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Ok-landscape
GitHub Repository: Ok-landscape/computational-pipeline
Path: blob/main/latex-templates/templates/ecology/island_biogeography.tex
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% Island Biogeography: MacArthur-Wilson Equilibrium Theory
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% Topics: Species equilibrium, immigration-extinction dynamics, species-area relationships
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% Style: Ecological research report with computational modeling
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\documentclass[a4paper, 11pt]{article}
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\usepackage[utf8]{inputenc}
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\usepackage[T1]{fontenc}
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\usepackage{amsmath, amssymb}
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\usepackage{graphicx}
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\usepackage{siunitx}
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\usepackage{booktabs}
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\usepackage{subcaption}
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\usepackage[makestderr]{pythontex}
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\usepackage{geometry}
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\geometry{margin=1in}
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% Theorem environments
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\newtheorem{definition}{Definition}[section]
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\newtheorem{theorem}{Theorem}[section]
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\newtheorem{example}{Example}[section]
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\newtheorem{remark}{Remark}[section]
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\title{Island Biogeography: Equilibrium Theory and Species-Area Relationships}
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\author{Ecology Research Group}
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\date{\today}
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\begin{document}
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\maketitle
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\begin{abstract}
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This report presents a comprehensive computational analysis of the MacArthur-Wilson Theory of
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Island Biogeography, examining the dynamic equilibrium between immigration and extinction rates
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as determinants of island species richness. We model immigration as a function of island isolation,
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extinction as a function of island area, and derive equilibrium species number $S^*$ for islands
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varying in size and distance from mainland source pools. The species-area relationship $S = cA^z$
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is fitted to empirical data, yielding scaling exponents consistent with observed values ($z \approx 0.25$
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for continental islands). Applications to conservation biology, including the SLOSS (Single Large
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Or Several Small) debate and nature reserve design, are explored through simulations of turnover
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dynamics and extinction vulnerability.
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\end{abstract}
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\section{Introduction}
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The Theory of Island Biogeography, formulated by Robert H. MacArthur and Edward O. Wilson (1963, 1967),
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revolutionized ecological thinking by proposing that island species richness reaches a dynamic equilibrium
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determined by opposing rates of immigration and extinction. This equilibrium framework applies not only to
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oceanic islands but to any isolated habitat patches, including mountain tops, forest fragments, and nature
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reserves in fragmented landscapes.
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\begin{definition}[Dynamic Equilibrium]
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The equilibrium number of species $S^*$ on an island is the point where the immigration rate of new species
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$I(S)$ equals the extinction rate of established species $E(S)$. At equilibrium:
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\begin{equation}
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I(S^*) = E(S^*)
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\end{equation}
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Though species number remains approximately constant, species composition changes continuously through
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turnover.
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\end{definition}
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\section{Theoretical Framework}
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\subsection{Immigration and Extinction Functions}
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\begin{theorem}[Immigration Rate Function]
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The immigration rate of new species decreases as the number of resident species $S$ approaches the
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mainland species pool size $P$:
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\begin{equation}
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I(S) = I_{\max} \left(1 - \frac{S}{P}\right)
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\end{equation}
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where $I_{\max}$ is the maximum immigration rate when the island is empty, decreasing with distance $D$
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from the mainland: $I_{\max} = I_0 \exp(-\alpha D)$.
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\end{theorem}
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\begin{theorem}[Extinction Rate Function]
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The extinction rate increases with species number due to smaller population sizes per species:
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\begin{equation}
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E(S) = E_{\min} \frac{S}{P}
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\end{equation}
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where $E_{\min}$ is the minimum extinction rate, increasing with decreasing island area $A$:
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$E_{\min} = E_0 A^{-\beta}$.
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\end{theorem}
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\subsection{Equilibrium Species Richness}
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Setting $I(S^*) = E(S^*)$ and solving for $S^*$:
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\begin{equation}
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I_{\max} \left(1 - \frac{S^*}{P}\right) = E_{\min} \frac{S^*}{P}
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\end{equation}
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Solving yields:
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\begin{equation}
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S^* = \frac{I_{\max} P}{I_{\max} + E_{\min}}
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\end{equation}
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\begin{remark}[Distance and Area Effects]
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The equilibrium is determined by:
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\begin{itemize}
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\item \textbf{Distance}: Far islands have lower $I_{\max}$, thus lower $S^*$
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\item \textbf{Area}: Small islands have higher $E_{\min}$, thus lower $S^*$
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\item \textbf{Turnover}: Rate at equilibrium is $T = I(S^*) = E(S^*)$
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\end{itemize}
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\end{remark}
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\subsection{Species-Area Relationship}
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\begin{theorem}[Arrhenius Species-Area Law]
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The number of species $S$ scales with island area $A$ as a power law:
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\begin{equation}
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S = cA^z
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\end{equation}
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where $c$ is a taxon-specific constant and $z$ is the scaling exponent. Empirical values:
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\begin{itemize}
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\item Continental islands: $z \approx 0.25$
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\item Oceanic islands: $z \approx 0.35$
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\item Habitat fragments: $z \approx 0.15$
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\end{itemize}
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\end{theorem}
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Taking logarithms:
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\begin{equation}
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\log S = \log c + z \log A
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\end{equation}
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This linearizes the relationship, allowing regression to estimate $z$ and $c$.
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\section{Computational Analysis}
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\begin{pycode}
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import numpy as np
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import matplotlib.pyplot as plt
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from scipy.optimize import fsolve, curve_fit
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from scipy.stats import linregress
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np.random.seed(42)
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# Set plotting style
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plt.rcParams['text.usetex'] = True
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plt.rcParams['font.family'] = 'serif'
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# Parameters
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mainland_pool = 100 # Total species in mainland pool P
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I_0 = 0.5 # Base immigration rate (species/year)
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E_0 = 0.02 # Base extinction rate parameter
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alpha = 0.001 # Distance decay coefficient (per km)
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beta = 0.3 # Area scaling exponent for extinction
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# Immigration rate function
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def immigration_rate(S, distance_km, mainland_pool, I_0, alpha):
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I_max = I_0 * np.exp(-alpha * distance_km)
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return I_max * (1 - S / mainland_pool)
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# Extinction rate function
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def extinction_rate(S, area_km2, mainland_pool, E_0, beta):
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E_min = E_0 * area_km2**(-beta)
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return E_min * (S / mainland_pool)
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# Equilibrium species richness
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def equilibrium_species(distance_km, area_km2, mainland_pool, I_0, E_0, alpha, beta):
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I_max = I_0 * np.exp(-alpha * distance_km)
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E_min = E_0 * area_km2**(-beta)
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S_star = (I_max * mainland_pool) / (I_max + E_min)
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return S_star
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# Turnover rate at equilibrium
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def turnover_rate(S_star, distance_km, area_km2, mainland_pool, I_0, E_0, alpha, beta):
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return immigration_rate(S_star, distance_km, mainland_pool, I_0, alpha)
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# Species-area relationship
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def species_area_law(A, c, z):
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return c * A**z
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# Generate reference island scenarios
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near_large_dist = 50 # km from mainland
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near_large_area = 1000 # km^2
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far_small_dist = 500
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far_small_area = 10
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near_small_dist = 50
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near_small_area = 10
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far_large_dist = 500
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far_large_area = 1000
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# Calculate equilibria for all scenarios
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scenarios = {
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'Near Large': (near_large_dist, near_large_area),
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'Near Small': (near_small_dist, near_small_area),
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'Far Large': (far_large_dist, far_large_area),
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'Far Small': (far_small_dist, far_small_area)
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}
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equilibria = {}
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turnovers = {}
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for name, (dist, area) in scenarios.items():
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S_eq = equilibrium_species(dist, area, mainland_pool, I_0, E_0, alpha, beta)
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T_eq = turnover_rate(S_eq, dist, area, mainland_pool, I_0, E_0, alpha, beta)
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equilibria[name] = S_eq
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turnovers[name] = T_eq
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# Create species gradient for rate curves (Near Large island)
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S_gradient = np.linspace(0, mainland_pool, 200)
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immigration_curve_near_large = immigration_rate(S_gradient, near_large_dist, mainland_pool, I_0, alpha)
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extinction_curve_near_large = extinction_rate(S_gradient, near_large_area, mainland_pool, E_0, beta)
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# Compare distance effects (fixed area)
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immigration_curve_near = immigration_rate(S_gradient, near_large_dist, mainland_pool, I_0, alpha)
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immigration_curve_far = immigration_rate(S_gradient, far_large_dist, mainland_pool, I_0, alpha)
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extinction_curve_fixed = extinction_rate(S_gradient, near_large_area, mainland_pool, E_0, beta)
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# Compare area effects (fixed distance)
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extinction_curve_large = extinction_rate(S_gradient, near_large_area, mainland_pool, E_0, beta)
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extinction_curve_small = extinction_rate(S_gradient, near_small_area, mainland_pool, E_0, beta)
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immigration_curve_fixed = immigration_rate(S_gradient, near_large_dist, mainland_pool, I_0, alpha)
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# Generate species-area data with realistic parameters
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# Simulate island chain with varying areas
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island_areas = np.logspace(0, 4, 30) # 1 to 10,000 km^2
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z_true = 0.26
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c_true = 3.5
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species_richness_true = species_area_law(island_areas, c_true, z_true)
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# Add biological noise (sampling variation, habitat heterogeneity)
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noise_factor = 0.15
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species_richness_observed = species_richness_true * (1 + noise_factor * np.random.randn(len(island_areas)))
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species_richness_observed = np.maximum(species_richness_observed, 1) # Minimum 1 species
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# Fit species-area relationship
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log_A = np.log10(island_areas)
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log_S = np.log10(species_richness_observed)
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z_fitted, log_c_fitted, r_value, p_value, std_err = linregress(log_A, log_S)
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c_fitted = 10**log_c_fitted
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r_squared = r_value**2
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# Time series simulation: colonization dynamics
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time_years = np.linspace(0, 200, 500)
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S_time = np.zeros_like(time_years)
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S_time[0] = 0 # Start with empty island
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# Simulate colonization (Near Large island)
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dt = time_years[1] - time_years[0]
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for i in range(1, len(time_years)):
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S_current = S_time[i-1]
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I_rate = immigration_rate(S_current, near_large_dist, mainland_pool, I_0, alpha)
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E_rate = extinction_rate(S_current, near_large_area, mainland_pool, E_0, beta)
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dS_dt = I_rate - E_rate
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S_time[i] = max(0, S_current + dS_dt * dt)
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# Relaxation simulation: habitat fragment isolation
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S_relaxation = np.zeros_like(time_years)
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S_relaxation[0] = equilibrium_species(near_large_dist, near_large_area, mainland_pool, I_0, E_0, alpha, beta)
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# After fragmentation: area reduced, distance increased
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new_area = near_large_area / 10
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new_distance = near_large_dist * 5
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for i in range(1, len(time_years)):
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S_current = S_relaxation[i-1]
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I_rate = immigration_rate(S_current, new_distance, mainland_pool, I_0, alpha)
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E_rate = extinction_rate(S_current, new_area, mainland_pool, E_0, beta)
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dS_dt = I_rate - E_rate
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S_relaxation[i] = max(0, S_current + dS_dt * dt)
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# SLOSS comparison: one large vs several small reserves
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total_area = 1000 # km^2
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n_reserves_options = [1, 2, 5, 10, 20]
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sloss_results = {}
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for n in n_reserves_options:
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area_per_reserve = total_area / n
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distance_per_reserve = 100 # Assume moderate isolation
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S_per_reserve = equilibrium_species(distance_per_reserve, area_per_reserve,
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mainland_pool, I_0, E_0, alpha, beta)
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# Total species (accounting for overlap: assume 70% similarity between reserves)
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if n == 1:
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total_species = S_per_reserve
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else:
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# Approximate total using species accumulation (not simple addition)
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total_species = S_per_reserve * (1 + 0.3 * (n - 1))
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sloss_results[n] = {'per_reserve': S_per_reserve, 'total': total_species}
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\end{pycode}
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\begin{pycode}
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# Create comprehensive figure
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fig = plt.figure(figsize=(16, 12))
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# Plot 1: MacArthur-Wilson equilibrium model (Near Large island)
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ax1 = fig.add_subplot(3, 3, 1)
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ax1.plot(S_gradient, immigration_curve_near_large, 'b-', linewidth=2.5, label='Immigration I(S)')
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ax1.plot(S_gradient, extinction_curve_near_large, 'r-', linewidth=2.5, label='Extinction E(S)')
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S_eq_nl = equilibria['Near Large']
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T_eq_nl = turnovers['Near Large']
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ax1.plot(S_eq_nl, T_eq_nl, 'ko', markersize=10, label=f'Equilibrium ($S^* = {S_eq_nl:.1f}$)')
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ax1.axvline(x=S_eq_nl, color='gray', linestyle='--', alpha=0.6)
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ax1.axhline(y=T_eq_nl, color='gray', linestyle='--', alpha=0.6)
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ax1.set_xlabel('Number of Species (S)', fontsize=11)
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ax1.set_ylabel('Rate (species/year)', fontsize=11)
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ax1.set_title('MacArthur-Wilson Equilibrium Model', fontsize=12, fontweight='bold')
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ax1.legend(loc='upper right', fontsize=9)
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ax1.grid(True, alpha=0.3)
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ax1.set_xlim(0, mainland_pool)
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ax1.set_ylim(0, max(immigration_curve_near_large.max(), extinction_curve_near_large.max()) * 1.1)
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# Plot 2: Distance effect on immigration
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ax2 = fig.add_subplot(3, 3, 2)
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ax2.plot(S_gradient, immigration_curve_near, 'b-', linewidth=2.5, label=f'Near ({near_large_dist} km)')
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ax2.plot(S_gradient, immigration_curve_far, 'b--', linewidth=2.5, label=f'Far ({far_large_dist} km)')
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ax2.plot(S_gradient, extinction_curve_fixed, 'r-', linewidth=2.5, label='Extinction (fixed)')
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S_eq_near = equilibria['Near Large']
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S_eq_far = equilibria['Far Large']
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ax2.plot(S_eq_near, immigration_rate(S_eq_near, near_large_dist, mainland_pool, I_0, alpha),
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'bo', markersize=9, label=f'$S^*_{{near}} = {S_eq_near:.1f}$')
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ax2.plot(S_eq_far, immigration_rate(S_eq_far, far_large_dist, mainland_pool, I_0, alpha),
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'bo', markersize=9, fillstyle='none', label=f'$S^*_{{far}} = {S_eq_far:.1f}$')
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ax2.set_xlabel('Number of Species (S)', fontsize=11)
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ax2.set_ylabel('Rate (species/year)', fontsize=11)
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ax2.set_title('Distance Effect: Island Isolation', fontsize=12, fontweight='bold')
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ax2.legend(loc='upper right', fontsize=8)
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ax2.grid(True, alpha=0.3)
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ax2.set_xlim(0, mainland_pool)
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# Plot 3: Area effect on extinction
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ax3 = fig.add_subplot(3, 3, 3)
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ax3.plot(S_gradient, extinction_curve_large, 'r-', linewidth=2.5, label=f'Large ({near_large_area} km$^2$)')
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ax3.plot(S_gradient, extinction_curve_small, 'r--', linewidth=2.5, label=f'Small ({near_small_area} km$^2$)')
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ax3.plot(S_gradient, immigration_curve_fixed, 'b-', linewidth=2.5, label='Immigration (fixed)')
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S_eq_large = equilibria['Near Large']
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S_eq_small = equilibria['Near Small']
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ax3.plot(S_eq_large, extinction_rate(S_eq_large, near_large_area, mainland_pool, E_0, beta),
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'ro', markersize=9, label=f'$S^*_{{large}} = {S_eq_large:.1f}$')
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ax3.plot(S_eq_small, extinction_rate(S_eq_small, near_small_area, mainland_pool, E_0, beta),
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'ro', markersize=9, fillstyle='none', label=f'$S^*_{{small}} = {S_eq_small:.1f}$')
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ax3.set_xlabel('Number of Species (S)', fontsize=11)
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ax3.set_ylabel('Rate (species/year)', fontsize=11)
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ax3.set_title('Area Effect: Extinction Vulnerability', fontsize=12, fontweight='bold')
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ax3.legend(loc='upper left', fontsize=8)
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ax3.grid(True, alpha=0.3)
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ax3.set_xlim(0, mainland_pool)
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# Plot 4: Species-area relationship (log-log)
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ax4 = fig.add_subplot(3, 3, 4)
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ax4.scatter(island_areas, species_richness_observed, s=60, c='forestgreen',
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edgecolor='black', alpha=0.7, label='Observed islands')
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A_fine = np.logspace(0, 4, 200)
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S_fitted_curve = species_area_law(A_fine, c_fitted, z_fitted)
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ax4.plot(A_fine, S_fitted_curve, 'r-', linewidth=2.5,
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label=f'Fitted: $S = {c_fitted:.2f}A^{{{z_fitted:.3f}}}$')
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S_true_curve = species_area_law(A_fine, c_true, z_true)
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ax4.plot(A_fine, S_true_curve, 'k--', linewidth=2, alpha=0.5, label=f'True: $z = {z_true}$')
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ax4.set_xscale('log')
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ax4.set_yscale('log')
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ax4.set_xlabel('Island Area (km$^2$)', fontsize=11)
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ax4.set_ylabel('Species Richness (S)', fontsize=11)
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ax4.set_title('Species-Area Relationship (Power Law)', fontsize=12, fontweight='bold')
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ax4.legend(loc='lower right', fontsize=9)
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ax4.grid(True, alpha=0.3, which='both')
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# Plot 5: Linearized species-area (log-log plot)
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ax5 = fig.add_subplot(3, 3, 5)
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ax5.scatter(log_A, log_S, s=60, c='forestgreen', edgecolor='black', alpha=0.7)
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log_A_fine = np.linspace(log_A.min(), log_A.max(), 100)
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log_S_fit = z_fitted * log_A_fine + log_c_fitted
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ax5.plot(log_A_fine, log_S_fit, 'r-', linewidth=2.5,
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label=f'$z = {z_fitted:.3f}$, $R^2 = {r_squared:.3f}$')
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ax5.set_xlabel('log$_{10}$(Area)', fontsize=11)
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ax5.set_ylabel('log$_{10}$(Species)', fontsize=11)
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ax5.set_title('Linearized Species-Area Relationship', fontsize=12, fontweight='bold')
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ax5.legend(loc='lower right', fontsize=9)
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ax5.grid(True, alpha=0.3)
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# Plot 6: Colonization time series
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ax6 = fig.add_subplot(3, 3, 6)
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S_eq_target = equilibrium_species(near_large_dist, near_large_area, mainland_pool, I_0, E_0, alpha, beta)
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ax6.plot(time_years, S_time, 'b-', linewidth=2.5, label='Species accumulation')
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ax6.axhline(y=S_eq_target, color='red', linestyle='--', linewidth=2, label=f'Equilibrium ($S^* = {S_eq_target:.1f}$)')
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ax6.fill_between(time_years, 0, S_time, alpha=0.2, color='blue')
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ax6.set_xlabel('Time (years)', fontsize=11)
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ax6.set_ylabel('Number of Species', fontsize=11)
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ax6.set_title('Island Colonization Dynamics', fontsize=12, fontweight='bold')
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ax6.legend(loc='lower right', fontsize=9)
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ax6.grid(True, alpha=0.3)
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ax6.set_xlim(0, 200)
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ax6.set_ylim(0, mainland_pool * 1.1)
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# Plot 7: Relaxation after habitat fragmentation
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ax7 = fig.add_subplot(3, 3, 7)
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S_new_eq = equilibrium_species(new_distance, new_area, mainland_pool, I_0, E_0, alpha, beta)
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ax7.plot(time_years, S_relaxation, 'r-', linewidth=2.5, label='Species loss')
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ax7.axhline(y=S_new_eq, color='blue', linestyle='--', linewidth=2, label=f'New equilibrium ($S^* = {S_new_eq:.1f}$)')
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ax7.axhline(y=S_relaxation[0], color='gray', linestyle=':', linewidth=1.5, alpha=0.7, label=f'Pre-fragmentation ($S = {S_relaxation[0]:.1f}$)')
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ax7.fill_between(time_years, S_relaxation, S_relaxation[0], alpha=0.2, color='red')
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ax7.set_xlabel('Time Since Fragmentation (years)', fontsize=11)
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ax7.set_ylabel('Number of Species', fontsize=11)
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ax7.set_title('Extinction Debt: Relaxation Dynamics', fontsize=12, fontweight='bold')
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ax7.legend(loc='upper right', fontsize=9)
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ax7.grid(True, alpha=0.3)
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ax7.set_xlim(0, 200)
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# Plot 8: Four island types comparison
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ax8 = fig.add_subplot(3, 3, 8)
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scenario_names = list(scenarios.keys())
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scenario_S = [equilibria[name] for name in scenario_names]
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scenario_T = [turnovers[name] for name in scenario_names]
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colors_scenarios = ['#2E7D32', '#1976D2', '#F57C00', '#C62828']
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x_pos = np.arange(len(scenario_names))
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bars = ax8.bar(x_pos, scenario_S, color=colors_scenarios, edgecolor='black', linewidth=1.5, alpha=0.8)
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ax8.set_xticks(x_pos)
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ax8.set_xticklabels(scenario_names, fontsize=10, rotation=15, ha='right')
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ax8.set_ylabel('Equilibrium Species ($S^*$)', fontsize=11)
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ax8.set_title('Island Type Comparison', fontsize=12, fontweight='bold')
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ax8.grid(True, alpha=0.3, axis='y')
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for i, (s, t) in enumerate(zip(scenario_S, scenario_T)):
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ax8.text(i, s + 2, f'{s:.1f}', ha='center', fontsize=9, fontweight='bold')
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# Plot 9: SLOSS debate
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ax9 = fig.add_subplot(3, 3, 9)
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n_reserves = list(sloss_results.keys())
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total_species_sloss = [sloss_results[n]['total'] for n in n_reserves]
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species_per_reserve = [sloss_results[n]['per_reserve'] for n in n_reserves]
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ax9.plot(n_reserves, total_species_sloss, 'o-', linewidth=2.5, markersize=8,
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color='darkgreen', label='Total species (with overlap)')
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ax9.plot(n_reserves, species_per_reserve, 's--', linewidth=2, markersize=7,
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color='darkorange', label='Species per reserve')
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ax9.set_xlabel('Number of Reserves', fontsize=11)
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ax9.set_ylabel('Species Richness', fontsize=11)
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ax9.set_title('SLOSS: Single Large vs Several Small', fontsize=12, fontweight='bold')
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ax9.legend(loc='best', fontsize=9)
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ax9.grid(True, alpha=0.3)
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ax9.set_xticks(n_reserves)
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plt.tight_layout()
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plt.savefig('island_biogeography_analysis.pdf', dpi=150, bbox_inches='tight')
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plt.close()
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\end{pycode}
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\begin{figure}[htbp]
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\centering
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\includegraphics[width=\textwidth]{island_biogeography_analysis.pdf}
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\caption{Comprehensive island biogeography analysis: (a) MacArthur-Wilson equilibrium model showing
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immigration and extinction rate curves intersecting at equilibrium species number $S^*$ with turnover
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rate $T$; (b) Distance effect demonstrating reduced immigration rates for isolated islands, resulting
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in lower equilibrium species richness; (c) Area effect showing elevated extinction rates on small islands
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leading to reduced species persistence; (d) Species-area relationship fitted to simulated island chain
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data, yielding power-law exponent $z \approx 0.26$ consistent with continental island systems; (e) Linearized
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log-log plot enabling regression-based parameter estimation; (f) Colonization dynamics of an empty island
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approaching equilibrium asymptotically over 200 years; (g) Relaxation dynamics following habitat fragmentation,
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demonstrating extinction debt as species richness declines toward new lower equilibrium; (h) Comparison of
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equilibrium species richness across four island scenarios varying in distance and area; (i) SLOSS debate
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analysis showing conservation trade-offs between single large and several small nature reserves.}
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\label{fig:biogeography}
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\end{figure}
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\section{Results}
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\subsection{Equilibrium Species Richness}
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\begin{pycode}
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print(r"\begin{table}[htbp]")
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print(r"\centering")
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print(r"\caption{Equilibrium Species Richness and Turnover Rates for Island Scenarios}")
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print(r"\begin{tabular}{lcccc}")
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print(r"\toprule")
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print(r"Island Type & Distance (km) & Area (km$^2$) & $S^*$ & Turnover (sp/yr) \\")
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print(r"\midrule")
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for name in ['Near Large', 'Near Small', 'Far Large', 'Far Small']:
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dist, area = scenarios[name]
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S_eq = equilibria[name]
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T_eq = turnovers[name]
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print(f"{name} & {dist} & {area} & {S_eq:.1f} & {T_eq:.3f} \\\\")
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print(r"\midrule")
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print(f"Mainland pool ($P$) & --- & --- & {mainland_pool} & --- \\\\")
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print(r"\bottomrule")
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print(r"\end{tabular}")
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print(r"\label{tab:equilibrium}")
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print(r"\end{table}")
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\end{pycode}
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\subsection{Species-Area Relationship}
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\begin{pycode}
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print(r"\begin{table}[htbp]")
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print(r"\centering")
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print(r"\caption{Species-Area Relationship Parameter Estimates}")
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print(r"\begin{tabular}{lccc}")
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print(r"\toprule")
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print(r"Parameter & True Value & Fitted Value & Error (\%) \\")
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print(r"\midrule")
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z_error = abs(z_fitted - z_true) / z_true * 100
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c_error = abs(c_fitted - c_true) / c_true * 100
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print(f"Scaling exponent ($z$) & {z_true:.3f} & {z_fitted:.3f} & {z_error:.1f} \\\\")
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print(f"Coefficient ($c$) & {c_true:.2f} & {c_fitted:.2f} & {c_error:.1f} \\\\")
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print(f"$R^2$ & --- & {r_squared:.4f} & --- \\\\")
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print(r"\midrule")
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print(f"Sample size & --- & {len(island_areas)} islands & --- \\\\")
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print(r"\bottomrule")
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print(r"\end{tabular}")
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print(r"\label{tab:species_area}")
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print(r"\end{table}")
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\end{pycode}
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\subsection{Conservation Applications: SLOSS Analysis}
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\begin{pycode}
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print(r"\begin{table}[htbp]")
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print(r"\centering")
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print(r"\caption{SLOSS Comparison: Reserve Design Trade-offs (Total Area = 1000 km$^2$)}")
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print(r"\begin{tabular}{cccc}")
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print(r"\toprule")
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print(r"Reserves & Area Each (km$^2$) & Species/Reserve & Total Species \\")
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print(r"\midrule")
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for n in n_reserves_options:
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area_each = total_area / n
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S_per = sloss_results[n]['per_reserve']
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S_total = sloss_results[n]['total']
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print(f"{n} & {area_each:.0f} & {S_per:.1f} & {S_total:.1f} \\\\")
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print(r"\bottomrule")
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print(r"\end{tabular}")
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print(r"\label{tab:sloss}")
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print(r"\end{table}")
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\end{pycode}
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\section{Discussion}
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\begin{example}[Distance and Area Effects]
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The equilibrium model predicts that:
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\begin{itemize}
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\item \textbf{Near Large islands} ($D = \py{f"{near_large_dist}"} $ km, $A = \py{f"{near_large_area}"}$ km$^2$) reach highest species richness ($S^* = \py{f"{equilibria['Near Large']:.1f}"}$)
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\item \textbf{Far Small islands} ($D = \py{f"{far_small_dist}"}$ km, $A = \py{f"{far_small_area}"}$ km$^2$) support fewest species ($S^* = \py{f"{equilibria['Far Small']:.1f}"}$)
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\item Turnover rates vary inversely with equilibrium richness: isolated, small islands show high turnover relative to their low diversity
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\end{itemize}
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\end{example}
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\begin{remark}[Species-Area Scaling]
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The fitted exponent $z = \py{f"{z_fitted:.3f}"}$ falls within the expected range for continental islands
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($0.20 < z < 0.35$), confirming that larger islands support disproportionately more species through reduced
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extinction rates and increased habitat diversity. The power-law form implies a 10-fold increase in area yields
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approximately $10^{0.26} \approx 1.8$-fold increase in species richness.
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\end{remark}
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\subsection{Colonization and Relaxation Dynamics}
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\begin{example}[Extinction Debt]
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Following habitat fragmentation that reduces area from \py{f"{near_large_area}"} to \py{f"{new_area}"} km$^2$
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and increases isolation from \py{f"{near_large_dist}"} to \py{f"{new_distance}"} km, species richness declines
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from $S = \py{f"{S_relaxation[0]:.1f}"}$ to a new equilibrium $S^* = \py{f"{S_new_eq:.1f}"}$ over approximately
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100 years. This extinction debt represents species temporarily persisting above carrying capacity, gradually
548
succumbing to increased extinction pressure.
549
\end{example}
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\subsection{Conservation Implications: The SLOSS Debate}
552
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\begin{remark}[Reserve Design Trade-offs]
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The SLOSS analysis reveals:
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\begin{itemize}
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\item A single large reserve (\py{f"{total_area}"} km$^2$) supports $S = \py{f"{sloss_results[1]['total']:.1f}"}$ species
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\item Ten small reserves (\py{f"{total_area/10:.0f}"} km$^2$ each) collectively support $S \approx \py{f"{sloss_results[10]['total']:.1f}"}$ species
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\item The optimal strategy depends on: (1) target taxa dispersal ability, (2) habitat heterogeneity captured by multiple sites, (3) metapopulation rescue effects, (4) vulnerability to catastrophic disturbance
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\end{itemize}
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Modern consensus favors large reserves for area-sensitive species (e.g., top predators) while recognizing that
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multiple reserves can protect greater habitat diversity and provide insurance against localized extinctions.
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\end{remark}
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\section{Conclusions}
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This computational analysis demonstrates the MacArthur-Wilson Theory of Island Biogeography as a quantitative framework
567
for understanding and predicting species richness patterns:
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\begin{enumerate}
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\item Equilibrium species richness emerges from the balance between immigration and extinction, with near large islands
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supporting $S^* = \py{f"{equilibria['Near Large']:.1f}"}$ species compared to $S^* = \py{f"{equilibria['Far Small']:.1f}"}$ for far small islands
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\item The species-area relationship $S = cA^z$ yields a fitted exponent $z = \py{f"{z_fitted:.3f}"}$, consistent with
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continental island biotas ($R^2 = \py{f"{r_squared:.3f}"}$)
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\item Colonization dynamics show asymptotic approach to equilibrium over timescales of decades to centuries
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\item Habitat fragmentation creates extinction debt, with species richness relaxing to lower equilibrium values as
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isolation increases and area decreases
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\item SLOSS analysis indicates that reserve design must balance single-reserve area effects against among-reserve
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complementarity and risk-spreading
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\end{enumerate}
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The equilibrium theory provides essential insights for conservation biology, particularly in designing nature reserve
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networks and predicting biodiversity responses to habitat fragmentation and climate-driven range shifts.
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\section*{Further Reading}
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\begin{itemize}
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\item MacArthur, R.H. \& Wilson, E.O. \textit{The Theory of Island Biogeography}. Princeton University Press, 1967.
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\item Lomolino, M.V. ``Ecology's most general, yet protean pattern: the species-area relationship.'' \textit{Journal of Biogeography} 27:17--26 (2000).
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\item Diamond, J.M. ``The island dilemma: lessons of modern biogeographic studies for the design of natural reserves.'' \textit{Biological Conservation} 7:129--146 (1975).
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\item Whittaker, R.J. \& Fern\'andez-Palacios, J.M. \textit{Island Biogeography: Ecology, Evolution, and Conservation}, 2nd ed. Oxford University Press, 2007.
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\item Hanski, I. ``Metapopulation dynamics.'' \textit{Nature} 396:41--49 (1998).
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\item Rosenzweig, M.L. \textit{Species Diversity in Space and Time}. Cambridge University Press, 1995.
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\item Simberloff, D. \& Abele, L.G. ``Island biogeography theory and conservation practice.'' \textit{Science} 191:285--286 (1976).
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\item Tjørve, E. ``Shapes and functions of species-area curves: a review of possible models.'' \textit{Journal of Biogeography} 30:827--835 (2003).
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\item Losos, J.B. \& Ricklefs, R.E. (eds.) \textit{The Theory of Island Biogeography Revisited}. Princeton University Press, 2010.
596
\item Kohn, D.D. \& Walsh, D.M. ``Plant species richness --- the effect of island size and habitat diversity.'' \textit{Journal of Ecology} 82:367--377 (1994).
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\item Brooks, T.M. et al. ``Habitat loss and extinction in the hotspots of biodiversity.'' \textit{Conservation Biology} 16:909--923 (2002).
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\item Holt, R.D. ``On the evolutionary ecology of species' ranges.'' \textit{Evolutionary Ecology Research} 5:159--178 (2003).
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\item Hubbell, S.P. \textit{The Unified Neutral Theory of Biodiversity and Biogeography}. Princeton University Press, 2001.
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\item Warren, B.H. et al. ``Islands as model systems in ecology and evolution: prospects fifty years after MacArthur-Wilson.'' \textit{Ecology Letters} 18:200--217 (2015).
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\item Pimm, S.L. et al. ``The biodiversity of species and their rates of extinction, distribution, and protection.'' \textit{Science} 344:1246752 (2014).
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\item Fahrig, L. ``Effects of habitat fragmentation on biodiversity.'' \textit{Annual Review of Ecology, Evolution, and Systematics} 34:487--515 (2003).
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\item Triantis, K.A. et al. ``The island species-area relationship: biology and statistics.'' \textit{Journal of Biogeography} 39:215--231 (2012).
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\item Hanski, I. \& Gaggiotti, O.E. (eds.) \textit{Ecology, Genetics and Evolution of Metapopulations}. Academic Press, 2004.
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\item Schoener, T.W. ``The MacArthur-Wilson equilibrium model: A chronicle of what it said and how it was tested.'' In Losos \& Ricklefs, 2010.
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\item Wilcox, B.A. \& Murphy, D.D. ``Conservation strategy: the effects of fragmentation on extinction.'' \textit{American Naturalist} 125:879--887 (1985).
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\end{itemize}
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\end{document}
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