有。」
他說該地區已知的多數考古場址都是位在低海拔地區而非山區。
共同作者,亞利桑那州立大學地質科學系的特聘教授 Andrew S. Cohen表示:「發生在地球歷史75000年前的單一事件,造成人類搖籃的人口數大幅縮減的說法並不成立。」
研究團隊的論文「Subdecadal phytolith and charcoal records from Lake Malawi, East Africa imply minimal effects on human evolution from the ~74 ka Toba supereruption」本周發表在《人類演化期刊》(Journal of Human Evolution)
YostCohen's共同進行研究的作者包括德州大學奧斯汀分校的Lily J. Jackson和印第安納州立大學的Jeffery R. Stone。資金來源則是美國國家科學基金會和國際陸地科學鑽探計畫。
Cohen是馬拉威湖鑽探計畫的主要研究人員之一,他說這項合作計畫於2005年從湖底成功取出了岩芯。馬拉威湖是地球上最深的湖泊之一,其岩芯所保存的物質紀錄可以追溯至超過100萬年以前。
沖刷至湖裡的動植物組織會一年一年地層層堆積在湖底,因此湖泊本身和周遭陸地的過往環境變化會被記錄在沉積物岩芯當中。
Yost的研究取自於湖泊的兩根岩芯:一根來自靠近山區的湖泊北端,另一根則是在湖泊的中心地帶。Cohen表示過往其他研究人員已經精確指出岩芯中的哪個層位含有來自多峇火山爆發的玻璃質和晶體。
Yost從岩芯中取出橫跨火山爆發前後區段的樣品,並分析其中的木炭以及含有矽質的植物組織――植矽體(phytolith)
Yost的專長為辨識特定植矽體是來自於何種植物,他說這項研究需要盯著顯微鏡數百個小時才得以完成。
如果多峇巨災理論為真,那麼大規模死亡的植被應該會使野火的發生次數增加,造成更多木炭被沖刷到湖裡。然而,他在噴發之後堆積的沉積物中,並沒有觀察到木炭數量增加至超過正常變動範圍之外。
「我們判定多峇火山爆發對生長在東非的植被並沒有造成重大的負面影響,」Yost表示。「我們希望這項結果可以成為宣告多峇巨災理論為錯誤的關鍵證據。」

No Volcanic Winter in East Africa From Ancient Toba Eruption
The supereruption 74,000 years ago did not trigger major environmental disruption that caused human populations in East Africa to decline, UA geoscientists say.
The massive Toba volcanic eruption on the island of Sumatra about 74,000 years ago did not cause a six-year-long "volcanic winter" in East Africa and thereby cause the human population in the region to plummet, according to new research from University of Arizona geoscientists.
The new findings disagree with the Toba catastrophe hypothesis, which says the eruption and its aftermath caused drastic, multiyear cooling and severe ecological disruption in East Africa.
"This is the first research that provides direct evidence for the effects of the Toba eruption on vegetation just before and just after the eruption," said lead author Chad L. Yost, a doctoral candidate in the UA Department of Geosciences. "The Toba eruption had no significant negative impact on vegetation growing in East Africa."
Researchers can use ancient plant parts that wash into and accumulate on the bottoms of lakes to reconstruct a region's past ecosystem. Yost and his colleagues studied microscopic bits of plants preserved in two sediment cores from Lake Malawi, which is approximately 570 kilometers (354 miles) long and is the southernmost of the East African Rift lakes.
Previous investigators found material from the Toba eruption in the Lake Malawi cores. That material pinpoints the time of the eruption and allowed Yost and colleagues to peer back in time 100 years before to 200 years after the Toba eruption. The team analyzed samples that represented, on average, every 8.5 years within that 300-year interval.
"It is surprising," Yost said. "You would have expected severe cooling based on the size of the Toba eruption — yet that's not what we see."
Yost and his colleagues did not find marked changes in lower-elevation vegetation post-eruption. The team did find some die-off of mountain plants just after the eruption. Cooling from the eruption might have injured frost-intolerant plants, he said.
Had the region experienced the drastic, multiyear cooling post-Toba, the cores would have evidence of a massive die-off of the region's vegetation at all elevations, Yost said.
Part of the Toba catastrophe hypothesis suggests the eruption caused human populations to shrink.
"We know anatomically modern humans were living within 50 kilometers of Lake Malawi," Yost said. "People would have been able to travel to habitats and lower elevations that had little to no cooling effect from the Toba eruption."
Most of the region's known archaeological sites are from low elevations, not the mountains, he said.
Co-author Andrew S. Cohen, UA Distinguished Professor of Geosciences, said, "That a singular event in Earth history 75,000 years ago caused human populations in the cradle of humankind to drop is not a tenable idea."
The team's paper, "Subdecadal phytolith and charcoal records from Lake Malawi, East Africa imply minimal effects on human evolution from the ~74 ka Toba supereruption," is published online this week in the Journal of Human Evolution.
Yost's and Cohen's co-authors are Lily J. Jackson of the University of Texas, Austin, and Jeffery R. Stone of Indiana State University. The National Science Foundation and the International Continental Scientific Drilling Program funded the research.
The Lake Malawi Drilling Project took the cores from the lake bottom in 2005, said Cohen, one of the principal investigators on the collaborative project. The lake is one of the deepest in the world. The material archived in the cores goes back more than 1 million years.
Plant and animal material washes into lakes and is deposited on the bottom in annual layers, so a sediment core contains a record of the past environments of a lake and of the surrounding land.
Yost studied two cores taken from the lake: one from the north end of the lake, which is closer to the mountains, and the other from the central part of the lake. Other researchers had pinpointed what layer in those cores had glass and crystals from the Toba eruption, Cohen said.
Yost took samples from the cores that straddled the eruption and analyzed the samples for charcoal and for silica-containing plant parts called phytoliths.
The work required hundreds of hours of peering through a microscope, said Yost, an expert in identifying the type of plant a particular phytolith came from.
If the Toba catastrophe hypothesis is true, the massive die-off of vegetation would have resulted in more wildfires and therefore more charcoal washing into the lake. However, he did not find an increase in charcoal outside the range of normal variability in the sediments deposited after the eruption.
"We determined that the Toba eruption had no significant negative impact on vegetation growing in East Africa," Yost said. "We hope this will put the final nail in the coffin of the Toba catastrophe hypothesis."
原始論文:Chad L. Yost, Lily J. Jackson, Jeffery R. Stone, Andrew S. Cohen. Subdecadal phytolith and charcoal records from Lake Malawi, East Africa imply minimal effects on human evolution from the 74 ka Toba supereruptionJournal of Human Evolution, 2018; 116: 75 DOI: 10.1016/j.jhevol.2017.11.005
引用自:University of Arizona. "No volcanic winter in East Africa from ancient Toba eruption."