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Ice retreat in Wilkes Basin of East Antarctica during a warm interglacial 期刊论文
NATURE, 2020, 583 (7817) : 554-+
作者:  T. Blackburn;  G. H. Edwards;  S. Tulaczyk;  M. Scudder;  G. Piccione;  B. Hallet;  N. McLean;  J. C. Zachos;  B. Cheney;  J. T. Babbe
收藏  |  浏览/下载:21/0  |  提交时间:2020/08/09

Uranium isotopes in subglacial precipitates from the Wilkes Basin of the East Antarctic Ice Sheet reveal ice retreat during a warm Pleistocene interglacial period about 400,000 years ago.


Efforts to improve sea level forecasting on a warming planet have focused on determining the temperature, sea level and extent of polar ice sheets during Earth'  s past interglacial warm periods(1-3). About 400,000 years ago, during the interglacial period known as Marine Isotopic Stage 11 (MIS11), the global temperature was 1 to 2 degrees Celsius greater(2)and sea level was 6 to 13 metres higher(1,3). Sea level estimates in excess of about 10 metres, however, have been discounted because these require a contribution from the East Antarctic Ice Sheet(3), which has been argued to have remained stable for millions of years before and includes MIS11(4,5). Here we show how the evolution of(234)U enrichment within the subglacial waters of East Antarctica recorded the ice sheet'  s response to MIS11 warming. Within the Wilkes Basin, subglacial chemical precipitates of opal and calcite record accumulation of(234)U (the product of rock-water contact within an isolated subglacial reservoir) up to 20 times higher than that found in marine waters. The timescales of(234)U enrichment place the inception of this reservoir at MIS11. Informed by the(234)U cycling observed in the Laurentide Ice Sheet, where(234)U accumulated during periods of ice stability(6)and was flushed to global oceans in response to deglaciation(7), we interpret our East Antarctic dataset to represent ice loss within the Wilkes Basin at MIS11. The(234)U accumulation within the Wilkes Basin is also observed in the McMurdo Dry Valleys brines(8-10), indicating(11)that the brine originated beneath the adjacent East Antarctic Ice Sheet. The marine origin of brine salts(10)and bacteria(12)implies that MIS11 ice loss was coupled with marine flooding. Collectively, these data indicate that during one of the warmest Pleistocene interglacials, the ice sheet margin at the Wilkes Basin retreated to near the precipitate location, about 700 kilometres inland from the current position of the ice margin, which-assuming current ice volumes-would have contributed about 3 to 4 metres(13)to global sea levels.


  
Sick plants in grassland communities: a growth-defense trade-off is the main driver of fungal pathogen abundance 期刊论文
ECOLOGY LETTERS, 2020
作者:  Cappelli, Seraina L.;  Pichon, Noemie A.;  Kempel, Anne;  Allan, Eric
收藏  |  浏览/下载:9/0  |  提交时间:2020/06/01
Biodiversity experiment  functional traits  fungal exclusion experiment  fungal pathogen  growth-defense trade-off  nitrogen enrichment  
成熟森林吸收大气额外二氧化碳的能力有限 快报文章
气候变化快报,2020年第9期
作者:  裴惠娟
Microsoft Word(15Kb)  |  收藏  |  浏览/下载:356/0  |  提交时间:2020/04/30
Mature Forest  Carbon Dioxide Enrichment  
The fate of carbon in a mature forest under carbon dioxide enrichment 期刊论文
NATURE, 2020, 580 (7802) : 227-+
作者:  Sun, P. Z.;  Yang, Q.;  Kuang, W. J.;  Stebunov, Y. V.;  Xiong, W. Q.;  Yu, J.;  Nair, R. R.;  Katsnelson, M. I.;  Yuan, S. J.;  Grigorieva, I. V.;  Lozada-Hidalgo, M.;  Wang, F. C.;  Geim, A. K.
收藏  |  浏览/下载:70/0  |  提交时间:2020/05/13

Carbon dioxide enrichment of a mature forest resulted in the emission of the excess carbon back into the atmosphere via enhanced ecosystem respiration, suggesting that mature forests may be limited in their capacity to mitigate climate change.


Atmospheric carbon dioxide enrichment (eCO(2)) can enhance plant carbon uptake and growth(1-5), thereby providing an important negative feedback to climate change by slowing the rate of increase of the atmospheric CO2 concentration(6). Although evidence gathered from young aggrading forests has generally indicated a strong CO2 fertilization effect on biomass growth(3-5), it is unclear whether mature forests respond to eCO(2) in a similar way. In mature trees and forest stands(7-10), photosynthetic uptake has been found to increase under eCO(2) without any apparent accompanying growth response, leaving the fate of additional carbon fixed under eCO(2) unclear(4,5,7-11). Here using data from the first ecosystem-scale Free-Air CO2 Enrichment (FACE) experiment in a mature forest, we constructed a comprehensive ecosystem carbon budget to track the fate of carbon as the forest responded to four years of eCO(2) exposure. We show that, although the eCO(2) treatment of +150 parts per million (+38 per cent) above ambient levels induced a 12 per cent (+247 grams of carbon per square metre per year) increase in carbon uptake through gross primary production, this additional carbon uptake did not lead to increased carbon sequestration at the ecosystem level. Instead, the majority of the extra carbon was emitted back into the atmosphere via several respiratory fluxes, with increased soil respiration alone accounting for half of the total uptake surplus. Our results call into question the predominant thinking that the capacity of forests to act as carbon sinks will be generally enhanced under eCO(2), and challenge the efficacy of climate mitigation strategies that rely on ubiquitous CO2 fertilization as a driver of increased carbon sinks in global forests.


  
Parental-to-embryo switch of chromosome organization in early embryogenesis 期刊论文
NATURE, 2020: 142-+
作者:  Kim, Eugene;  Kerssemakers, Jacob;  Shaltiel, Indra A.;  Haering, Christian H.;  Dekker, Cees
收藏  |  浏览/下载:18/0  |  提交时间:2020/07/03

Single-cell allelic HiC analysis, combined with allelic gene expression and chromatin states, reveals parent-of-origin-specific dynamics of chromosome organization and gene expression during mouse preimplantation development.


Paternal and maternal epigenomes undergo marked changes after fertilization(1). Recent epigenomic studies have revealed the unusual chromatin landscapes that are present in oocytes, sperm and early preimplantation embryos, including atypical patterns of histone modifications(2-4) and differences in chromosome organization and accessibility, both in gametes(5-8) and after fertilization(5,8-10). However, these studies have led to very different conclusions: the global absence of local topological-associated domains (TADs) in gametes and their appearance in the embryo(8,9) versus the pre-existence of TADs and loops in the zygote(5,11). The questions of whether parental structures can be inherited in the newly formed embryo and how these structures might relate to allele-specific gene regulation remain open. Here we map genomic interactions for each parental genome (including the X chromosome), using an optimized single-cell high-throughput chromosome conformation capture (HiC) protocol(12,13), during preimplantation in the mouse. We integrate chromosome organization with allelic expression states and chromatin marks, and reveal that higher-order chromatin structure after fertilization coincides with an allele-specific enrichment of methylation of histone H3 at lysine 27. These early parental-specific domains correlate with gene repression and participate in parentally biased gene expression-including in recently described, transiently imprinted loci(14). We also find TADs that arise in a non-parental-specific manner during a second wave of genome assembly. These de novo domains are associated with active chromatin. Finally, we obtain insights into the relationship between TADs and gene expression by investigating structural changes to the paternal X chromosome before and during X chromosome inactivation in preimplantation female embryos(15). We find that TADs are lost as genes become silenced on the paternal X chromosome but linger in regions that escape X chromosome inactivation. These findings demonstrate the complex dynamics of three-dimensional genome organization and gene expression during early development.


  
Mechanism of adrenergic Ca(V)1.2 stimulation revealed by proximity proteomics 期刊论文
NATURE, 2020, 577 (7792) : 695-+
作者:  Peng, Guangdun;  Suo, Shengbao;  Cui, Guizhong;  Yu, Fang;  Wang, Ran;  Chen, Jun;  Chen, Shirui;  Liu, Zhiwen;  Chen, Guoyu;  Qian, Yun;  Tam, Patrick P. L.;  Han, Jing-Dong J.;  Jing, Naihe
收藏  |  浏览/下载:26/0  |  提交时间:2020/07/03

An in vivo approach to identify proteins whose enrichment near cardiac Ca(V)1.2 channels changes upon beta-adrenergic stimulation finds the G protein Rad, which is phosphorylated by protein kinase A, thereby relieving channel inhibition by Rad and causing an increased Ca2+ current.


Increased cardiac contractility during the fight-or-flight response is caused by beta-adrenergic augmentation of Ca(V)1.2 voltage-gated calcium channels(1-4). However, this augmentation persists in transgenic murine hearts expressing mutant Ca(V)1.2 alpha(1C) and beta subunits that can no longer be phosphorylated by protein kinase A-an essential downstream mediator of beta-adrenergic signalling-suggesting that non-channel factors are also required. Here we identify the mechanism by which beta-adrenergic agonists stimulate voltage-gated calcium channels. We express alpha(1C) or beta(2B) subunits conjugated to ascorbate peroxidase(5) in mouse hearts, and use multiplexed quantitative proteomics(6,7) to track hundreds of proteins in the proximity of Ca(V)1.2. We observe that the calcium-channel inhibitor Rad(8,9), a monomeric G protein, is enriched in the Ca(V)1.2 microenvironment but is depleted during beta-adrenergic stimulation. Phosphorylation by protein kinase A of specific serine residues on Rad decreases its affinity for beta subunits and relieves constitutive inhibition of Ca(V)1.2, observed as an increase in channel open probability. Expression of Rad or its homologue Rem in HEK293T cells also imparts stimulation of Ca(V)1.3 and Ca(V)2.2 by protein kinase A, revealing an evolutionarily conserved mechanism that confers adrenergic modulation upon voltage-gated calcium channels.


  
An orbital water-ice cycle on comet 67P from colour changes 期刊论文
NATURE, 2020, 578 (7793) : 49-+
作者:  Oh, Myoung Hwan;  Cho, Min Gee;  Chung, Dong Young;  Park, Inchul;  Kwon, Youngwook Paul;  Ophus, Colin;  Kim, Dokyoon;  Kim, Min Gyu;  Jeong, Beomgyun;  Gu, X. Wendy;  Jo, Jinwoung;  Yoo, Ji Mun;  Hong, Jaeyoung;  McMains, Sara;  Kang, Kisuk;  Sung, Yung-Eun;  Alivisatos, A. Paul;  Hyeon, Taeghwan
收藏  |  浏览/下载:52/0  |  提交时间:2020/07/03

Solar heating of a cometary surface provides the energy necessary to sustain gaseous activity, through which dust is removed(1,2). In this dynamical environment, both the coma(3,4) and the nucleus(5,6) evolve during the orbit, changing their physical and compositional properties. The environment around an active nucleus is populated by dust grains with complex and variegated shapes(7), lifted and diffused by gases freed from the sublimation of surface ices(8,9). The visible colour of dust particles is highly variable: carbonaceous organic material-rich grains(10) appear red while magnesium silicate-rich(11,12) and water-ice-rich(13,14) grains appear blue, with some dependence on grain size distribution, viewing geometry, activity level and comet family type. We know that local colour changes are associated with grain size variations, such as in the bluer jets made of submicrometre grains on comet Hale-Bopp(15) or in the fragmented grains in the coma(16) of C/1999 S4 (LINEAR). Apart from grain size, composition also influences the coma'  s colour response, because transparent volatiles can introduce a substantial blueing in scattered light, as observed in the dust particles ejected after the collision of the Deep Impact probe with comet 9P/Tempel 1(17). Here we report observations of two opposite seasonal colour cycles in the coma and on the surface of comet 67P/Churyumov-Gerasimenko through its perihelion passage(18). Spectral analysis indicates an enrichment of submicrometre grains made of organic material and amorphous carbon in the coma, causing reddening during the passage. At the same time, the progressive removal of dust from the nucleus causes the exposure of more pristine and bluish icy layers on the surface. Far from the Sun, we find that the abundance of water ice on the nucleus is reduced owing to redeposition of dust and dehydration of the surface layer while the coma becomes less red.


  
Global change biology: A primer 期刊论文
GLOBAL CHANGE BIOLOGY, 2020, 26 (1) : 3-30
作者:  Sage, Rowan F.
收藏  |  浏览/下载:9/0  |  提交时间:2020/02/17
biodiversity  climate change  CO2 enrichment  eutrophication  extinction  global change driver  invasive species  land transformation  
The acclimation of leaf photosynthesis of wheat and rice to seasonal temperature changes in T-FACE environments 期刊论文
GLOBAL CHANGE BIOLOGY, 2019
作者:  Cai, Chuang;  Li, Gang;  Di, Lijun;  Ding, Yunjie;  Fu, Lin;  Guo, Xuanhe;  Struik, Paul C.;  Pan, Genxing;  Li, Haozheng;  Chen, Weiping;  Luo, Weihong;  Yin, Xinyou
收藏  |  浏览/下载:8/0  |  提交时间:2019/11/27
climate change  free-air CO2 enrichment  growth temperature  leaf nitrogen content  Oryza sativa L  photosynthesis model  stomatal conductance  Triticum aestivum L  
Tropical forest subjected to intensive post-logging silviculture maintains functionally diverse dung beetle communities 期刊论文
FOREST ECOLOGY AND MANAGEMENT, 2019, 444: 318-326
作者:  Cerullo, G. R.;  Edwards, F. A.;  Mills, S. C.;  Edwards, D. P.
收藏  |  浏览/下载:9/0  |  提交时间:2019/11/27
REDD  Silviculture  Restoration  Biodiversity  Enrichment planting  Lianas  Sustainable forest management