Understanding Ocean Acidification
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Drought and Ecosystem Carbon Cycling
Agricultural and Forest Meteorology 151 (2011) 765–773 Contents lists available at ScienceDirect Agricultural and Forest Meteorology journal homepage: www.elsevier.com/locate/agrformet Review Drought and ecosystem carbon cycling M.K. van der Molen a,b,∗, A.J. Dolman a, P. Ciais c, T. Eglin c, N. Gobron d, B.E. Law e, P. Meir f, W. Peters b, O.L. Phillips g, M. Reichstein h, T. Chen a, S.C. Dekker i, M. Doubková j, M.A. Friedl k, M. Jung h, B.J.J.M. van den Hurk l, R.A.M. de Jeu a, B. Kruijt m, T. Ohta n, K.T. Rebel i, S. Plummer o, S.I. Seneviratne p, S. Sitch g, A.J. Teuling p,r, G.R. van der Werf a, G. Wang a a Department of Hydrology and Geo-Environmental Sciences, Faculty of Earth and Life Sciences, VU-University Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands b Meteorology and Air Quality Group, Wageningen University and Research Centre, P.O. box 47, 6700 AA Wageningen, The Netherlands c LSCE CEA-CNRS-UVSQ, Orme des Merisiers, F-91191 Gif-sur-Yvette, France d Institute for Environment and Sustainability, EC Joint Research Centre, TP 272, 2749 via E. Fermi, I-21027 Ispra, VA, Italy e College of Forestry, Oregon State University, Corvallis, OR 97331-5752 USA f School of Geosciences, University of Edinburgh, EH8 9XP Edinburgh, UK g School of Geography, University of Leeds, Leeds LS2 9JT, UK h Max Planck Institute for Biogeochemistry, PO Box 100164, D-07701 Jena, Germany i Department of Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht University, PO Box 80115, 3508 TC Utrecht, The Netherlands j Institute of Photogrammetry and Remote Sensing, Vienna University of Technology, Gusshausstraße 27-29, 1040 Vienna, Austria k Geography and Environment, Boston University, 675 Commonwealth Avenue, Boston, MA 02215, USA l Department of Global Climate, Royal Netherlands Meteorological Institute, P.O. -
Forestry As a Natural Climate Solution: the Positive Outcomes of Negative Carbon Emissions
PNW Pacific Northwest Research Station INSIDE Tracking Carbon Through Forests and Streams . 2 Mapping Carbon in Soil. .3 Alaska Land Carbon Project . .4 What’s Next in Carbon Cycle Research . 4 FINDINGS issue two hundred twenty-five / march 2020 “Science affects the way we think together.” Lewis Thomas Forestry as a Natural Climate Solution: The Positive Outcomes of Negative Carbon Emissions IN SUMMARY Forests are considered a natural solu- tion for mitigating climate change David D’A more because they absorb and store atmos- pheric carbon. With Alaska boasting 129 million acres of forest, this state can play a crucial role as a carbon sink for the United States. Until recently, the vol- ume of carbon stored in Alaska’s forests was unknown, as was their future car- bon sequestration capacity. In 2007, Congress passed the Energy Independence and Security Act that directed the Department of the Inte- rior to assess the stock and flow of carbon in all the lands and waters of the United States. In 2012, a team com- posed of researchers with the U.S. Geological Survey, U.S. Forest Ser- vice, and the University of Alaska assessed how much carbon Alaska’s An unthinned, even-aged stand in southeast Alaska. New research on carbon sequestration in the region’s coastal temperate rainforests, and how this may change over the next 80 years, is helping land managers forests can sequester. evaluate tradeoffs among management options. The researchers concluded that ecosys- tems of Alaska could be a substantial “Stones have been known to move sunlight, water, and atmospheric carbon diox- carbon sink. -
Carbon Cycling and Biosequestration Integrating Biology and Climate Through Systems Science March 2008 Workshop Report
Carbon Cycling and Biosequestration Integrating Biology and Climate through Systems Science March 2008 Workshop Report http://genomicsgtl.energy.gov/carboncycle/ ne of the most daunting challenges facing science in processes that drive the global carbon cycle, (2) achieve greater the 21st Century is to predict how Earth’s ecosystems integration of experimental biology and biogeochemical mod- will respond to global climate change. The global eling approaches, (3) assess the viability of potential carbon Ocarbon cycle plays a central role in regulating atmospheric biosequestration strategies, and (4) develop novel experimental carbon dioxide (CO2) levels and thus Earth’s climate, but our approaches to validate climate model predictions. basic understanding of the myriad tightly interlinked biologi- cal processes that drive the global carbon cycle remains lim- A Science Strategy for the Future ited. Whether terrestrial and ocean ecosystems will capture, Understanding and predicting processes of the global carbon store, or release carbon is highly dependent on how changing cycle will require bold new research approaches aimed at linking climate conditions affect processes performed by the organ- global-scale climate phenomena; biogeochemical processes of isms that form Earth’s biosphere. Advancing our knowledge ecosystems; and functional activities encoded in the genomes of of biological components of the global carbon cycle is crucial microbes, plants, and biological communities. This goal presents to predicting potential climate change impacts, assessing the a formidable challenge, but emerging systems biology research viability of climate change adaptation and mitigation strate- approaches provide new opportunities to bridge the knowledge gies, and informing relevant policy decisions. gap between molecular- and global-scale phenomena. -
Aragonite Formation in Confinements: a Step Toward Understanding Polymorph Control COMMENTARY Yifei Xua,B,C and Nico A
COMMENTARY Aragonite formation in confinements: A step toward understanding polymorph control COMMENTARY Yifei Xua,b,c and Nico A. J. M. Sommerdijka,b,c,1 Calcium carbonate (CaCO3) is one of the most com- unclear but were generally attributed to the interac- mon minerals on Earth; it not only forms rocks like tion between the acidic functional groups of the limestone or marble but is also a main component of biomacromolecules and the mineral components. Ad- biominerals such as pearls, the nacre of seashells, and ditionally, it was reported that a macromolecular sea-urchin skeletons (1). Despite many years of re- hydrogel-like 3D network is formed before the miner- search, the polymorphism of CaCO3 is still far from alization of nacre (11), which may play a role in the being understood. CaCO3 has three anhydrous crys- crystallization process by confining the crystallization talline forms: calcite, aragonite, and vaterite, with a to defined small volumes. Nonetheless, confinement decreasing thermodynamic stability under aqueous has never been directly correlated with aragonite for- ambient conditions (calcite > aragonite > vaterite) mation in biominerals, although its capability of con- (2). While vaterite is rare in nature, calcite and arago- trolling crystal orientation and polymorphism has nite are both frequently found in rocks or biominerals been shown in many recent reports (12–15). (1). A well-known example is the aragonite structure of Now, Zeng et al. (5) explore for the first time the nacre (3), where the organization of the crystals leads impact of confinement on aragonite formation. By to extraordinary mechanical performance. However, precipitating CaCO3 within the cylindrical pores of in synthetic systems, crystallization experiments only track-etched membranes (Fig. -
The Carbon Cycle
The Carbon Cycle Overview of the Carbon Cycle The movement of carbon from one area to another is the basis for the carbon cycle. Carbon is important for all life on Earth. All living things are made up of carbon. Carbon is produced by both natural and human-made (anthropogenic) sources. Carbon Cycle Page 1 Nature’s Carbon Sources Carbon is found in the Carbon is found in the lithosphere Carbon is found in the Carbon is found in the atmosphere mostly as carbon in the form of carbonate rocks. biosphere stored in plants and hydrosphere dissolved in ocean dioxide. Animal and plant Carbonate rocks came from trees. Plants use carbon dioxide water and lakes. respiration place carbon into ancient marine plankton that sunk from the atmosphere to make the atmosphere. When you to the bottom of the ocean the building blocks of food Carbon is used by many exhale, you are placing carbon hundreds of millions of years ago during photosynthesis. organisms to produce shells. dioxide into the atmosphere. that were then exposed to heat Marine plants use cabon for and pressure. photosynthesis. The organic matter that is produced Carbon is also found in fossil fuels, becomes food in the aquatic such as petroleum (crude oil), coal, ecosystem. and natural gas. Carbon is also found in soil from dead and decaying animals and animal waste. Carbon Cycle Page 2 Natural Carbon Releases into the Atmosphere Carbon is released into the atmosphere from both natural and man-made causes. Here are examples to how nature places carbon into the atmosphere. -
Characteristics and Crystal Structure of Calcareous Deposit Films Formed by Electrodeposition Process in Artificial and Natural Seawater
coatings Article Characteristics and Crystal Structure of Calcareous Deposit Films Formed by Electrodeposition Process in Artificial and Natural Seawater Jun-Mu Park 1, Myeong-Hoon Lee 1 and Seung-Hyo Lee 2,* 1 Division of Marine Engineering, Korea Maritime and Ocean University, Busan 49112, Korea; [email protected] (J.-M.P.); [email protected] (M.-H.L.) 2 Department of Ocean Advanced Materials Convergence Engineering, Korea Maritime and Ocean University, Busan 49112, Korea * Correspondence: [email protected] Abstract: In this study, we tried to form the calcareous deposit films by the electrodeposition process. The uniform and compact calcareous deposit films were formed by electrodeposition process and their crystal structure and characteristics were analyzed and evaluated using various surface analytical techniques. The mechanism of formation for the calcareous deposit films could be confirmed and the role of magnesium was verified by experiments in artificial and natural seawater solutions. The highest amount of the calcareous deposit film was obtained at 5 A/m2 while current densities between 1–3 A/m2 facilitated the formation of the most uniform and dense layers. In addition, the adhesion characteristics were found to be the best at 3 A/m2. The excellent characteristics of the calcareous deposit films were obtained when the dense film of brucite-Mg(OH)2 and metastable aragonite-CaCO3 was formed in the appropriate ratio. Citation: Park, J.-M.; Lee, M.-H.; Lee, Keywords: electrodeposition process; calcareous deposit films; aragonite crystal structure; seawater S.-H. Characteristics and Crystal Structure of Calcareous Deposit Films Formed by Electrodeposition Process in Artificial and Natural Seawater. -
Permafrost Soils and Carbon Cycling
SOIL, 1, 147–171, 2015 www.soil-journal.net/1/147/2015/ doi:10.5194/soil-1-147-2015 SOIL © Author(s) 2015. CC Attribution 3.0 License. Permafrost soils and carbon cycling C. L. Ping1, J. D. Jastrow2, M. T. Jorgenson3, G. J. Michaelson1, and Y. L. Shur4 1Agricultural and Forestry Experiment Station, Palmer Research Center, University of Alaska Fairbanks, 1509 South Georgeson Road, Palmer, AK 99645, USA 2Biosciences Division, Argonne National Laboratory, Argonne, IL 60439, USA 3Alaska Ecoscience, Fairbanks, AK 99775, USA 4Department of Civil and Environmental Engineering, University of Alaska Fairbanks, Fairbanks, AK 99775, USA Correspondence to: C. L. Ping ([email protected]) Received: 4 October 2014 – Published in SOIL Discuss.: 30 October 2014 Revised: – – Accepted: 24 December 2014 – Published: 5 February 2015 Abstract. Knowledge of soils in the permafrost region has advanced immensely in recent decades, despite the remoteness and inaccessibility of most of the region and the sampling limitations posed by the severe environ- ment. These efforts significantly increased estimates of the amount of organic carbon stored in permafrost-region soils and improved understanding of how pedogenic processes unique to permafrost environments built enor- mous organic carbon stocks during the Quaternary. This knowledge has also called attention to the importance of permafrost-affected soils to the global carbon cycle and the potential vulnerability of the region’s soil or- ganic carbon (SOC) stocks to changing climatic conditions. In this review, we briefly introduce the permafrost characteristics, ice structures, and cryopedogenic processes that shape the development of permafrost-affected soils, and discuss their effects on soil structures and on organic matter distributions within the soil profile. -
The Crystallization Process of Vaterite Microdisc Mesocrystals Via Proto-Vaterite Amorphous Calcium Carbonate Characterized by Cryo-X-Ray Absorption Spectroscopy
crystals Communication The Crystallization Process of Vaterite Microdisc Mesocrystals via Proto-Vaterite Amorphous Calcium Carbonate Characterized by Cryo-X-ray Absorption Spectroscopy Li Qiao 1, Ivo Zizak 2, Paul Zaslansky 3 and Yurong Ma 1,* 1 School of Chemistry and Chemical Engineering, Beijing Institute of Technology, Beijing 100081, China; [email protected] 2 Department Structure and Dynamics of Energy Materials, Helmholtz-Zentrum-Berlin, 14109 Berlin, Germany; [email protected] 3 Department for Operative and Preventive Dentistry, Charité-Universitätsmedizin Berlin, 10117 Berlin, Germany; [email protected] * Correspondence: [email protected] Received: 27 July 2020; Accepted: 23 August 2020; Published: 26 August 2020 Abstract: Investigation on the formation mechanism of crystals via amorphous precursors has attracted a lot of interests in the last years. The formation mechanism of thermodynamically meta-stable vaterite in pure alcohols in the absence of any additive is less known. Herein, the crystallization process of vaterite microdisc mesocrystals via proto-vaterite amorphous calcium carbonate (ACC) in isopropanol was tracked by using Ca K-edge X-ray absorption spectroscopy (XAS) characterization under cryo-condition. Ca K-edge X-ray absorption near edge structure (XANES) spectra show that the absorption edges of the Ca ions of the vaterite samples with different crystallization times shift to lower photoelectron energy while increasing the crystallization times from 0.5 to 20 d, indicating the increase of crystallinity degree of calcium carbonate. Ca K-edge extended X-ray absorption fine structure (EXAFS) spectra exhibit that the coordination number of the nearest neighbor atom O around Ca increases slowly with the increase of crystallization time and tends to be stable as 4.3 ( 1.4). -
The Carbon Cycle and Climate Change/J Bret Bennington – First Edition ISBN 1 3: 978-0-495-73855-8;;, ISBN 1 0: 0-495-73855-7
38557_00_cover.qxd 12/24/08 4:36 PM Page 1 The collection of chemical pathways by which carbon moves between Earth systems is called the carbon cycle and it is the flow of carbon through this cycle that ties together the functioning of the Earth’s atmosphere, biosphere, geosphere, and oceans to regulate the climate of our planet. This means that as drivers of planet Earth, anything we do to change the function or state of one Earth system will change the function and state of all Earth systems. If we change the composition of the atmosphere, we will also cause changes to propagate through the biosphere, hydrosphere, and geosphere, altering our planet in ways that will likely not be beneficial to human welfare. Understanding the functioning of the carbon cycle in detail so that we can predict the effects of human activities on the Earth and its climate is one of the most important scientific challenges of the 21st century. Package this module with any Cengage Learning text where learning about the car- bon cycle and humanity’s impact on the environment is important. About the Author Dr. J Bret Bennington grew up on Long Island and studied geology as an under- graduate at the University of Rochester in upstate New York. He earned his doctorate in Paleontology from the Department of Geological Sciences at Virginia Tech in 1995 and has been on the faculty of the Department of Geology at Hofstra University since 1993. Dr. Bennington’s research is focused on quantifying stability and change in marine benthic paleocommunities in the fossil record and on integrating paleontological and sedimentological data to understand the development of depositional sequences in both Carboniferous and Cretaceous marine environments. -
Ocean Acidification! What Is It? Why Does It Matter? What Can I Do About It?
Promoting Climate Literacy College Course Outreach Activity Ocean Acidification! What is it? Why does it matter? What can I do about it? Synopsis of the Activity Learners investigate what ocean acidification is, what causes it, and how it affects marine organisms through a series of hands-on activities, discussions and short exploration of text. Audience This activity is designed for the general public and is best accessed by learners in middle school or older. It is best done with small groups of visitors. Setting This activity works well as a cart anywhere in an informal science setting. Activity Goals Learners will gain a deeper understanding of: a. What is ocean acidification? b. What causes ocean acidification? c. What organisms are affected by ocean acidification? d. Where is ocean acidification happening? e. What actions they can take to decrease ocean acidification in the future? Concepts 1. Since the start of the Industrial Revolution, the ocean has gotten about 25% more acidic. This has been caused by excess CO2 entering the atmosphere and then being absorbed by the ocean. The extra CO2 comes from the burning of fossil fuels from human industry. 2. Some organisms with exoskeletons and shells will have difficulty building hard parts and others’ hard parts may dissolve due to ocean acidification. This will harm those species and other organisms that rely on the affected organisms within a food web. 3. Ocean acidification is happening globally, but some areas are experiencing higher levels of ocean acidification than others. 4. By taking steps to decrease our individual and collective carbon footprints, we can decrease the extent of ocean acidification in the future. -
Forest Carbon Primer
Forest Carbon Primer Updated May 5, 2020 Congressional Research Service https://crsreports.congress.gov R46312 SUMMARY R46312 Forest Carbon Primer May 5, 2020 The global carbon cycle is the process by which the element carbon moves between the air, land, ocean, and Earth’s crust. The movement of increasing amounts of carbon into the atmosphere, Katie Hoover particularly as greenhouse gases, is the dominant contributor to the observed warming trend in Specialist in Natural global temperatures. Forests are a significant part of the global carbon cycle, because they Resources Policy contain the largest store of terrestrial (land-based) carbon and continuously transfer carbon between the terrestrial biosphere and the atmosphere. Consequently, forest carbon optimization Anne A. Riddle and management strategies are often included in climate mitigation policy proposals. Analyst in Natural Resources Policy The forest carbon cycle starts with the sequestration and accumulation of atmospheric carbon due to tree growth. The accumulated carbon is stored in five different pools in the forest ecosystem: aboveground biomass (e.g., leaves, trunks, limbs), belowground biomass (e.g., roots), deadwood, litter (e.g., fallen leaves, stems), and soils. As trees or parts of trees die, the carbon cycles through those different pools, from the living biomass pools to the deadwood, litter, and soil pools. The length of time carbon stays in each pool varies considerably, ranging from months (litter) to millennia (soil). The cycle continues as carbon flows out of the forest ecosystem and returns to the atmosphere through several processes, including respiration, combustion, and decomposition. Carbon also leaves the forest ecosystem through timber harvests, by which it enters the product pool. -
Carbon Sequestration
Forest Management No. 32 UI Extension Forestry Information Series Carbon Sequestration... What’s That? Randy Brooks There has been growing concern about the amount of In 1992, nearly all countries in the world signed the carbon being emitted into the atmosphere, and the United Nations Framework Convention on Climate possible effect of those emissions on our climate. The Change (UNFCCC), establishing a long-term goal to amount of carbon dioxide (CO2) in the atmosphere is stabilize atmospheric concentrations of greenhouse rising, according to most sources, supposedly creating gases. Each party to the convention is committed to the global warming effect. Many observers have limiting greenhouse gas emissions and protecting and identified reducing fossil fuel emissions as the only enhancing greenhouse gas sinks and reservoirs. In solution to this global crisis, yet recent debate suggests December of 1997, as part of efforts to fulfill the this solution by itself is not economically feasible in Convention, international negotiators signed the Kyoto time to make a difference. Protocol in Japan. The protocol directs developed countries to reduce their emissions of CO and five Carbon is transferred to and from the earth’s atmosphere 2 other prominent greenhouse gases by at least 5% in a continuous cycle. CO and other gases that natu- 2 below 1990 levels between 2008-2012. The US is rally occur in the atmosphere capture solar radiation and committed to reductions of 7 percent and Canada to 6 reflect it back to earth. This warms the surface of the percent. earth and is referred to as the “greenhouse effect”. With- out this effect, our planet would be about 56 degrees F To help achieve these targets, the Protocol allows colder on average.