Table S1. Concentrations of dissolved inorganic nitrogen (DIN) and phosphate (DIP)

Size: px
Start display at page:

Download "Table S1. Concentrations of dissolved inorganic nitrogen (DIN) and phosphate (DIP)"

Transcription

1 Table S1. Concentrations of dissolved inorganic nitrogen (DIN) and phosphate (DIP) before and at the end of incubations at different nutrient conditions, and particulate organic nitrogen (PON) concentration at the end of incubations. DIN (μmol L 1 ) DIP (μmol L 1 ) PON (μmol L 1 ) HNHP Before 11 ± ±.2 End 92.8 ± 9.7 ± ± 2.7 Molar drawdown 8. ± 1.7 ±.2 LN Before 8.8 ±.1 End 1. ± 9. ± 2.9 Molar drawdown 7.8 ± LP Before ±.1 End < ± 2.7 Molar drawdown ±.1 PON concentration was calculated based on PON quota and cell number at the end of incubation.

2 Table S2. Carbonate chemistry parameters of the media before and at the end of incubations at different nutrient conditions and pco 2 levels. pco 2 (μatm) ph (total TA (μmol DIC (μmol HCO (μmol 2 CO (μmol CO 2 (μmol Ω calcite scale) L 1 ) L 1 ) L 1 ) L 1 ) L 1 ) HNHP LC Before 51±17 a 8.4±1 a 2228±17 a 24±2 a 1829±21 a 159±2 a 1±1 a.8±.1 a End 428±57 b 8.11±5 b 2225±24 a 197±22 b 177±4 b 18±18 a 14±2 b 4.±.5 a HC Before 1±5 a 7.71±2 a 2219±19 a 211±22 a 21±22 a 81±2 a 9±2 a 1.9±.1 a End 95±19 b 7.81± b 2225±24 a 298± b 19±17 b ±14 b ±4 b ±. b LN LC Before 48±2 a 8.±2 a 224±1 a 197±1 a 179±1 a 12± a 1±1 a.9±.1 a End 91±9 b 8.± b 2±8 b 18±45 b 179±48 b 175±9 b 1±1 b 4.2±.2 b HC Before 1± a 7.7±2 a 221± a 215±7 a 198±9 a 85±4 a ±2 a 2±.1 a End 888±114 b 7.82±5 b 2142±8 b 21±47 b 189±49 b 98±8 b 29±4 b ±.2 b LP LC Before 97±1 a 8.14±2 a 2248± a 1982±22 a 1777±17 a 192±8 a 1±1 a 4.±.2 a End 5±24 b 8.1±2 a 2219±2 b 1942±22 b 171±25 b 199±8 a ±1 b 4.8±.2 a HC Before 114±11 a 7.7±4 a 2215±41 a 28±4 a 25±4 a 8±7 a 7±4 a 2.1±.2 a End 78±4 b 7.88±2 b 2228±14 a 284±11 b 1941± b 117± b 25±1 b 2.8±.1 b Different letters represent statistically differences between before and end of the experiments (Tukey Post hoc, p < 5). For more detail information, see Table 1.

3 Table S. Results of three-way ANOVAs for comparison of apparent light use efficiency (α) between growth, POC and PIC production rates at different CO 2 levels and nutrient conditions. Factor F value p value Factor F value p value α N 4.2 =48 P 4.1 <1 Para <1 Para 292. <1 C <.1 =.988 C 14.9 <1 N Para 1.2 <1 P Para 7.5 =2 N C 1.1 = P C 8. = Para C.2 =42 Para C 7.7 =2 N Para C =.54 P Para C.2 =54 α, slop of fitted curves for growth, POC and PIC production rates; N, dissolved inorganic nitrogen (DIN, μmol L 1 ); P, dissolved inorganic phosphate (DIP, μmol L 1 ); C, pco 2 (μatm); Para, growth rate (d 1 ), POC and PIC production rates (pg C cell 1 d 1 ).

4 Emiliania huxleyi N : P = 11 : 1.5 (HNHP) N : P = 8.8 : 1.5 (LN) N : P = 11 : (LP) 41 μatm pco 2 (LC) 925 μatm pco 2 (HC) 8,, 2, 2, 48 μ mol photons m 2 1 s PAR Interactive effects of ocean acidification, light intensity and nutrient availability on physiology and calcification of E. huxleyi Figure S1. A flow chart for the experimental treatments. PAR represents photosynthetically active radiation.

5 Carotenoid (pg cell 1 ) Chl a (pg cell 1 ) HNHP LN LP.18 (a).18 (b).18 (c) LC HC (d) (e) (f) Figure S2. At both LC and HC, light responses of Chl a contents at HNHP (a), LN (b) and LP (c) conditions. At both LC and HC, light responses of carotenoid contents at HNHP (d), LN (e) and LP (f) conditions. The values represent the mean ± standard deviation for four replicates.

6 ETR (mol e g 1 Chl a h 1 ) ETR (mol e g 1 Chl a h 1 ) ETR (mol e g 1 Chl a h 1 ) 48 2 ETR (mol e g 1 Chl a h 1 ) ETR (mol e g 1 Chl a h 1 ) LC HC HNHP (a) (b) LN (f) (g) LP (k) (l) 2 (c) (h) (m) (d) (i) (n) 8 (e) (j) (o) Light intensity ( mol electrons m 2 s 1 ) Light intensity ( mol electrons m 2 s 1 ) Light intensity ( mol electrons m 2 s 1 ) Figure S. Electron transport rate (ETR) of E. huxleyi as a function of instant light intensities, and fitted response curves of ETR to instant light intensities (P-I curves, dashed lines) emitted by the XE-PAM. Under HNHP, at both LC and HC, ETR as a

7 function of instant light intensities and the fitted P-I curves when E. huxleyi were incubated at 48 (a), 2 (b), 2 (c), (d), 8 (e) μmol photons m 2 s 1. Under LN, at both LC and HC, ETR as a function of instant light intensities and the fitted P-I curves when E. huxleyi were incubated at 48 (f), 2 (g), 2 (h), (i), 8 (j) μmol photons m 2 s 1. Under LP, at both LC and HC, ETR as a function of instant light intensities and the fitted P-I curves when E. huxleyi were incubated at 48 (k), 2 (l), 2 (m), (n), 8 (o) μmol photons m 2 s 1. Dashed lines were fitted according to Jasby and Platt (197). The values represent the mean ± standard deviation for four replicates.

8 I k ( mol photons m 2 s 1 ) alpha HNHP LN LP (a) (b) (c).2 LC HC (d) 9 (e) 9 (f) Figure S4. At both LC and HC, the slop (alpha) of fitted P-I curves of E. huxleyi as a function of incubation light intensities at HNHP (a), LN (b) and LP (c) conditions. At both LC and HC, fitted saturation light intensity (I k ) of E. huxleyi as a function of incubation light intensities at HNHP (d), LN (e) and LP (f) conditions. The values represent the mean ± standard deviation for four replicates.

9 PIC production rate (pg C cell 1 d 1 ) POC production rate (pg C cell 1 d 1 ) 1 14 (a) HNHP 1 14 (b) LN 1 14 (c) LP 1 8 LC HC (d) 9 (e) 9 (f) Figure S5. At both LC and HC, POC production rates of E. huixleyi as a function of light intensities at HNHP (a), LN (b) and LP (c) conditions. At both LC and HC, PIC production rates of E. huixleyi as a function of light intensities at HNHP (d), LN (e) and LP (f) conditions. The solid lines in each panel were fitted using the model provided by Eilers and Peeters (1988). The values represent the mean ± standard deviation for four replicates.

10 PON production rate (pg N cell 1 d 1 ) PON quota (pg N cell 1 ). HNHP LN (a). (b). (c) LP 1.8 LC HC (d) (e) (f) Figure S. At both LC and HC, PON quota of E. huixleyi as a function of light intensities at HNHP (a), LN (b) and LP (c) conditions. At both LC and HC, PON production rates of E. huixleyi as a function of light intensities at HNHP (d), LN (e) and LP (f) conditions. The solid lines in each panel were fitted using the model provided by Eilers and Peeters (1988). The values represent the mean ± standard deviation for four replicates.

Supplement of Simultaneous shifts in elemental stoichiometry and fatty acids of Emiliania huxleyi in response to environmental changes

Supplement of Simultaneous shifts in elemental stoichiometry and fatty acids of Emiliania huxleyi in response to environmental changes Supplement of Biogeosciences, 15, 1029 1045, 2018 https://doi.org/10.5194/bg-15-1029-2018-supplement Author(s) 2018. This work is distributed under the Creative Commons Attribution 3.0 License. Supplement

More information

Supplementary Figure 1. Observed Aragonite saturation variability and its drivers.

Supplementary Figure 1. Observed Aragonite saturation variability and its drivers. Supplementary Figure 1. Observed Aragonite saturation variability and its drivers. Mean shift in aragonite saturation state from open ocean values, ΔΩ ocean-reef (left), due to freshwater fluxes, ΔΩ fresh

More information

Experimental approaches of carbonate chemistry manipulation. in CO 2 pertubation studies. K. G. Schulz, U. Riebesell

Experimental approaches of carbonate chemistry manipulation. in CO 2 pertubation studies. K. G. Schulz, U. Riebesell Experimental approaches of carbonate chemistry manipulation in CO 2 pertubation studies K. G. Schulz, U. Riebesell Monaco, 06.-09.10.2008 Atmospheric CO 2 variability and marine life increase to about

More information

Carbon Dioxide, Alkalinity and ph

Carbon Dioxide, Alkalinity and ph Carbon Dioxide, Alkalinity and ph OCN 623 Chemical Oceanography 15 March 2018 Reading: Libes, Chapter 15, pp. 383 389 (Remainder of chapter will be used with the classes Global Carbon Dioxide and Biogenic

More information

rotating at 1 rpm encompassing three acidification scenarios and 5 concentrations of the clay

rotating at 1 rpm encompassing three acidification scenarios and 5 concentrations of the clay Respective publication: Passow, Uta, Christina L. De La Rocha, Caitlin Fairfield, Katrin Schmidt submitted to L&O in Dec 2012 : Aggregation as a function of pco 2 and mineral particles Methods Roller tanks

More information

Satellite tools and approaches

Satellite tools and approaches Satellite tools and approaches for OA research William M. Balch Bigelow Laboratory for Ocean Sciences E. Boothbay, ME 04544 With help from: J. Salisbury, D. Vandemark, B. Jönsson, S. Chakraborty,S Lohrenz,

More information

Environmental controls on the physiology of the marine. coccolithophore Emiliania huxleyi strain NIWA 1108

Environmental controls on the physiology of the marine. coccolithophore Emiliania huxleyi strain NIWA 1108 Environmental controls on the physiology of the marine coccolithophore Emiliania huxleyi strain NIWA 1108 by Yuanyuan Feng A thesis submitted in fulfillment of the requirements for the degree of Doctor

More information

INTRODUCTION TO CO2 CHEMISTRY

INTRODUCTION TO CO2 CHEMISTRY INTRODUCTION TO CO2 CHEMISTRY IN SEA WATER Andrew G. Dickson Scripps Institution of Oceanography, UC San Diego Mauna Loa Observatory, Hawaii Monthly Average Carbon Dioxide Concentration Data from Scripps

More information

Table S1. Shimakawa et al.

Table S1. Shimakawa et al. Supplemental Table S1. Effects of ᴅ-glucose on photosynthesis in secondary algae Control 10 min in ᴅ-glucose Control 10 min in ᴅ-glucose E. gracilis O 2 evolution rate / µmol O 2 (mg Chl) 1 h 1 Relative

More information

Individual and population-level responses to ocean acidification

Individual and population-level responses to ocean acidification Individual and population-level responses to ocean acidification Ben P. Harvey, Niall J. McKeown, Samuel P.S. Rastrick, Camilla Bertolini, Andy Foggo, Helen Graham, Jason M. Hall-Spencer, Marco Milazzo,

More information

CLIMATE CHANGE EFFECTS ON SEAGRASSES, MACROALGAE AND THEIR ECOSYSTEMS: ELEVATED DIC, TEMPERATURE, OA AND THEIR INTERACTIONS

CLIMATE CHANGE EFFECTS ON SEAGRASSES, MACROALGAE AND THEIR ECOSYSTEMS: ELEVATED DIC, TEMPERATURE, OA AND THEIR INTERACTIONS CLIMATE CHANGE EFFECTS ON SEAGRASSES, MACROALGAE AND THEIR ECOSYSTEMS: ELEVATED DIC, TEMPERATURE, OA AND THEIR INTERACTIONS Marguerite S. Koch, George E. Bowes, Cliff Ross, XingHai Zhang Josh Filina, Kate

More information

INTRODUCTION TO CO2 CHEMISTRY

INTRODUCTION TO CO2 CHEMISTRY INTRODUCTION TO CO2 CHEMISTRY IN SEA WATER Andrew G. Dickson Scripps Institution of Oceanography, UC San Diego 410 Mauna Loa Observatory, Hawaii Monthly Average Carbon Dioxide Concentration Data from Scripps

More information

Dissolution of olivine (potential, side effects) in simulated CO 2 removal experiments

Dissolution of olivine (potential, side effects) in simulated CO 2 removal experiments Peter Köhler 1 October 2015 Dissolution of olivine (potential, side effects) in simulated CO 2 removal experiments enhanced weathering, ocean alkalinization, ocean fertilization Peter Köhler, Judith Hauck

More information

I. Micro-nutrients in the oceans

I. Micro-nutrients in the oceans Impact of global change on ocean biogeochemical cycles (N, P, C and trace elements) Palma de Mallorca, 17 21 Oct 2011 I. Micro-nutrients in the oceans X. Antón Álvarez Salgado CSIC, Instituto de Investigacións

More information

CO 2 perturbation experiments: similarities and differences between dissolved inorganic carbon and total alkalinity manipulations

CO 2 perturbation experiments: similarities and differences between dissolved inorganic carbon and total alkalinity manipulations Biogeosciences, 6, 2145 215, 29 www.biogeosciences.net/6/2145/29/ Author(s) 29. This work is distributed under the Creative Commons Attribution. License. Biogeosciences CO 2 perturbation experiments: similarities

More information

: 1.9 ppm y -1

: 1.9 ppm y -1 Atmospheric CO 2 Concentration Year 2006 Atmospheric CO 2 concentration: 381 ppm 35% above pre-industrial Atmoapheric [CO2] (ppmv) 4001850 1870 1890 1910 1930 1950 1970 1990 2010 380 360 340 320 300 280

More information

Ocean Acidification: What It Means To Alaska

Ocean Acidification: What It Means To Alaska Ocean Acidification: What It Means To Alaska Ocean Research and Resources Advisory Panel Alaska Sea Life Center July 27 th, 2010 Jeremy T. Mathis Institute of Marine Science School of Fisheries and Ocean

More information

ARTICLE IN PRESS. La Jolla, CA , USA. Received 13 February 2006; received in revised form 15 September 2006; accepted 4 January 2007

ARTICLE IN PRESS. La Jolla, CA , USA. Received 13 February 2006; received in revised form 15 September 2006; accepted 4 January 2007 MARCHE-02440; No of Pages 14 ARTICLE IN PRESS + MODEL Marine Chemistry xx (2007) xxx xxx www.elsevier.com/locate/marchem Total alkalinity: The explicit conservative expression and its application to biogeochemical

More information

Generic analysis of the response of calcifying microalgae to an elevation of pco2 : qualitative vs quantitative analysis

Generic analysis of the response of calcifying microalgae to an elevation of pco2 : qualitative vs quantitative analysis Generic analysis of the response of calcifying microalgae to an elevation of pco2 : qualitative vs quantitative analysis Olivier Bernard, Antoine Sciandre To cite this version: Olivier Bernard, Antoine

More information

Chapter 12: Acids and Bases: Ocean Carbonate System James Murray 4/30/01 Univ. Washington

Chapter 12: Acids and Bases: Ocean Carbonate System James Murray 4/30/01 Univ. Washington Chapter 12: Acids and Bases: Ocean Carbonate System James Murray 4/30/01 Univ. Washington Last lecture was concerned with gas exchange and one example we looked at was the solubility of CO 2. Next we have

More information

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY INFORMATION SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO1635 Extensive dissolution of live pteropods in the Southern Ocean Bednaršek N 1, 2, 3, Tarling GA 1 *, Bakker DCE 2, Fielding S 1, Jones EM 3, Venables HJ 1,

More information

Does the Iron Cycle Regulate Atmospheric CO2?

Does the Iron Cycle Regulate Atmospheric CO2? Does the Iron Cycle Regulate Atmospheric CO2? Mick Follows, Dec 2005 http://ocean.mit.edu/~mick What regulates atmospheric CO2 on glacial-interglacial timescales? Role of ocean biology? Does the iron cycle

More information

Chemical Oceanography Spring 2000 Final Exam (Use the back of the pages if necessary)(more than one answer may be correct.)

Chemical Oceanography Spring 2000 Final Exam (Use the back of the pages if necessary)(more than one answer may be correct.) Ocean 421 Your Name Chemical Oceanography Spring 2000 Final Exam (Use the back of the pages if necessary)(more than one answer may be correct.) 1. Due to the water molecule's (H 2 O) great abundance in

More information

Biogeochemistry of the Earth System QMS Lecture 5 Dr Zanna Chase 16 June 2015

Biogeochemistry of the Earth System QMS Lecture 5 Dr Zanna Chase 16 June 2015 Biogeochemistry of the Earth System QMS512 2015 Lecture 5 Dr Zanna Chase 16 June 2015 Lecture 5: Inorganic carbon chemistry Outline Inorganic carbon speciation in seawater- conceptual overview Inorganic

More information

Part 1: Seawater carbonate chemistry

Part 1: Seawater carbonate chemistry Part 1: Seawater carbonate chemistry 2 Approaches and tools to manipulate the carbonate chemistry Jean-Pierre Gattuso 1,2, Kunshan Gao 3, Kitack Lee 4, Björn Rost 5 and Kai G. Schulz 6 1 Laboratoire d

More information

Significance of HCO 3 alkalinity in calcification and utilization of dissolved inorganic carbon in Chara vulgaris

Significance of HCO 3 alkalinity in calcification and utilization of dissolved inorganic carbon in Chara vulgaris Vol. 26: 169 178, 2017 https://doi.org/10.3354/ab00684 AQUATIC BIOLOGY Aquat Biol Published November 2 OPEN ACCESS Significance of HCO 3 alkalinity in calcification and utilization of dissolved inorganic

More information

Chemical Oceanography 14 March 2012 Points are in parentheses (show all your work) Final Exam

Chemical Oceanography 14 March 2012 Points are in parentheses (show all your work) Final Exam Ocean 400 Name: Chemical Oceanography 14 March 2012 Winter 2012 Points are in parentheses (show all your work) (give as much detail as you can) (use back if necessary) Final Exam 1. Sarmiento and Gruber

More information

Light-dependent carbon isotope fractionation in the coccolithophorid Emiliania huxleyi

Light-dependent carbon isotope fractionation in the coccolithophorid Emiliania huxleyi Limnol. Oceanogr., 47(1), 2002, 120 128 2002, by the American Society of Limnology and Oceanography, Inc. Light-dependent carbon isotope fractionation in the coccolithophorid Emiliania huxleyi Björn Rost,

More information

Mid-Term #1 (125 points total)

Mid-Term #1 (125 points total) Ocean 520 Name: Chemical Oceanography 20 October 2009 Fall 2009 Points are in parentheses (show all your work) (use back if necessary) MidTerm #1 (125 points total) 1. Doney et al (2008) Ocean Acidification

More information

Nutrients; Aerobic Carbon Production and Consumption

Nutrients; Aerobic Carbon Production and Consumption Nutrients; Aerobic Carbon Production and Consumption OCN 623 Chemical Oceanography Reading: Libes, Chapters 8 and 9 Why is organic matter such a good electron donor? Every (other) breath you take is a

More information

Nutrients; Aerobic Carbon Production and Consumption

Nutrients; Aerobic Carbon Production and Consumption Nutrients; Aerobic Carbon Production and Consumption OCN 623 Chemical Oceanography Reading: Libes, Chapters 8 and 9 Formation and respiration of organic matter DINutrients POM Primary Producers Autotrophs

More information

MAR 510 Chemical Oceanography

MAR 510 Chemical Oceanography Carbonate Equilibrium -Key Concepts- Major buffer system influencing ph (master variable) Linked to geological, biological and climatological cycles Complex chemistry involving gaseous, dissolved, and

More information

EBS 566/666 Lecture 8: (i) Energy flow, (ii) food webs

EBS 566/666 Lecture 8: (i) Energy flow, (ii) food webs EBS 566/666 Lecture 8: (i) Energy flow, (ii) food webs Topics Light in the aquatic environment Energy transfer and food webs Algal bloom as seen from space (NASA) Feb 1, 2010 - EBS566/666 1 Requirements

More information

Apical (Boron) Lateral (Boron) Growing edge (SNARF) Seawater ph T

Apical (Boron) Lateral (Boron) Growing edge (SNARF) Seawater ph T Supplemental Materials for: Coral calcifying fluid ph dictates response to ocean acidification Authors: M. Holcomb, A. A. Venn, E. Tambutté, S. Tambutté, D. Allemand, J. Trotter, M. McCulloch 1.4 1.2 1.0

More information

Combined effects of elevated pco 2 and nitrogen limitation on bloom-forming dinoflagellate species

Combined effects of elevated pco 2 and nitrogen limitation on bloom-forming dinoflagellate species Combined effects of elevated pco 2 and nitrogen limitation on bloom-forming dinoflagellate species Produced at the Alfred Wegener Institute for Marine and Polar Research Bremerhaven, Section Marine BioGeoScience

More information

Global-scale variations of the ratios of carbon to phosphorus in exported marine organic matter

Global-scale variations of the ratios of carbon to phosphorus in exported marine organic matter SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO2303 Global-scale variations of the ratios of carbon to phosphorus in exported marine organic matter Yi-Cheng Teng 1, Francois W. Primeau 1, J. Keith Moore 1,

More information

Seagrasses (Zostera marina) and (Zostera japonica) Display a Differential Photosynthetic Response to TCO2: Implications for Acidification Mitigation

Seagrasses (Zostera marina) and (Zostera japonica) Display a Differential Photosynthetic Response to TCO2: Implications for Acidification Mitigation Western Washington University Western CEDAR WWU Masters Thesis Collection WWU Graduate and Undergraduate Scholarship Summer 2016 Seagrasses (Zostera marina) and (Zostera japonica) Display a Differential

More information

Responses of the Emiliania huxleyi Proteome to Ocean Acidification

Responses of the Emiliania huxleyi Proteome to Ocean Acidification Responses of the Emiliania huxleyi Proteome to Ocean Acidification Bethan M. Jones 1 *, M. Debora Iglesias-Rodriguez 1,2,3, Paul J. Skipp 2,4,5, Richard J. Edwards 2,4,5, Mervyn J. Greaves 6, Jeremy R.

More information

CO 2 mediation of adverse effects of seawater acidification in Calcidiscus leptoporus

CO 2 mediation of adverse effects of seawater acidification in Calcidiscus leptoporus Article Volume 12, Number 5 5 May 2011 Q05001, doi:10.1029/2010gc003393 ISSN: 1525 2027 CO 2 mediation of adverse effects of seawater acidification in Calcidiscus leptoporus Gerald Langer ICTA, Autonomous

More information

Ocean acidification in NZ offshore waters

Ocean acidification in NZ offshore waters Ocean acidification in NZ offshore waters Cliff Law NIWA Review susceptible groups in NZ offshore waters Examples from international research of responses Identify potential impacts in the NZ EEZ Plankton

More information

Liverpool NEMO Shelf Arctic Ocean modelling

Liverpool NEMO Shelf Arctic Ocean modelling St. Andrews 22 July 2013 ROAM @ Liverpool NEMO Shelf Arctic Ocean modelling Maria Luneva, Jason Holt, Sarah Wakelin NEMO shelf Arctic Ocean model About 50% of the Arctic is shelf sea (

More information

Nutrients; Aerobic Carbon Production and Consumption

Nutrients; Aerobic Carbon Production and Consumption Nutrients; Aerobic Carbon Production and Consumption OCN 623 Chemical Oceanography Reading: Libes, Chapters 8 and 9 Formation and respiration of organic matter DINutrients POM Primary Producers Autotrophs

More information

Combined Effects of Ocean Acidification and Light or Nitrogen Availabilities on 13 C Fractionation in Marine Dinoflagellates

Combined Effects of Ocean Acidification and Light or Nitrogen Availabilities on 13 C Fractionation in Marine Dinoflagellates RESEARCH ARTICLE Combined Effects of Ocean Acidification and Light or Nitrogen Availabilities on 13 C Fractionation in Marine Dinoflagellates Mirja Hoins 1,2 *, Tim Eberlein 2, Christian H. Groβmann 2,

More information

Environmental Plant Physiology Photosynthesis - Aging. Department of Plant and Soil Sciences

Environmental Plant Physiology Photosynthesis - Aging. Department of Plant and Soil Sciences Environmental Plant Physiology Photosynthesis - Aging krreddy@ra.msstate.edu Department of Plant and Soil Sciences Photosynthesis and Environment Leaf and Canopy Aging Goals and Learning Objectives: To

More information

1 Carbon - Motivation

1 Carbon - Motivation 1 Carbon - Motivation Figure 1: Atmospheric pco 2 over the past 400 thousand years as recorded in the ice core from Vostok, Antarctica (Petit et al., 1999). Figure 2: Air-sea flux of CO 2 (mol m 2 yr 1

More information

Photosynthesis - Aging Leaf Level. Environmental Plant Physiology Photosynthesis - Aging. Department of Plant and Soil Sciences

Photosynthesis - Aging Leaf Level. Environmental Plant Physiology Photosynthesis - Aging. Department of Plant and Soil Sciences Environmental Plant Physiology Photosynthesis and Environment Leaf and Canopy Aging krreddy@ra.msstate.edu Department of Plant and Soil Sciences Goals and Learning Objectives: To understand the effects

More information

University of Southampton Research Repository eprints Soton

University of Southampton Research Repository eprints Soton University of Southampton Research Repository eprints Soton Copyright and Moral Rights for this thesis are retained by the author and/or other copyright owners. A copy can be downloaded for personal non-commercial

More information

Permeable coral reef sediment dissolution driven by elevated pco 2 and pore water advection

Permeable coral reef sediment dissolution driven by elevated pco 2 and pore water advection GEOPHYSICAL RESEARCH LETTERS, VOL. 40, 4876 4881, doi:10.1002/grl.50948, 2013 Permeable coral reef sediment dissolution driven by elevated pco 2 and pore water advection T. Cyronak, 1 I. R. Santos, 1 and

More information

Major Nutrients Trends and some Statistics

Major Nutrients Trends and some Statistics Environmental Factors Nutrients K. Raja Reddy Krreddy@pss.msstate.edu Environmental and Cultural Factors Limiting Potential Yields Atmospheric Carbon Dioxide Temperature (Extremes) Solar Radiation Water

More information

CO 2 and the carbonate system. 1/45

CO 2 and the carbonate system.  1/45 CO 2 and the carbonate system http://eps.mcgill.ca/~courses/c542/ 1/45 The Atmospheric CO 2 -Climate Connection From: http://www.google.ca/imgres?imgurl=http:/ /www.tallbergfoundation.org/ From: Ruddiman,

More information

Term paper topics, due February 8

Term paper topics, due February 8 Term paper topics, due February 8 ODV mini-projects, due March 13 (10% final grade) Individuals or teams of two Using any available datasets, put together a ~7-10 minute talk to present in class on March

More information

Responses to future climate change: biogeochemistry

Responses to future climate change: biogeochemistry Responses to future climate change: biogeochemistry Jean-Pierre Gattuso Laboratoire d Océanographie de Villefranche (LOV) CNRS - Université Pierre et Marie Curie - Paris 6 Villefranche-sur-mer, France

More information

University of Cape Town

University of Cape Town The copyright of this thesis vests in the author. No quotation from it or information derived from it is to be published without full acknowledgement of the source. The thesis is to be used for private

More information

Term paper topics, due February 9

Term paper topics, due February 9 Term paper topics, due February 9 ODV mini-projects, due March 14 (10% final grade) Individuals or teams of two Using any available datasets, put together a ~7-10 minute talk to present in class on March

More information

Estimates of Rates of Biological Productivity at BATS: Is there convergence?

Estimates of Rates of Biological Productivity at BATS: Is there convergence? Estimates of Rates of Biological Productivity at BATS: Is there convergence? Rachel H. R. Stanley Woods Hole Oceanographic Institution Outline 1) Introduction to Bermuda Atlantic Time-series Site (BATS)

More information

Department of Chemistry, School of Science and Engineering, Kinki University Kowakae, Higashiosaka, Osaka , Japan

Department of Chemistry, School of Science and Engineering, Kinki University Kowakae, Higashiosaka, Osaka , Japan Chikyukagaku Geochemistry Behavior and seasonal variation of eutrophication substances in the Yodo River system Yuzuru NAKAGUCHI,YoshitakaYAMAGUCHI,TakashiNISHIMURA, Yoshiyuki HATANO,Masayo IMANAKA and

More information

(Received 26 July 2001; in revised form 29 November 2001; accepted 29 November 2001)

(Received 26 July 2001; in revised form 29 November 2001; accepted 29 November 2001) Journal of Oceanography, Vol. 58, pp. 227 to 243, 2002 Review Seasonal and Interannual Variability in the Distribution of Surface Nutrients and Dissolved Inorganic Carbon in the Northern North Pacific:

More information

Phytoplankton iron limitation in the Humboldt Current and Peru Upwelling

Phytoplankton iron limitation in the Humboldt Current and Peru Upwelling Limnol. Oceanogr., 47(4),, 997 111, by the American Society of Limnology and Oceanography, Inc. Phytoplankton iron limitation in the Humboldt Current and Peru Upwelling D. A. Hutchins, 1 C. E. Hare, R.

More information

Overview of CO 2 -induced Changes in Seawater Chemistry

Overview of CO 2 -induced Changes in Seawater Chemistry Overview of CO 2 -induced Changes in Seawater Chemistry Joan Kleypas & Chris Langdon I. Background II. Facts vs Hypotheses III. Future directions 10-Oct-00 9th Int Coral Reef Symp. 1 Effects of CO 2 on

More information

INTRODUCTION TO CO2 MEASUREMENTS IN SEA WATER

INTRODUCTION TO CO2 MEASUREMENTS IN SEA WATER INTRODUCTION TO CO2 MEASUREMENTS IN SEA WATER Andrew G. Dickson Scripps Institution of Oceanography, UC San Diego METHODS FOR MEASURING THE CO 2 PARAMETERS IN SEA WATER USUAL PARAMETERS MEASURED Total

More information

PHOTOACCLIMATION OF PHOTOSYNTHESIS IRRADIANCE RESPONSE CURVES AND PHOTOSYNTHETIC PIGMENTS IN MICROALGAE AND CYANOBACTERIA 1

PHOTOACCLIMATION OF PHOTOSYNTHESIS IRRADIANCE RESPONSE CURVES AND PHOTOSYNTHETIC PIGMENTS IN MICROALGAE AND CYANOBACTERIA 1 J. Phycol. 38, 17 38 (2002) REVIEW PHOTOALIMATION OF PHOTOSYNTHESIS IRRADIANE RESPONSE URVES AND PHOTOSYNTHETI PIGMENTS IN MIROALGAE AND YANOBATERIA 1 Hugh L. MacIntyre, 2 Todd M. Kana University of Maryland

More information

Time-series observations in the Northern Indian Ocean V.V.S.S. Sarma National Institute of Oceanography Visakhapatnam, India

Time-series observations in the Northern Indian Ocean V.V.S.S. Sarma National Institute of Oceanography Visakhapatnam, India The Second GEOSS Asia-Pacific Symposium, Tokyo, 14-16 th April 28 Time-series observations in the Northern Indian Ocean V.V.S.S. Sarma National Institute of Oceanography Visakhapatnam, India Seasonal variations

More information

Distributions of dissolved inorganic carbon and total alkalinity in the Western Arctic Ocean

Distributions of dissolved inorganic carbon and total alkalinity in the Western Arctic Ocean Article Advances in Polar Science doi:10.3724/sp.j.1085.2011.00246 December 2011 Vol.22 No.4 246 252 Distributions of dissolved inorganic carbon and total alkalinity in the Western Arctic Ocean SUN Heng

More information

Marine geochemical data assimilation in an efficient Earth System Model of global biogeochemical cycling

Marine geochemical data assimilation in an efficient Earth System Model of global biogeochemical cycling Biogeosciences, 4, 87 14, 27 www.biogeosciences.net/4/87/27/ Author(s) 27. This work is licensed under a Creative Commons License. Biogeosciences Marine geochemical data assimilation in an efficient Earth

More information

OCB Summer Workshop WHOI, July 16-19,

OCB Summer Workshop WHOI, July 16-19, Transformation and fluxes of carbon in a changing Arctic Ocean and it s impact on ocean acidification, the Atlantic view Leif G. Anderson Department t of Chemistry and Molecular l Biology University of

More information

Effect of CO 2 concentration on C :N:P ratio in marine phytoplankton: A species comparison

Effect of CO 2 concentration on C :N:P ratio in marine phytoplankton: A species comparison Limnol. Oceanogr., 44(3), 1999, 683 690 1999, by the American Society of Limnology and Oceanography, Inc. Effect of CO 2 concentration on C :N:P ratio in marine phytoplankton: A species comparison Steffen

More information

VOCABULARY COMPTETENCIES. Students, after mastering the materials of Plant Physiology course, should be able to:

VOCABULARY COMPTETENCIES. Students, after mastering the materials of Plant Physiology course, should be able to: 1 VOCABULARY Forget not, exam includes ENGLISH WORDS 1. Involve 2. Bundle 3. Sheath 4. Subsequent 5. Ambient 6. Stick together 7. Determine 8. Evolution 9. Thrive 10. Allow COMPTETENCIES Students, after

More information

Section A. Homi Bhabha Centre for Science Education Tata Institute of Fundamental Research, Mumbai 1

Section A. Homi Bhabha Centre for Science Education Tata Institute of Fundamental Research, Mumbai 1 Section A Q.No. (a) (b) (c) (d) Q.No. (a) (b) (c) (d) 1 16 2 17 3 18 4 19 5 20 6 21 7 22 8 23 9 24 10 25 11 26 12 27 13 28 14 29 15 30 1 Ans 31. SECTION B (Long questions) The question is based on a Scientific

More information

Ocean Acidifica+on: past analogies, present concerns, future predic+ons. Sco8 Wieman

Ocean Acidifica+on: past analogies, present concerns, future predic+ons. Sco8 Wieman Ocean Acidifica+on: past analogies, present concerns, future predic+ons Sco8 Wieman Effects Planktonic calcifica+on Carbon and nutrient assimila+on Primary produc+on Acid-base balance Larval stages of

More information

Temporal decoupling of carbon and nitrogen dynamics in a mesocosm diatom bloom

Temporal decoupling of carbon and nitrogen dynamics in a mesocosm diatom bloom Limnol. Oceanogr., 47(3), 2002, 753 761 2002, by the American Society of Limnology and Oceanography, Inc. Temporal decoupling of carbon and nitrogen dynamics in a mesocosm diatom bloom Anja Engel, 1 Sarah

More information

Testing the direct effect of C 02 concentration on a bloom of the coccolithophorid Emiliania huxleyi in mesocosm experiments

Testing the direct effect of C 02 concentration on a bloom of the coccolithophorid Emiliania huxleyi in mesocosm experiments Limnol. Oceanogr., 50(2), 2005, 493-507 2005, by the American Society of Limnology and Oceanography, Inc. Testing the direct effect of C 02 concentration on a bloom of the coccolithophorid Emiliania huxleyi

More information

Algal Physiology. I. Photosynthesis in algae II. Characteristics to distinguish algal divisions. I. Photosynthesis

Algal Physiology. I. Photosynthesis in algae II. Characteristics to distinguish algal divisions. I. Photosynthesis Algal Physiology I. Photosynthesis in algae II. Characteristics to distinguish algal divisions 1 I. Photosynthesis 2 1 PSU : Photosynthetic Unit = Antennae + rxn center Light reactions: solar energy is

More information

GCE A level 1324/01 PHYSICS PH4 Oscillations and Fields

GCE A level 1324/01 PHYSICS PH4 Oscillations and Fields Surname Centre Number Candidate Number Other Names 2 GCE A level 1324/01 PHYSICS PH4 Oscillations and Fields P.M. WEDNESDAY, 11 June 2014 1 hour 30 minutes For s use Question Maximum Mark Mark Awarded

More information

Life Sciences For NET & SLET Exams Of UGC-CSIR. Section B and C. Volume-10. Contents A. PHOTOSYNTHESIS 1 B. RESPIRATION AND PHOTORESPIRATION 33

Life Sciences For NET & SLET Exams Of UGC-CSIR. Section B and C. Volume-10. Contents A. PHOTOSYNTHESIS 1 B. RESPIRATION AND PHOTORESPIRATION 33 Section B and C Volume-10 Contents 6. SYSTEM PHYSIOLOGY-PLANTS A. PHOTOSYNTHESIS 1 B. RESPIRATION AND PHOTORESPIRATION 33 C. NITROGEN METABOLISM 51 D. PLANT HORMONES 73 0 6. SYSTEM PHYSIOLOGY-PLANTS A.

More information

I. Photosynthesis. Algal Physiology. I. Photosynthesis in algae II. Characteristics to distinguish algal divisions

I. Photosynthesis. Algal Physiology. I. Photosynthesis in algae II. Characteristics to distinguish algal divisions Algal Physiology I. Photosynthesis I. Photosynthesis in algae II. Characteristics to distinguish algal divisions 1 2 PSU : Photosynthetic Unit = Antennae + rxn center Light reactions: solar energy is harvested

More information

CHEMISTRY OF ENVIRONMENTAL SCIENCE

CHEMISTRY OF ENVIRONMENTAL SCIENCE CHEMISTRY OF ENVIRONMENTAL SCIENCE WUCT 208 This is the Environmental Science Topic Exam. A group of two students will work together on this exam. A copy of the test will be provided to each student, but

More information

EFFECT OF OCEAN ACIDIFICATION ON MARINE PHYTOPLANKTON Debora Iglesias-Rodriguez

EFFECT OF OCEAN ACIDIFICATION ON MARINE PHYTOPLANKTON Debora Iglesias-Rodriguez EFFECT OF OCEAN ACIDIFICATION ON MARINE PHYTOPLANKTON Debora Iglesias-Rodriguez Changes in physiology biogeochemistry O 2 photosynthesis CO 2 OCEAN ACIDIFICATION Time series of atmospheric CO 2 Mauna Loa

More information

Simulation of export production and biological pump structure in the South China Sea

Simulation of export production and biological pump structure in the South China Sea Appendix Electronic Supplementary Material Geo-Marine Letters volume issue 6 December 0 Simulation of export production and biological pump structure in the South hina Sea Wentao Ma Fei hai Peng Xiu Huijie

More information

CHEMISTRY 102 A/E Fall 2008 HOUR EXAM I NAME Dr. Christine Yerkes. A. DO NOT open the exam until you are instructed to do so.

CHEMISTRY 102 A/E Fall 2008 HOUR EXAM I NAME Dr. Christine Yerkes. A. DO NOT open the exam until you are instructed to do so. CHEMISTRY 102 A/E Fall 2008 HOUR EXAM I NAME Dr. Christine Yerkes October 1, 2008 SIGNATURE Test Form A QUIZ TA A. DO NOT open the exam until you are instructed to do so. B. The exam has 6 pages. After

More information

Continent-Ocean Interaction: Role of Weathering

Continent-Ocean Interaction: Role of Weathering Institute of Astrophysics and Geophysics (Build. B5c) Room 0/13 email: Guy.Munhoven@ulg.ac.be Phone: 04-3669771 28th February 2018 Organisation of the Lecture 1 Carbon cycle processes time scales modelling:

More information

[2] State in what form the energy is released in such a reaction.... [1]

[2] State in what form the energy is released in such a reaction.... [1] (a) The following nuclear reaction occurs when a slow-moving neutron is absorbed by an isotope of uranium-35. 0n + 35 9 U 4 56 Ba + 9 36Kr + 3 0 n Explain how this reaction is able to produce energy....

More information

Pigment packaging effects in Thalassiosira pseudonana under light regulated steady-state growth

Pigment packaging effects in Thalassiosira pseudonana under light regulated steady-state growth Pigment packaging effects in Thalassiosira pseudonana under light regulated steady-state growth B. Greg Mitchell, Niu Du, Elliot Weiss and Maria Vernet Scripps Institution of Oceanography, UCSD Acknowledgements:

More information

Biogeochemical modelling and data assimilation: status in Australia

Biogeochemical modelling and data assimilation: status in Australia Biogeochemical modelling and data assimilation: status in Australia Richard Matear, Andrew Lenton, Matt Chamberlain, Mathieu Mongin, Emlyn Jones, Mark Baird www.cmar.csiro.au/staff/oke/ Biogeochemical

More information

1/24/2011. Why do we care about biomass? Direct aggregation and pulsed export is also important

1/24/2011. Why do we care about biomass? Direct aggregation and pulsed export is also important Food web structure is a key determinant on carbon fluxes: 1) Cell size and geometry influence sinking rate 2) Zooplankton repackage material and vertically migrate 3) Small cells support longer food webs

More information

Calcification in the planktonic foraminifera Globigerina bulloides linked to phosphate concentrations in surface waters of the North Atlantic Ocean

Calcification in the planktonic foraminifera Globigerina bulloides linked to phosphate concentrations in surface waters of the North Atlantic Ocean Biogeosciences, 9, 1725 179, 2012 doi:10.519/bg-9-1725-2012 Author(s) 2012. CC Attribution.0 License. Biogeosciences Calcification in the planktonic foraminifera Globigerina bulloides linked to phosphate

More information

Problem Set #4 ANSWER KEY Fall 2009 Due: 9:30, Monday, Nov 30

Problem Set #4 ANSWER KEY Fall 2009 Due: 9:30, Monday, Nov 30 OCN 520 Problem Set #4 ANSWER KEY Fall 2009 Due: 9:30, Monday, Nov 30 1. Two-Box Ocean Model The B Flux Using a 2 box model like the one you have worked on in problem set #4 (question 1) assume the following

More information

Chemistry 142 (Practice) MIDTERM EXAM II November. Fill in your name, section, and student number on Side 1 of the Answer Sheet.

Chemistry 142 (Practice) MIDTERM EXAM II November. Fill in your name, section, and student number on Side 1 of the Answer Sheet. Chemistry 4 (Practice) MIDTERM EXAM II 009 November (a) Before starting, please check to see that your exam has 5 pages, which includes the periodic table. (b) (c) Fill in your name, section, and student

More information

2006 AGU Ocean Science Meeting in Hawaii

2006 AGU Ocean Science Meeting in Hawaii 26 AGU Ocean Science Meeting in Hawaii Session: Sinking Particle in the Twilight Zone OS23H- Mutsu Institute for Oceanography Linkage between seasonal variability of nutrients in the epipelagic layer and

More information

Tracking El Niño using optical indices of phytoplankton dynamics in the equatorial Pacific

Tracking El Niño using optical indices of phytoplankton dynamics in the equatorial Pacific Abstract Tracking El Niño using optical indices of phytoplankton dynamics in the equatorial Pacific Joel Craig 1, Pete Strutton 2, Wiley Evans 2 1. College of Earth and Atmospheric Science, Georgia Institute

More information

Gas exchange of CO 2 and O 2 in partially ice-covered regions of the Arctic Ocean investigated using in situ sensors

Gas exchange of CO 2 and O 2 in partially ice-covered regions of the Arctic Ocean investigated using in situ sensors Gas exchange of CO 2 and O 2 in partially ice-covered regions of the Arctic Ocean investigated using in situ sensors F Islam 1, M DeGrandpre 1, C Beatty 1, R Krishfield 2 and J Toole 2 1 Department of

More information

Impact of Environmental and Stress Factors on the Photosynthetic Capabilities of Plants

Impact of Environmental and Stress Factors on the Photosynthetic Capabilities of Plants Universal Journal of Agricultural Research 5(2): 113-118, 2017 DOI: 10.13189/ujar.2017.050205 http://www.hrpub.org Impact of Environmental and Stress Factors on the Photosynthetic Capabilities of Plants

More information

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY INFORMATION SUPPLEMENTARY INFORMATION Site Information: Table S1: Sites Modern Location Modern SST ( C) PO4(µM)-0m PO4(µM)-75m 130-806 0.5N, 159.5E 29.2 0.24 0.34 *(6) 154-925 4.5N, 43.5W 27.4 0.24 0.35 *(S35) 198-1208

More information

Equation for Global Warming

Equation for Global Warming Equation for Global Warming Derivation and Application Contents 1. Amazing carbon dioxide How can a small change in carbon dioxide (CO 2 ) content make a critical difference to the actual global surface

More information

Coastal ocean CO 2 carbonic acid carbonate sediment system of the Anthropocene

Coastal ocean CO 2 carbonic acid carbonate sediment system of the Anthropocene GLOBAL BIOGEOCHEMICAL CYCLES, VOL. 20,, doi:10.1029/2005gb002506, 2006 Coastal ocean CO 2 carbonic acid carbonate sediment system of the Anthropocene Andreas J. Andersson, 1 Fred T. Mackenzie, 1 and Abraham

More information

1. Forming a Precipitate 2. Solubility Product Constant (One Source of Ions)

1. Forming a Precipitate 2. Solubility Product Constant (One Source of Ions) Chemistry 12 Solubility Equilibrium II Name: Date: Block: 1. Forming a Precipitate 2. Solubility Product Constant (One Source of Ions) Forming a Precipitate Example: A solution may contain the ions Ca

More information

The Cherenkov effect

The Cherenkov effect The Cherenkov effect A charged particle traveling in a dielectric medium with n>1 radiates Cherenkov radiation if its velocity is larger than the phase velocity of light v>c/n or β > 1/n (threshold) A

More information

Quality assurance of analytical measurements of CO2 parameters. Andrew G. Dickson

Quality assurance of analytical measurements of CO2 parameters. Andrew G. Dickson Quality assurance of analytical measurements of CO2 parameters Andrew G. Dickson 1 Quality assurance constitutes the system by which an analytical laboratory can assure outside users that the analytical

More information

Ocean carbon cycle feedbacks in the tropics from CMIP5 models

Ocean carbon cycle feedbacks in the tropics from CMIP5 models WWW.BJERKNES.UIB.NO Ocean carbon cycle feedbacks in the tropics from CMIP5 models Jerry Tjiputra 1, K. Lindsay 2, J. Orr 3, J. Segschneider 4, I. Totterdell 5, and C. Heinze 1 1 Bjerknes Centre for Climate

More information

Chemistry 2000 Lecture 11: Chemical equilibrium

Chemistry 2000 Lecture 11: Chemical equilibrium Chemistry 2000 Lecture 11: Chemical equilibrium Marc R. Roussel February 4, 2019 Marc R. Roussel Chemical equilibrium February 4, 2019 1 / 27 Equilibrium and free energy Thermodynamic criterion for equilibrium

More information