Local intraspecific aggregation in phytoplankton model communities spatial scales of occurrence and implications for coexistence

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Local intraspecific aggregation in phytoplankton model
communities: spatial scales of occurrence and
implications for coexistence
Coralie Picoche1,, William R. Young2, Frédéric Barraquand1,
1Institute of Mathematics of Bordeaux, University of Bordeaux and CNRS, Talence, France
2Scripps Institution of Oceanography, La Jolla, California, USA
Abstract
The coexistence of multiple phytoplankton species despite their reliance on similar resources
is often explained with mean-field models assuming mixed populations. In reality, observa-
tions of phytoplankton indicate spatial aggregation at all scales, including at the scale of a
few individuals. Local spatial aggregation can hinder competitive exclusion since individu-
als then interact mostly with other individuals of their own species, rather than competitors
from different species. To evaluate how microscale spatial aggregation might explain phyto-
plankton diversity maintenance, an individual-based, multispecies representation of cells in a
hydrodynamic environment is required. We formulate a three-dimensional and multispecies
individual-based model of phytoplankton population dynamics at the Kolmogorov scale. The
model is studied through both simulations and the derivation of spatial moment equations,
in connection with point process theory. The spatial moment equations show a good match
between theory and simulations. We parameterized the model based on phytoplankters’ eco-
logical and physical characteristics, for both large and small phytoplankton. Defining a zone
of potential interactions as the overlap between nutrient depletion volumes, we show that
local species composition—within the range of possible interactions—depends on the size
class of phytoplankton. In small phytoplankton, individuals remain in mostly monospecific
clusters. Spatial structure therefore favours intra- over inter-specific interactions for small
phytoplankton, contributing to coexistence. Large phytoplankton cell neighbourhoods ap-
pear more mixed. Although some small-scale self-organizing spatial structure remains and
could influence coexistence mechanisms, other factors may need to be explored to explain
diversity maintenance in large phytoplankton.
Keywords: aggregation; coexistence; individual-based model; phytoplankton; spatial
moment equations; spatial point process
correspondence to: frederic.barraquand@u-bordeaux.fr &cpicoche@gmail.com
Published in Journal of Mathematical Biology with DOI:10.1007/s00285-024-02067-y
arXiv:2210.11364v2 [q-bio.PE] 22 Apr 2024
Introduction
Phytoplankton communities are among the most important photosynthetic groups on Earth,
being at the bottom of the marine food chain, and responsible for approximately half the
global primary production (Field et al.,1998). Their contribution to ecosystem functions
is only matched by their contribution to biodiversity. Indeed, phytoplankton communities
are characterized by a surprisingly high number of species. For example, a single sample
as small as a few mL can contain up to seventy species (REPHY,2017;Widdicombe &
Harbour,2021). This observation is usually called the “paradox of the plankton” (a term
coined by Hutchinson,1961), which refers to the conflict between the observed diversity of
species competing for similar resources in a seemingly homogeneous environment, and models
predicting that only a few species will persist by outcompeting the others (MacArthur &
Levins,1964;Huisman & Weissing,1999;Schippers et al.,2001). Phytoplankton models for
coexistence are now almost as diverse as their model organisms (Record et al.,2014), but they
often describe only a handful of species, which does not correspond to the diversity observed in
the field. When modeling rich communities (> 10 species), classical answers to the plankton
paradox involving temporal fluctuations (e.g., Li & Chesson,2016;Chesson,2018) are not
sufficient to maintain a realistic diversity. For instance, we found that a phytoplankton
community dynamics model with environmental fluctuations and storage effect still requires
extra niche differentiation for coexistence, which manifests in stronger intraspecific than
interspecific interactions (Picoche & Barraquand,2019). However, it is not clear that we
should resort to hidden niches to explain phytoplankton coexistence, as most models also
make hidden simplifying assumptions that could be relaxed. One that we relax here is mean-
field dynamics at the microscale. Indeed, field observations have revealed phytoplankton
patchiness for decades, with early records in the past centuries (Bainbridge,1957;Stocker,
2012), from the macro- to the micro-scale (Leonard et al.,2001;Doubell et al.,2006;Font-
Muñoz et al.,2017).
Phytoplankton patchiness can at least be partly explained by the hydrodynamics of their
environment: the size of these organisms is mostly below the size of the smallest eddy (i.e.,
the Kolmogorov scale). In a typical aquatic environment such as the ocean, phytoplankton
individuals are embedded in viscous micro-structures (Peters & Marrasé,2000) while phy-
toplankton populations are displaced by a turbulent flow at slighly larger scales (Martin,
2003;Prairie et al.,2012). Phytoplankton organisms therefore live in an environment where
fluid viscosity dominates at the scale of an individual but turbulent dispersion dominates on
length scales characteristic of a small population of those individuals (Estrada et al.,1987;
Prairie et al.,2012).
2
This leads us to consider demography in the context of this environmental variation cre-
ated by hydrodynamic processes. Individual-based models provide a convenient depiction of
population dynamics and movement at the microscale (Hellweger & Bucci,2009). In this
framework, population growth is a result of individual births and deaths. Aggregation of
individuals can emerge from local reproduction coupled with limited dispersal, which can
happen in a fluid where turbulence and diffusion are not strong enough to disperse kin ag-
gregates (Young et al.,2001). The resulting local aggregation can then affect the community
dynamics at larger spatial scales, even when all competitors are equivalent (i.e., with equal
interaction strengths irrespective of species identity). Indeed, the combination of local dis-
persal after reproduction and local interactions leads to stronger intraspecific interactions
than interspecific interactions at the population level (Detto & Muller-Landau,2016). This
mechanism stabilizes the community, as a high intra-to-interspecific interaction strength ratio
makes a species control its abundance more than it controls the abundance of other species,
which is associated with coexistence in theoretical models (Levine & HilleRisLambers,2009;
Barabás et al.,2017) and often observed in the field at the population level (Adler et al.,
2018;Picoche & Barraquand,2020). Therefore, the microscale spatial distribution of indi-
viduals likely affects the interaction structure within a community, and may sustain diversity
(Haegeman & Rapaport,2008).
Existing models of phytoplankton populations near the Kolmogorov scale — between 1
mm and 1 cm in an oceanic environment (Barton et al.,2014) — focus on a single species and
the clustering of its individuals (Young et al.,2001;Birch & Young,2006;Bouderbala et al.,
2018;Breier et al.,2018). These models share similarities to dynamic point process models
(Law et al.,2003;Bolker & Pacala,1999;Plank & Law,2015) developed initially with larger
organisms in mind. When phytoplankton individual-based models consider multiple types of
organisms, they focus for now on how organisms with opposite characteristics (e.g., increase
versus decrease in density with turbulence in Borgnino et al.,2019;Arrieta et al.,2020)
segregate spatially, or on coexistence of species that have contrasting trait values (e.g., size
in Benczik et al.,2006). Such models are useful as an explanation of how species with marked
differences might coexist. The difficulty of the coexistence problem, however, is that we also
have to explain how closely related species or genera (e.g., within diatoms), many of whom
have similar size, buoyancy, chemical composition, etc., manage to coexist within a single
trophic level. This requires modelling similar species in a spatially realistic environment and
objectively quantifying whether they aggregate or segregate in space.
To do so, we build a multispecies version of the Brownian Bug Model (BBM) of Young
et al. (2001), an individual-based model which includes an advection process mimicking a
turbulent fluid flow, passive diffusion of organisms, as well as stochastic birth and death pro-
3
cesses. The initial version of this model (Young et al.,2001) coupled limited dispersal and
local reproduction with ocean-like microscale hydrodynamics, and showed spatial clusters of
individuals of the same species. The original BBM was limited to a single species and was
illustrated with two-dimensional simulations. The model was not strongly quantitative (Pic-
oche et al.,2022) in the sense that parameters were not informed by current knowledge on
phytoplankton biology (numbers of cells per liter, diffusion characteristics, etc.). As phyto-
plankton organisms live in a three-dimensional environment, informing the model with more
realistic parameters requires us to shift to three dimensions. We also extend the model to
multiple species, and consider two size classes for our phytoplankton communities, which are
either made of nanophytoplankton (3 µm diameter, 106cells L1) or microphytoplankton
(50 µm, 104cells L1). We populate each community with 3 to 10 different species.
The Brownian Bug Model (in its original single-species form as in the multispecies ver-
sion considered here) is related to spatial branching processes. Without advection, it com-
bines a continuous-time, discrete-state model for population growth and a continuous-time,
continuous-space Brownian motion for particle diffusion (Birch & Young,2006). It is fur-
ther complexified by a turbulent flow in Young et al. (2001); Picoche et al. (2022) as well
as here. In spite of this complexity, it remains possible to derive the dynamics of pair den-
sity functions, which quantify the degree of intra- and interspecific clustering of organisms,
via correlations between positions of organisms (see next section). Thus we can understand
emergent spatial structures in analytic detail and compare these predictions to the results
from three-dimensional simulations. Furthermore, because we do not consider direct inter-
actions between organisms, the multispecies spatial point process that represents the stable
state of the BBM is a random superposition of spatial point processes for each species (Illian
et al.,2008). This enables us to derive, in addition to pair correlation functions, analytical
formulas for the species composition in the neighbourhood of an individual, which are more
readily ecologically interpreted than pair density or correlation functions.
Model and spatial statistics
Brownian Bug Model
The Brownian Bug Model (BBM) describes the dynamics of individuals in a turbulent and
viscous environment, including demographic processes. The model is continuous in space
and time. Here we extend the mostly two-dimensional, monospecific version in Young et al.
(2001), to three dimensions and Sspecies.
Each individual is characterized by its species identity iand its position xT= (x, y, z).
4
The population dynamics are modelled by a linear birth-death process with birth rate λi
and death rate µi. Each individual independently follows a Brownian motion with diffusivity
Di, and is advected by a common stochastic and chaotic flow modelling turbulence. The
model applies in the Batchelor regime, which means that the separation s(t)between two
individuals kand lgrows exponentially with time with stretching parameter γ, i.e., s(t) =
ln (|xkxl|(t)) 3γt (Kraichnan,1974;Young et al.,2001).
Within a given community (the set of all individuals of the Sspecies), all species share the
same parameters: λi,µiand Divalues can change between communities, as we later consider
small and large phytoplankton, but are set to common values within a community. On the
contrary, γdescribes the environment and is not community-specific, i.e., all individuals
are displaced by the same turbulent stirring. For numerical simulations, time needs to be
discretized (this is required for diffusion and advection modelling). The approximated model
advances through time in small steps of duration τ. During each interval, events unroll as
follows:
1. Demography: each individual can either reproduce with probability pi=λiτ(forming
a new individual of the same species iat the same position xas the parent), die with
probability qi=µiτ, or remain unchanged with probability 1piqi.
2. Diffusion: each individual moves to a new position x(t) = x(t) + δx(t), with t < t<
t+τ. The random displacement δx(t)is drawn from a Gaussian distribution N(0,2
i)
with Di= ∆2
i/2τthe diffusivity. This diffusive step separates the initially coincident
pairs produced by reproduction in step 1 above.
3. Turbulence: each individual is displaced by a turbulent flow, modelled with the Pier-
rehumbert map (Pierrehumbert,1994), adapted to three dimensions following Ngan &
Vanneste (2011). Thus given the position at time tthe updated position at time t+τ
is
x(t+τ) = x(t) + Uτ
3cos (ky(t) + ϕ(t))
y(t+τ) = y(t) + Uτ
3cos (kz(t) + θ(t))
z(t+τ) = z(t) + U τ
3cos (kx(t+τ) + ψ(t)) .
(1)
Above, Uis the velocity of the flow, k= 2π/Lsis the wavenumber for the flow at the length
scale Ls(see below) and ϕ(t),θ(t),ψ(t)are random phases drawn from a uniform distribution
between 0and 2π; these phases remain constant during the interval between tand t+τ.
The shift from continuous to discrete-time turbulence modelling is described in Section S1 in
the Supplementary Information. The velocity Uis related to γ. As the separation between
two points grows exponentially with parameter 3γdue to turbulence, the exponent γcan be
5
摘要:

Localintraspecificaggregationinphytoplanktonmodelcommunities:spatialscalesofoccurrenceandimplicationsforcoexistenceCoraliePicoche1,∗,WilliamR.Young2,FrédéricBarraquand1,∗1InstituteofMathematicsofBordeaux,UniversityofBordeauxandCNRS,Talence,France2ScrippsInstitutionofOceanography,LaJolla,California,U...

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