Competition-induced starvation drives large-scale population cycles in Antarctic krill

Similar documents
SUPPLEMENTARY INFORMATION

2001 State of the Ocean: Chemical and Biological Oceanographic Conditions in the Newfoundland Region

Summary. A Bird s- Eye View of Community and Population Effects of Ontogenetic Development

Temperature. (1) directly controls metabolic rates of ectotherms (invertebrates, fish) Individual species

Name Student ID. Good luck and impress us with your toolkit of ecological knowledge and concepts!

Biogeochemical modelling and data assimilation: status in Australia

Tasmanian Institute of Agriculture, University of Tasmania;

Ecology 302: Lecture VI. Evolution of Life Histories

Understanding the role of the YS Bottom Cold Water ( 10 C) on the survival strategy of Euphausia pacifica throughout the hot summer

Marine Resources Development Foundation/MarineLab Grades: 9, 10, 11, 12 States: AP Biology Course Description Subjects: Science

Chapter 6 Lecture. Life History Strategies. Spring 2013

Citation for published version (APA): Hin, V. (2017). Ontogenesis: Eco-evolutionary perspective on life history complexity.

Chapter 8. Biogeographic Processes. Upon completion of this chapter the student will be able to:

SECTION 7: STEADY-STATE ERROR. ESE 499 Feedback Control Systems

Arctic Ocean Biology. from the surface to the deep sea

2 One-dimensional models in discrete time

Aggregations on larger scales. Metapopulation. Definition: A group of interconnected subpopulations Sources and Sinks

History and meaning of the word Ecology A. Definition 1. Oikos, ology - the study of the house - the place we live

PULSE-SEASONAL HARVESTING VIA NONLINEAR DELAY DIFFERENTIAL EQUATIONS AND APPLICATIONS IN FISHERY MANAGEMENT. Lev V. Idels

Supplementary Figure 1 Surface distribution and concentration of the dinoflagellate N. scintillans

Plant responses to climate change in the Negev

Turbulence and the Spring Phytoplankton Bloom

Revisiting the biodiversity ecosystem multifunctionality relationship

Palmer LTER: Seasonal process sea-ice cruise, June- July 1999 (NBP99-06)

LESSON THREE Time, Temperature, Chlorophyll a Does sea surface temperature affect chlorophyll a concentrations?

Curriculum Map. Biology, Quarter 1 Big Ideas: From Molecules to Organisms: Structures and Processes (BIO1.LS1)

Lecture 2: Individual-based Modelling

Project. Aim: How does energy flow in Arctic and Antarctic ecosystems? Explore. The four food webs are:

Radiative Effects of Contrails and Contrail Cirrus

Water Balance in the Murray-Darling Basin and the recent drought as modelled with WRF

Copepod community growth rates in relation to body size, temperature, and food availability in the East China Sea: A test of Metabolic Theory

Biology Unit Overview and Pacing Guide

Current controversies in Marine Ecology with an emphasis on Coral reef systems

CSC 578 Neural Networks and Deep Learning

Lecture 20/Lab 21: Systems of Nonlinear ODEs

The functional biology of krill (Thysanoessa raschii)

Environmental forcing on forage fish and apex predators in the California Current: Results from a fully coupled ecosystem model

Correlations to Next Generation Science Standards. Life Sciences Disciplinary Core Ideas. LS-1 From Molecules to Organisms: Structures and Processes

Lecture 3. STAT161/261 Introduction to Pattern Recognition and Machine Learning Spring 2018 Prof. Allie Fletcher

NATS 104 LIFE ON EARTH SPRING, 2002 SECOND 100-pt EXAM.

Phytoplankton. Zooplankton. Nutrients

Individual-Based modeling of Copepods MAR524 Unit 11

Name Date Class. As you read Chapter 12, which begins on page 278 of your textbook, answer the following questions.

UPPLEMENT A COMPARISON OF THE EARLY TWENTY-FIRST CENTURY DROUGHT IN THE UNITED STATES TO THE 1930S AND 1950S DROUGHT EPISODES

Oct.23,2014. PICES2014,Yeosu

Coevolution of competitors

Supplementary Material for: Scientific Uncertainty and Climate Change: Part I. Uncertainty and Unabated Emissions

Chapter 6 Reading Questions

Current controversies in Marine Ecology with an emphasis on Coral reef systems. Niche Diversification Hypothesis Assumptions:

Spatio-temporal dynamics of Marbled Murrelet hotspots during nesting in nearshore waters along the Washington to California coast

Deep-ocean observatories, biogeochemical & biophysical time-series data: NZ-Australia & international linkages

Ice matters. Arctic and Antarctic under-ice communities linking sea ice with the pelagic food web

VI) Population and Community Stability. VI) Population and Community Stability. I. Background / questions - refer back to succession

VI) Population and Community Stability. VI) Population and Community Stability

Ecology of krill in Icelandic waters. Teresa Silva

SUPPLEMENTARY INFORMATION. Antarctic-wide array of high-resolution ice core records reveals pervasive lead pollution began in 1889 and persists today

Exxon Valdez Oil Spill Restoration Project Annual Report

Oikos. Appendix A1. o20830

Maintenance of species diversity

James Thorson, Steve Munch, Jason Cope, Jin Gao

A Posteriori Error Estimates For Discontinuous Galerkin Methods Using Non-polynomial Basis Functions

Age (x) nx lx. Population dynamics Population size through time should be predictable N t+1 = N t + B + I - D - E

VEGETATION PROCESSES IN THE PELAGIC: A MODEL FOR ECOSYSTEM THEORY

Variability and trend of the heat balance in the southeast Indian Ocean

Oklahoma Academic Standards for Biology I

Investigating the active flux of carbon in the Southern Ocean: the contribution of a prominent euphausiid

Population Dynamics of Gulf Blue Crabs. Caz Taylor & Erin Grey Department of Ecology & Evolutionary Biology Tulane University

Impacts of Changes in Extreme Weather and Climate on Wild Plants and Animals. Camille Parmesan Integrative Biology University of Texas at Austin

Future of Kuroshio/Oyashio ecosystems: an outcome of the CFAME Task Team and WG20

Life history evolution

Antarctic sea-ice expansion between 2000 and 2014 driven by tropical Pacific decadal climate variability

Sediment impacts on coral communities: gametogenesis, spawning, recruitment and early post-recruitment survival Dr Luke Smith

Extinction and the Allee Effect in an Age Structured Population Model

Current and future climate of the Cook Islands. Pacific-Australia Climate Change Science and Adaptation Planning Program

peak half-hourly Tasmania

Climate change, ocean acidification and individual-based models: Why the little things matter

Chapter 6 Vocabulary. Environment Population Community Ecosystem Abiotic Factor Biotic Factor Biome

Species specific geographical distribution patterns in a warm Barents Sea: haddock vs. cod

Investigating the contribution of allochthonous subsidies to kelp forests in central California

Optimal control of single species biological population

SARSIM Model Output for the Distribution of Sardine in Canadian, US and Mexican Waters. Richard Parrish October 13, 2015

Students will observe how population size can vary from generation to generation in response to changing environmental conditions.

Evolution 1 Star. 6. The different tools used during the beaks of finches lab represented. A. feeding adaptations in finches

Coupling OSMOSE and ROMS NPZD models: towards end to end modelling of the Benguela upwelling ecosystem

Populations in lakes. Limnology Lecture 9

Population Ecology and the Distribution of Organisms. Essential Knowledge Objectives 2.D.1 (a-c), 4.A.5 (c), 4.A.6 (e)

Ice Station POLarstern (ISPOL 1)

Lecture 3. Linear Regression

PICES W3 [D-504], Sep 22, 2017, 11:40-12:05

Name ECOLOGY TEST #1 Fall, 2014

REVISION: POPULATION ECOLOGY 18 SEPTEMBER 2013

Ocean acidification in NZ offshore waters

Individual-Based modeling of Copepods

4º ESO BIOLOGY & GEOLOGY SUMMER REINFORCEMENT: CONTENTS & ACTIVITIES

A Synthesis of Results from the Norwegian ESSAS (N-ESSAS) Project

Stockton Unified School District Instructional Guide for BIOLOGY NGSS Pilot for both 4X4 and Traditional. 1st Quarter

Student Name: Teacher: Date: District: London City. Assessment: 07 Science Science Test 4. Description: Life Science Final 1.

The role of sea-ice in extended range prediction of atmosphere and ocean

Biology 11 Unit 1: Fundamentals. Lesson 1: Ecology

Case Study: Australia. LI: To understand urbanisation issues and management strategies in Australia

Transcription:

In the format provided by the authors and unedited. SUPPLEMENTARY INFORMATION VOLUME: 1 ARTICLE NUMBER: 0177 Competition-induced starvation drives large-scale population cycles in Antarctic krill Alexey B. Ryabov 1 *, André M. de Roos 2, Bettina Meyer 1, 3, 4, So Kawaguchi 5, 6 and Bernd Blasius 1, 4 Affiliations: 1 Institute for Chemistry and Biology of the Marine Environment, University of Oldenburg, Oldenburg, Germany 2 Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, The Netherlands 3 Alfred Wegener Institute for Polar and Marine Research, Scientific Division Polar Biological Oceanography, Bremerhaven, Germany 4 Helmholtz Institute for Functional Marine Biodiversity at the University of Oldenburg, Germany, www.hifmb.de 5 Australian Antarctic Division, Kingston, Tasmania, Australia 6 Antarctic Climate and Ecosystems Cooperative Research Centre, Hobart, Australia. *Correspondence to: alexey.ryabov@uni-oldenburg.de. Content: Supplementary Figures 1 to 12 Supplementary Tables 1 to 5 NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 1

cc(tt, aa, ww) (PP, ww) Supplementary Figure 1. The ontogenetic modeling of krill population dynamics and the interactions between krill cohorts and the environment. a, Krill cohorts (orange bars) increase their weight and move from left to right along the weight axis. The dotted orange line shows the krill weight distribution cc(tt, aa, ww). b, The interaction between krill cohorts and the environment. The traditional concept suggests that fluctuations in krill abundance follow the changes in food level caused by periodical environmental changes (black arrow). Our study complements this approach and shows that the feedback of krill biomass on the food level (highlighted by black dashed outlines) plays a crucial role in the appearance of krill population cycles. NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 2

Supplementary Figure 2. Krill reproductive capacity. a, Temporal changes in the biomass of females with red thelycum (i.e., in reproductive cycle, grey dashed line) compared to total krill biomass (red). Total biomass of females in reproductive cycles depends on krill abundance, length distribution and available food. The maxima of reproductive female biomass do not coincide with the maxima in total biomass as the reproductive female biomass is large when an abundant strong krill cohort reaches larger sizes and when summer conditions are favorable for reproduction. b, The abundance of juveniles decreases with the biomass of female in reproductive cycle in the preceding year. The inset shows a box plot of the same data divided into two groups (Small, Large) with the female biomass either smaller or larger than 1.5 mg DW/m 3 (insignificant, pp = 0.3). NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 3

Supplementary Figure 3. Robustness of the krill cycles to different grazing modes. Simulated population cycles when phytoplankton is consumed by all cohorts (left), only by larvae (adults and juveniles are still limited by the same phytoplankton, middle), or only by adults and juveniles (larvae are limited by the same phytoplankton, right). The figures show oscillations in the length distribution in color coding (top) and abundances (black lines) and biomass (red lines) (bottom). NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 4

Supplementary Figure 4. Sensitivity of the krill cycle to inter-annual environmental variability. Environmental disturbances are simulated as random inter-annual changes in phytoplankton carrying capacity KK PPh in a gradient from unperturbed to strongly perturbed (three upper rows) and assuming that phytoplankton carrying capacity, KK PPh, is driven by Southern Annular Oscillations index 9, namely, KK PPh = KK PPh,0 exp( 0.3 SAM) (bottom). (Left panel) Time course of simulated phytoplankton carrying capacity (black dashed line), phytoplankton concentration (green) and total krill abundance (red line). (Middle panel) Relation between summer phytoplankton concentration and krill abundance in the following year (green dots) and linear regression (black line). (Right panel) Relation between krill biomass and juvenile abundance in the following year (green dots, compare to Fig. 1h). The insets show a box plot of the same data divided into two groups (Small, Large) with the total krill biomass either smaller or larger than 20 mg DW/m 3. See Methods (Environmental interannual disturbances) for model parameters. NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 5

Supplementary Figure 5. The modeled dynamics of phytoplankton, krill biomass and different krill stages. a, The annual maxima of phytoplankton concentrations (green line) correlate with the annual minima of total biomass (adults + juveniles) and vice versa. b, Embryo abundances approximately follow the pattern for total krill biomass, because reproduction is not food limited. c, The maximal abundance of larvae is proportional to the number of embryos with a 30 days delay. However, the number of larvae can subsequently drop abruptly if autumn phytoplankton concentration is extremely low. The model predicts no positive relationship between the abundance of larvae at the end of summer and the abundance of juveniles at the beginning of the next summer. If autumn phytoplankton concentration is small even a big cohort of larvae does not result in substantial recruitment, and if the autumn conditions are good, a relatively small cohort of larvae can result in a strong cohort of juveniles, which become dominating adults in the following year (d) and increases total krill abundance (e). The black, and green, arrows connect the different stages of a weak cohort which becomes extinct, and of a strong cohort, respectively NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 6

Supplementary Figure 6. The effect of krill loss rates on population dynamics. The bifurcation diagram shows the effect of krill mortality on the summer maxima of the total abundance of adult and juvenile krill (grey dots) and on the average over 50 years abundance of larvae (orange) and adults (red). The data are plotted with respect to the adult mortality, for juveniles we assumed mm JJ = 2mm AA. NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 7

Model phytoplankton net growth rate, gg PPh ll, day -1 Supplementary Figure 7. The seasonal drivers of the population dynamics. The krill model integrates the combined effect of several seasonal drivers. a, The metabolic rate of adults. b, The modelled dynamics of phytoplankton concentrations (green) in the presence of krill compared to the levels of chlorophyll-a measured during 11 years at Palmer station (orange) and the net growth rate of phytoplankton (black line), as defined by equation (6). c, The model outcome for seasonal dependence of ice algae. NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 8

Dry weight, mg 10 2 10 1 10 0 Fitting Meyer et al., 2009 Atkinson et al., 2006 Lowe et al., 2012 Ross and Quetin 1984 Assimilated food 1 0.8 0.6 0.4 Growth Reproduction 10-1 0.2 10-2 10 0 10 1 Length, mm 0 0 10 20 30 40 50 60 70 Krill length, mm Supplementary Figure 8. Parametrization of the krill model. a, Relationship between dry weight and length of the individuals, ww = cc ww LL σσ 1+σσ 2 ln LL, see parameter values in Supplementary Table 3. b, The splitting of the assimilated food with increasing length of the individuals into growth and reproduction processes as defined by the function KK(ww) = (1 + ee kk(ll(ww) LLrrrrrrrr) ) 1. NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 9

Supplementary Figure 9. Krill life traits. Comparison of the model prediction for (a) the daily growth rates and (b) daily fecundity rate for different levels of food (mg C/m 3, shown by different colors) with field data 33,34,39,45,49 (symbols). Note: Krill can shrink if the resource is less than 1 mg C/m3. c, Modelled krill mortality as a function of krill length for different levels of food availability. The dark red line shows the background mortality which decreases with krill size. The other lines show a sum of the background mortality and starvation mortality for different food levels. The maximal mortality is 40 year -1,which implies that after 14 days of starvation only approximately 20% of population survive. d, The dynamics of krill shrinking 17 (black lines) in comparison with the model outcome (blue lines) for starving krill. NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 10

Supplementary Figure 10. A map of the LTER grid for 1991-1997. During the observational period, the data were sampled with different frequency across the LTER grid. The grid lines were spaced 100 km apart with sampling stations along every line spaced 20 km apart. The number of a grid line or a grid station shows the distance in km from line 000 or station 000, respectively. The title shows the number (nn) of stations, which were sampled during the cruise, and the total number of samples, which can be larger than the number of stations when more than one sample was taken at the same location. NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 11

Supplementary Figures 11. The same as Fig. S10, years 1998-2005 NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 12

Supplementary Figures 12 The same as Fig. S10, years 2006-2013 NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 13

Supplementary Table 1. Krill growth and reproduction Parameter Value Units Meaning Source larvae age 30 days minimal age of larvae Juvenile age 1 years The minimal age of juveniles Reproductive age 2 years Minimal age for reproduction life span 5.9 years krill life span LL ll 7 mm minimal larvae size kk_ll 1/3 mm-1 LL rrrrrrrr,mmmmmm 35 mm the minimal length for reproduction 45 LL rrrrrrrr 43 mm the length at which 50% of female reproduce 36 kk rrrrrrrr 1/5 mm-1 LL ee 0.6 mm Egg size 32,50 ww ee 0.027 mg Egg dry weight εε oooooooooo 0.82 the relative weight of eggs in ovary tissue TT 0.003 1/day Maintenance coefficient TT_ll 0.01 d-1 Maintenance of larvae 17 dd ee 5 year-1 Mortality of embryos dd ll 5 year-1 Mortality of larvae dd jj 1 year-1 Mortality of juveniles 46 dd aa 0.5 year-1 Mortality of adults 46 dd ssss 40 year-1 Maximal starvation mortality NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 14

Supplementary Table 2. Krill Ingestion rate Parameter Value Units Meaning Source HH 25 mg C/m3 Half-saturation constant for growth rate and ingestion rage II 0 10 (% body C/d-1) Maximal ingestion rate 38 εε 1.04 mg DW /mg consumed C SUPPLEMENTARY INFORMATION Assimilation efficiency of consumed carbon into dry weight γγ CC2DDDD 0.4 mgc/mgdw Carbon weight dry weight 38 39 Supplementary Table 3 Relationship between krill length and dry weight, Eq (1) Parameter Value Units Meaning Source cc ww 0.0058 33 35 σσ 1 1.8050 σσ 2 0.2380 LL ee 0.6 mm Egg size 32,50 ww ee 0.0277 mg Egg dry weight NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 15

Supplementary Table 4. Parameters of carbon production Parameter Value Units Meaning PP PPh mg C/m 3 Density of phytoplankton in the water column PP IIIIII mg C/m 3 The density of ice algae CC: CChll 50 mg C/mg Chl Carbon to chlorophyll ratio tt PPh 305 (1st of November) day of year The midpoint of phytoplankton growth period TT PPh 180 days The duration of summer period gg PPh,mmmmmm 0.07 Maximal phytoplankton growth rate KK PPh 120 mg C/m 3 Carrying capacity of phytoplankton growth ll PPh 0.01 day -1 Loss rate of phytoplankton δδ PPh,iiii 0.01 mg C m -3 day -1 Inflow rate of phytoplankton from adjacent patches tt IIIIII 250 day of year The middle of the winter period TT IIIIII 140 days The duration of summer period gg IIIIII,mmmmmm 1 day -1 Maximal growth rate of ice algae KK IIIIII 50 mg C/m 3 Carrying capacity for ice alga ll IIIIII 0.2 day -1 Loss rate of ice algae δδ IIIIII,iiii 0.01 mg C m -3 day -1 ρρ 20 SUPPLEMENTARY INFORMATION Inflow rate of phytoplankton from adjacent patches The ratio of the feeding depths for larvae feeding in the water column or at the surface ice The parameters in table S4 were chosen to fit LTER data chlorophyll dynamics, figure S7 NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 16

Supplementary Table 5. Krill abundance, biomass and recruitment (Fig. 1 c, e) Year Recruitment 95%CI (std) Abundance, ind/m 3 95% CI (std) Biomass, mg DW/m 3 95% CI (std) Number of samples, included 1991 nov 0.93± (0.029) 10 1993 0.03±0.012 (0.028) 0.23±0.06 (0.14) 18±5.4 (13) 36 1994 0.071±0.027 (0.063) 0.046±0.009 (0.021) 4.5±1.1 (2.6) 35 1995 0.22±0.029 (0.078) 0.012±0.0018 (0.0048) 1.6±0.3 (0.8) 45 1996 0.76±0.09 (0.26) 0.059±0.0072 (0.02) 3±0.51 (1.4) 50 1997 0.5±0.093 (0.27) 0.25±0.046 (0.13) 9.2±1.7 (5) 54 1998 0.11±0.031 (0.084) 0.086±0.017 (0.047) 5.8±1.1 (3) 45 1999 0.0021±0.00054 (0.0018) 0.037±0.0034 (0.011) 5.9±0.93 (3.1) 71 2000 0.066±0.024 (0.062) 0.016±0.0019 (0.0049) 2.6±0.46 (1.2) 43 2001 0.076±0.02 (0.054) 0.011±0.0012 (0.0033) 2.3±0.4 (1.1) 48 2002 0.87±0.052 (0.14) 0.11±0.016 (0.045) 2.8±0.46 (1.3) 47 2003 0.4±0.05 (0.15) 0.14±0.022 (0.063) 8.3±1.5 (4.4) 53 2004 0.13±0.041 (0.12) 0.038±0.0057 (0.017) 3.5±0.61 (1.8) 54 2005 0.086±0.018 (0.053) 0.027±0.0033 (0.0096) 3.4±0.54 (1.6) 55 2006 0.15±0.032 (0.09) 0.019±0.0025 (0.0071) 3.7±0.69 (2) 51 2007 0.66±0.069 (0.21) 0.046±0.0068 (0.02) 3±0.54 (1.6) 55 2008 0.75±0.075 (0.22) 0.3±0.058 (0.18) 11±2 (5.9) 56 2009 0.18±0.021 (0.031) 0.046±0.019 (0.029) 3.9±1.6 (2.3) 14 2010 0.16±0.031 (0.05) 0.016±0.006 (0.0096) 2.1±0.64 (1) 16 2011 0.66±0.17 (0.29) 0.028±0.0074 (0.013) 1.8±0.55 (0.97) 19 2012 0.64±0.1 (0.15) 0.42±0.22 (0.33) 8.1±2.6 (3.9) 14 2013 0.3±0.075 (0.13) 19 NATURE ECOLOGY & EVOLUTION DOI: 10.1038/s41559-017-0177 www.nature.com/natecolevol 17