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% Island Biogeography: MacArthur-Wilson Equilibrium Theory1% Topics: Species equilibrium, immigration-extinction dynamics, species-area relationships2% Style: Ecological research report with computational modeling34\documentclass[a4paper, 11pt]{article}5\usepackage[utf8]{inputenc}6\usepackage[T1]{fontenc}7\usepackage{amsmath, amssymb}8\usepackage{graphicx}9\usepackage{siunitx}10\usepackage{booktabs}11\usepackage{subcaption}12\usepackage[makestderr]{pythontex}13\usepackage{geometry}14\geometry{margin=1in}1516% Theorem environments17\newtheorem{definition}{Definition}[section]18\newtheorem{theorem}{Theorem}[section]19\newtheorem{example}{Example}[section]20\newtheorem{remark}{Remark}[section]2122\title{Island Biogeography: Equilibrium Theory and Species-Area Relationships}23\author{Ecology Research Group}24\date{\today}2526\begin{document}27\maketitle2829\begin{abstract}30This report presents a comprehensive computational analysis of the MacArthur-Wilson Theory of31Island Biogeography, examining the dynamic equilibrium between immigration and extinction rates32as determinants of island species richness. We model immigration as a function of island isolation,33extinction as a function of island area, and derive equilibrium species number $S^*$ for islands34varying in size and distance from mainland source pools. The species-area relationship $S = cA^z$35is fitted to empirical data, yielding scaling exponents consistent with observed values ($z \approx 0.25$36for continental islands). Applications to conservation biology, including the SLOSS (Single Large37Or Several Small) debate and nature reserve design, are explored through simulations of turnover38dynamics and extinction vulnerability.39\end{abstract}4041\section{Introduction}4243The Theory of Island Biogeography, formulated by Robert H. MacArthur and Edward O. Wilson (1963, 1967),44revolutionized ecological thinking by proposing that island species richness reaches a dynamic equilibrium45determined by opposing rates of immigration and extinction. This equilibrium framework applies not only to46oceanic islands but to any isolated habitat patches, including mountain tops, forest fragments, and nature47reserves in fragmented landscapes.4849\begin{definition}[Dynamic Equilibrium]50The equilibrium number of species $S^*$ on an island is the point where the immigration rate of new species51$I(S)$ equals the extinction rate of established species $E(S)$. At equilibrium:52\begin{equation}53I(S^*) = E(S^*)54\end{equation}55Though species number remains approximately constant, species composition changes continuously through56turnover.57\end{definition}5859\section{Theoretical Framework}6061\subsection{Immigration and Extinction Functions}6263\begin{theorem}[Immigration Rate Function]64The immigration rate of new species decreases as the number of resident species $S$ approaches the65mainland species pool size $P$:66\begin{equation}67I(S) = I_{\max} \left(1 - \frac{S}{P}\right)68\end{equation}69where $I_{\max}$ is the maximum immigration rate when the island is empty, decreasing with distance $D$70from the mainland: $I_{\max} = I_0 \exp(-\alpha D)$.71\end{theorem}7273\begin{theorem}[Extinction Rate Function]74The extinction rate increases with species number due to smaller population sizes per species:75\begin{equation}76E(S) = E_{\min} \frac{S}{P}77\end{equation}78where $E_{\min}$ is the minimum extinction rate, increasing with decreasing island area $A$:79$E_{\min} = E_0 A^{-\beta}$.80\end{theorem}8182\subsection{Equilibrium Species Richness}8384Setting $I(S^*) = E(S^*)$ and solving for $S^*$:85\begin{equation}86I_{\max} \left(1 - \frac{S^*}{P}\right) = E_{\min} \frac{S^*}{P}87\end{equation}8889Solving yields:90\begin{equation}91S^* = \frac{I_{\max} P}{I_{\max} + E_{\min}}92\end{equation}9394\begin{remark}[Distance and Area Effects]95The equilibrium is determined by:96\begin{itemize}97\item \textbf{Distance}: Far islands have lower $I_{\max}$, thus lower $S^*$98\item \textbf{Area}: Small islands have higher $E_{\min}$, thus lower $S^*$99\item \textbf{Turnover}: Rate at equilibrium is $T = I(S^*) = E(S^*)$100\end{itemize}101\end{remark}102103\subsection{Species-Area Relationship}104105\begin{theorem}[Arrhenius Species-Area Law]106The number of species $S$ scales with island area $A$ as a power law:107\begin{equation}108S = cA^z109\end{equation}110where $c$ is a taxon-specific constant and $z$ is the scaling exponent. Empirical values:111\begin{itemize}112\item Continental islands: $z \approx 0.25$113\item Oceanic islands: $z \approx 0.35$114\item Habitat fragments: $z \approx 0.15$115\end{itemize}116\end{theorem}117118Taking logarithms:119\begin{equation}120\log S = \log c + z \log A121\end{equation}122This linearizes the relationship, allowing regression to estimate $z$ and $c$.123124\section{Computational Analysis}125126\begin{pycode}127import numpy as np128import matplotlib.pyplot as plt129from scipy.optimize import fsolve, curve_fit130from scipy.stats import linregress131132np.random.seed(42)133134# Set plotting style135plt.rcParams['text.usetex'] = True136plt.rcParams['font.family'] = 'serif'137138# Parameters139mainland_pool = 100 # Total species in mainland pool P140I_0 = 0.5 # Base immigration rate (species/year)141E_0 = 0.02 # Base extinction rate parameter142alpha = 0.001 # Distance decay coefficient (per km)143beta = 0.3 # Area scaling exponent for extinction144145# Immigration rate function146def immigration_rate(S, distance_km, mainland_pool, I_0, alpha):147I_max = I_0 * np.exp(-alpha * distance_km)148return I_max * (1 - S / mainland_pool)149150# Extinction rate function151def extinction_rate(S, area_km2, mainland_pool, E_0, beta):152E_min = E_0 * area_km2**(-beta)153return E_min * (S / mainland_pool)154155# Equilibrium species richness156def equilibrium_species(distance_km, area_km2, mainland_pool, I_0, E_0, alpha, beta):157I_max = I_0 * np.exp(-alpha * distance_km)158E_min = E_0 * area_km2**(-beta)159S_star = (I_max * mainland_pool) / (I_max + E_min)160return S_star161162# Turnover rate at equilibrium163def turnover_rate(S_star, distance_km, area_km2, mainland_pool, I_0, E_0, alpha, beta):164return immigration_rate(S_star, distance_km, mainland_pool, I_0, alpha)165166# Species-area relationship167def species_area_law(A, c, z):168return c * A**z169170# Generate reference island scenarios171near_large_dist = 50 # km from mainland172near_large_area = 1000 # km^2173far_small_dist = 500174far_small_area = 10175near_small_dist = 50176near_small_area = 10177far_large_dist = 500178far_large_area = 1000179180# Calculate equilibria for all scenarios181scenarios = {182'Near Large': (near_large_dist, near_large_area),183'Near Small': (near_small_dist, near_small_area),184'Far Large': (far_large_dist, far_large_area),185'Far Small': (far_small_dist, far_small_area)186}187188equilibria = {}189turnovers = {}190for name, (dist, area) in scenarios.items():191S_eq = equilibrium_species(dist, area, mainland_pool, I_0, E_0, alpha, beta)192T_eq = turnover_rate(S_eq, dist, area, mainland_pool, I_0, E_0, alpha, beta)193equilibria[name] = S_eq194turnovers[name] = T_eq195196# Create species gradient for rate curves (Near Large island)197S_gradient = np.linspace(0, mainland_pool, 200)198immigration_curve_near_large = immigration_rate(S_gradient, near_large_dist, mainland_pool, I_0, alpha)199extinction_curve_near_large = extinction_rate(S_gradient, near_large_area, mainland_pool, E_0, beta)200201# Compare distance effects (fixed area)202immigration_curve_near = immigration_rate(S_gradient, near_large_dist, mainland_pool, I_0, alpha)203immigration_curve_far = immigration_rate(S_gradient, far_large_dist, mainland_pool, I_0, alpha)204extinction_curve_fixed = extinction_rate(S_gradient, near_large_area, mainland_pool, E_0, beta)205206# Compare area effects (fixed distance)207extinction_curve_large = extinction_rate(S_gradient, near_large_area, mainland_pool, E_0, beta)208extinction_curve_small = extinction_rate(S_gradient, near_small_area, mainland_pool, E_0, beta)209immigration_curve_fixed = immigration_rate(S_gradient, near_large_dist, mainland_pool, I_0, alpha)210211# Generate species-area data with realistic parameters212# Simulate island chain with varying areas213island_areas = np.logspace(0, 4, 30) # 1 to 10,000 km^2214z_true = 0.26215c_true = 3.5216species_richness_true = species_area_law(island_areas, c_true, z_true)217218# Add biological noise (sampling variation, habitat heterogeneity)219noise_factor = 0.15220species_richness_observed = species_richness_true * (1 + noise_factor * np.random.randn(len(island_areas)))221species_richness_observed = np.maximum(species_richness_observed, 1) # Minimum 1 species222223# Fit species-area relationship224log_A = np.log10(island_areas)225log_S = np.log10(species_richness_observed)226z_fitted, log_c_fitted, r_value, p_value, std_err = linregress(log_A, log_S)227c_fitted = 10**log_c_fitted228r_squared = r_value**2229230# Time series simulation: colonization dynamics231time_years = np.linspace(0, 200, 500)232S_time = np.zeros_like(time_years)233S_time[0] = 0 # Start with empty island234235# Simulate colonization (Near Large island)236dt = time_years[1] - time_years[0]237for i in range(1, len(time_years)):238S_current = S_time[i-1]239I_rate = immigration_rate(S_current, near_large_dist, mainland_pool, I_0, alpha)240E_rate = extinction_rate(S_current, near_large_area, mainland_pool, E_0, beta)241dS_dt = I_rate - E_rate242S_time[i] = max(0, S_current + dS_dt * dt)243244# Relaxation simulation: habitat fragment isolation245S_relaxation = np.zeros_like(time_years)246S_relaxation[0] = equilibrium_species(near_large_dist, near_large_area, mainland_pool, I_0, E_0, alpha, beta)247248# After fragmentation: area reduced, distance increased249new_area = near_large_area / 10250new_distance = near_large_dist * 5251252for i in range(1, len(time_years)):253S_current = S_relaxation[i-1]254I_rate = immigration_rate(S_current, new_distance, mainland_pool, I_0, alpha)255E_rate = extinction_rate(S_current, new_area, mainland_pool, E_0, beta)256dS_dt = I_rate - E_rate257S_relaxation[i] = max(0, S_current + dS_dt * dt)258259# SLOSS comparison: one large vs several small reserves260total_area = 1000 # km^2261n_reserves_options = [1, 2, 5, 10, 20]262sloss_results = {}263for n in n_reserves_options:264area_per_reserve = total_area / n265distance_per_reserve = 100 # Assume moderate isolation266S_per_reserve = equilibrium_species(distance_per_reserve, area_per_reserve,267mainland_pool, I_0, E_0, alpha, beta)268# Total species (accounting for overlap: assume 70% similarity between reserves)269if n == 1:270total_species = S_per_reserve271else:272# Approximate total using species accumulation (not simple addition)273total_species = S_per_reserve * (1 + 0.3 * (n - 1))274sloss_results[n] = {'per_reserve': S_per_reserve, 'total': total_species}275\end{pycode}276277\begin{pycode}278# Create comprehensive figure279fig = plt.figure(figsize=(16, 12))280281# Plot 1: MacArthur-Wilson equilibrium model (Near Large island)282ax1 = fig.add_subplot(3, 3, 1)283ax1.plot(S_gradient, immigration_curve_near_large, 'b-', linewidth=2.5, label='Immigration I(S)')284ax1.plot(S_gradient, extinction_curve_near_large, 'r-', linewidth=2.5, label='Extinction E(S)')285S_eq_nl = equilibria['Near Large']286T_eq_nl = turnovers['Near Large']287ax1.plot(S_eq_nl, T_eq_nl, 'ko', markersize=10, label=f'Equilibrium ($S^* = {S_eq_nl:.1f}$)')288ax1.axvline(x=S_eq_nl, color='gray', linestyle='--', alpha=0.6)289ax1.axhline(y=T_eq_nl, color='gray', linestyle='--', alpha=0.6)290ax1.set_xlabel('Number of Species (S)', fontsize=11)291ax1.set_ylabel('Rate (species/year)', fontsize=11)292ax1.set_title('MacArthur-Wilson Equilibrium Model', fontsize=12, fontweight='bold')293ax1.legend(loc='upper right', fontsize=9)294ax1.grid(True, alpha=0.3)295ax1.set_xlim(0, mainland_pool)296ax1.set_ylim(0, max(immigration_curve_near_large.max(), extinction_curve_near_large.max()) * 1.1)297298# Plot 2: Distance effect on immigration299ax2 = fig.add_subplot(3, 3, 2)300ax2.plot(S_gradient, immigration_curve_near, 'b-', linewidth=2.5, label=f'Near ({near_large_dist} km)')301ax2.plot(S_gradient, immigration_curve_far, 'b--', linewidth=2.5, label=f'Far ({far_large_dist} km)')302ax2.plot(S_gradient, extinction_curve_fixed, 'r-', linewidth=2.5, label='Extinction (fixed)')303S_eq_near = equilibria['Near Large']304S_eq_far = equilibria['Far Large']305ax2.plot(S_eq_near, immigration_rate(S_eq_near, near_large_dist, mainland_pool, I_0, alpha),306'bo', markersize=9, label=f'$S^*_{{near}} = {S_eq_near:.1f}$')307ax2.plot(S_eq_far, immigration_rate(S_eq_far, far_large_dist, mainland_pool, I_0, alpha),308'bo', markersize=9, fillstyle='none', label=f'$S^*_{{far}} = {S_eq_far:.1f}$')309ax2.set_xlabel('Number of Species (S)', fontsize=11)310ax2.set_ylabel('Rate (species/year)', fontsize=11)311ax2.set_title('Distance Effect: Island Isolation', fontsize=12, fontweight='bold')312ax2.legend(loc='upper right', fontsize=8)313ax2.grid(True, alpha=0.3)314ax2.set_xlim(0, mainland_pool)315316# Plot 3: Area effect on extinction317ax3 = fig.add_subplot(3, 3, 3)318ax3.plot(S_gradient, extinction_curve_large, 'r-', linewidth=2.5, label=f'Large ({near_large_area} km$^2$)')319ax3.plot(S_gradient, extinction_curve_small, 'r--', linewidth=2.5, label=f'Small ({near_small_area} km$^2$)')320ax3.plot(S_gradient, immigration_curve_fixed, 'b-', linewidth=2.5, label='Immigration (fixed)')321S_eq_large = equilibria['Near Large']322S_eq_small = equilibria['Near Small']323ax3.plot(S_eq_large, extinction_rate(S_eq_large, near_large_area, mainland_pool, E_0, beta),324'ro', markersize=9, label=f'$S^*_{{large}} = {S_eq_large:.1f}$')325ax3.plot(S_eq_small, extinction_rate(S_eq_small, near_small_area, mainland_pool, E_0, beta),326'ro', markersize=9, fillstyle='none', label=f'$S^*_{{small}} = {S_eq_small:.1f}$')327ax3.set_xlabel('Number of Species (S)', fontsize=11)328ax3.set_ylabel('Rate (species/year)', fontsize=11)329ax3.set_title('Area Effect: Extinction Vulnerability', fontsize=12, fontweight='bold')330ax3.legend(loc='upper left', fontsize=8)331ax3.grid(True, alpha=0.3)332ax3.set_xlim(0, mainland_pool)333334# Plot 4: Species-area relationship (log-log)335ax4 = fig.add_subplot(3, 3, 4)336ax4.scatter(island_areas, species_richness_observed, s=60, c='forestgreen',337edgecolor='black', alpha=0.7, label='Observed islands')338A_fine = np.logspace(0, 4, 200)339S_fitted_curve = species_area_law(A_fine, c_fitted, z_fitted)340ax4.plot(A_fine, S_fitted_curve, 'r-', linewidth=2.5,341label=f'Fitted: $S = {c_fitted:.2f}A^{{{z_fitted:.3f}}}$')342S_true_curve = species_area_law(A_fine, c_true, z_true)343ax4.plot(A_fine, S_true_curve, 'k--', linewidth=2, alpha=0.5, label=f'True: $z = {z_true}$')344ax4.set_xscale('log')345ax4.set_yscale('log')346ax4.set_xlabel('Island Area (km$^2$)', fontsize=11)347ax4.set_ylabel('Species Richness (S)', fontsize=11)348ax4.set_title('Species-Area Relationship (Power Law)', fontsize=12, fontweight='bold')349ax4.legend(loc='lower right', fontsize=9)350ax4.grid(True, alpha=0.3, which='both')351352# Plot 5: Linearized species-area (log-log plot)353ax5 = fig.add_subplot(3, 3, 5)354ax5.scatter(log_A, log_S, s=60, c='forestgreen', edgecolor='black', alpha=0.7)355log_A_fine = np.linspace(log_A.min(), log_A.max(), 100)356log_S_fit = z_fitted * log_A_fine + log_c_fitted357ax5.plot(log_A_fine, log_S_fit, 'r-', linewidth=2.5,358label=f'$z = {z_fitted:.3f}$, $R^2 = {r_squared:.3f}$')359ax5.set_xlabel('log$_{10}$(Area)', fontsize=11)360ax5.set_ylabel('log$_{10}$(Species)', fontsize=11)361ax5.set_title('Linearized Species-Area Relationship', fontsize=12, fontweight='bold')362ax5.legend(loc='lower right', fontsize=9)363ax5.grid(True, alpha=0.3)364365# Plot 6: Colonization time series366ax6 = fig.add_subplot(3, 3, 6)367S_eq_target = equilibrium_species(near_large_dist, near_large_area, mainland_pool, I_0, E_0, alpha, beta)368ax6.plot(time_years, S_time, 'b-', linewidth=2.5, label='Species accumulation')369ax6.axhline(y=S_eq_target, color='red', linestyle='--', linewidth=2, label=f'Equilibrium ($S^* = {S_eq_target:.1f}$)')370ax6.fill_between(time_years, 0, S_time, alpha=0.2, color='blue')371ax6.set_xlabel('Time (years)', fontsize=11)372ax6.set_ylabel('Number of Species', fontsize=11)373ax6.set_title('Island Colonization Dynamics', fontsize=12, fontweight='bold')374ax6.legend(loc='lower right', fontsize=9)375ax6.grid(True, alpha=0.3)376ax6.set_xlim(0, 200)377ax6.set_ylim(0, mainland_pool * 1.1)378379# Plot 7: Relaxation after habitat fragmentation380ax7 = fig.add_subplot(3, 3, 7)381S_new_eq = equilibrium_species(new_distance, new_area, mainland_pool, I_0, E_0, alpha, beta)382ax7.plot(time_years, S_relaxation, 'r-', linewidth=2.5, label='Species loss')383ax7.axhline(y=S_new_eq, color='blue', linestyle='--', linewidth=2, label=f'New equilibrium ($S^* = {S_new_eq:.1f}$)')384ax7.axhline(y=S_relaxation[0], color='gray', linestyle=':', linewidth=1.5, alpha=0.7, label=f'Pre-fragmentation ($S = {S_relaxation[0]:.1f}$)')385ax7.fill_between(time_years, S_relaxation, S_relaxation[0], alpha=0.2, color='red')386ax7.set_xlabel('Time Since Fragmentation (years)', fontsize=11)387ax7.set_ylabel('Number of Species', fontsize=11)388ax7.set_title('Extinction Debt: Relaxation Dynamics', fontsize=12, fontweight='bold')389ax7.legend(loc='upper right', fontsize=9)390ax7.grid(True, alpha=0.3)391ax7.set_xlim(0, 200)392393# Plot 8: Four island types comparison394ax8 = fig.add_subplot(3, 3, 8)395scenario_names = list(scenarios.keys())396scenario_S = [equilibria[name] for name in scenario_names]397scenario_T = [turnovers[name] for name in scenario_names]398colors_scenarios = ['#2E7D32', '#1976D2', '#F57C00', '#C62828']399x_pos = np.arange(len(scenario_names))400bars = ax8.bar(x_pos, scenario_S, color=colors_scenarios, edgecolor='black', linewidth=1.5, alpha=0.8)401ax8.set_xticks(x_pos)402ax8.set_xticklabels(scenario_names, fontsize=10, rotation=15, ha='right')403ax8.set_ylabel('Equilibrium Species ($S^*$)', fontsize=11)404ax8.set_title('Island Type Comparison', fontsize=12, fontweight='bold')405ax8.grid(True, alpha=0.3, axis='y')406for i, (s, t) in enumerate(zip(scenario_S, scenario_T)):407ax8.text(i, s + 2, f'{s:.1f}', ha='center', fontsize=9, fontweight='bold')408409# Plot 9: SLOSS debate410ax9 = fig.add_subplot(3, 3, 9)411n_reserves = list(sloss_results.keys())412total_species_sloss = [sloss_results[n]['total'] for n in n_reserves]413species_per_reserve = [sloss_results[n]['per_reserve'] for n in n_reserves]414ax9.plot(n_reserves, total_species_sloss, 'o-', linewidth=2.5, markersize=8,415color='darkgreen', label='Total species (with overlap)')416ax9.plot(n_reserves, species_per_reserve, 's--', linewidth=2, markersize=7,417color='darkorange', label='Species per reserve')418ax9.set_xlabel('Number of Reserves', fontsize=11)419ax9.set_ylabel('Species Richness', fontsize=11)420ax9.set_title('SLOSS: Single Large vs Several Small', fontsize=12, fontweight='bold')421ax9.legend(loc='best', fontsize=9)422ax9.grid(True, alpha=0.3)423ax9.set_xticks(n_reserves)424425plt.tight_layout()426plt.savefig('island_biogeography_analysis.pdf', dpi=150, bbox_inches='tight')427plt.close()428\end{pycode}429430\begin{figure}[htbp]431\centering432\includegraphics[width=\textwidth]{island_biogeography_analysis.pdf}433\caption{Comprehensive island biogeography analysis: (a) MacArthur-Wilson equilibrium model showing434immigration and extinction rate curves intersecting at equilibrium species number $S^*$ with turnover435rate $T$; (b) Distance effect demonstrating reduced immigration rates for isolated islands, resulting436in lower equilibrium species richness; (c) Area effect showing elevated extinction rates on small islands437leading to reduced species persistence; (d) Species-area relationship fitted to simulated island chain438data, yielding power-law exponent $z \approx 0.26$ consistent with continental island systems; (e) Linearized439log-log plot enabling regression-based parameter estimation; (f) Colonization dynamics of an empty island440approaching equilibrium asymptotically over 200 years; (g) Relaxation dynamics following habitat fragmentation,441demonstrating extinction debt as species richness declines toward new lower equilibrium; (h) Comparison of442equilibrium species richness across four island scenarios varying in distance and area; (i) SLOSS debate443analysis showing conservation trade-offs between single large and several small nature reserves.}444\label{fig:biogeography}445\end{figure}446447\section{Results}448449\subsection{Equilibrium Species Richness}450451\begin{pycode}452print(r"\begin{table}[htbp]")453print(r"\centering")454print(r"\caption{Equilibrium Species Richness and Turnover Rates for Island Scenarios}")455print(r"\begin{tabular}{lcccc}")456print(r"\toprule")457print(r"Island Type & Distance (km) & Area (km$^2$) & $S^*$ & Turnover (sp/yr) \\")458print(r"\midrule")459460for name in ['Near Large', 'Near Small', 'Far Large', 'Far Small']:461dist, area = scenarios[name]462S_eq = equilibria[name]463T_eq = turnovers[name]464print(f"{name} & {dist} & {area} & {S_eq:.1f} & {T_eq:.3f} \\\\")465466print(r"\midrule")467print(f"Mainland pool ($P$) & --- & --- & {mainland_pool} & --- \\\\")468print(r"\bottomrule")469print(r"\end{tabular}")470print(r"\label{tab:equilibrium}")471print(r"\end{table}")472\end{pycode}473474\subsection{Species-Area Relationship}475476\begin{pycode}477print(r"\begin{table}[htbp]")478print(r"\centering")479print(r"\caption{Species-Area Relationship Parameter Estimates}")480print(r"\begin{tabular}{lccc}")481print(r"\toprule")482print(r"Parameter & True Value & Fitted Value & Error (\%) \\")483print(r"\midrule")484485z_error = abs(z_fitted - z_true) / z_true * 100486c_error = abs(c_fitted - c_true) / c_true * 100487488print(f"Scaling exponent ($z$) & {z_true:.3f} & {z_fitted:.3f} & {z_error:.1f} \\\\")489print(f"Coefficient ($c$) & {c_true:.2f} & {c_fitted:.2f} & {c_error:.1f} \\\\")490print(f"$R^2$ & --- & {r_squared:.4f} & --- \\\\")491print(r"\midrule")492print(f"Sample size & --- & {len(island_areas)} islands & --- \\\\")493print(r"\bottomrule")494print(r"\end{tabular}")495print(r"\label{tab:species_area}")496print(r"\end{table}")497\end{pycode}498499\subsection{Conservation Applications: SLOSS Analysis}500501\begin{pycode}502print(r"\begin{table}[htbp]")503print(r"\centering")504print(r"\caption{SLOSS Comparison: Reserve Design Trade-offs (Total Area = 1000 km$^2$)}")505print(r"\begin{tabular}{cccc}")506print(r"\toprule")507print(r"Reserves & Area Each (km$^2$) & Species/Reserve & Total Species \\")508print(r"\midrule")509510for n in n_reserves_options:511area_each = total_area / n512S_per = sloss_results[n]['per_reserve']513S_total = sloss_results[n]['total']514print(f"{n} & {area_each:.0f} & {S_per:.1f} & {S_total:.1f} \\\\")515516print(r"\bottomrule")517print(r"\end{tabular}")518print(r"\label{tab:sloss}")519print(r"\end{table}")520\end{pycode}521522\section{Discussion}523524\begin{example}[Distance and Area Effects]525The equilibrium model predicts that:526\begin{itemize}527\item \textbf{Near Large islands} ($D = \py{f"{near_large_dist}"} $ km, $A = \py{f"{near_large_area}"}$ km$^2$) reach highest species richness ($S^* = \py{f"{equilibria['Near Large']:.1f}"}$)528\item \textbf{Far Small islands} ($D = \py{f"{far_small_dist}"}$ km, $A = \py{f"{far_small_area}"}$ km$^2$) support fewest species ($S^* = \py{f"{equilibria['Far Small']:.1f}"}$)529\item Turnover rates vary inversely with equilibrium richness: isolated, small islands show high turnover relative to their low diversity530\end{itemize}531\end{example}532533\begin{remark}[Species-Area Scaling]534The fitted exponent $z = \py{f"{z_fitted:.3f}"}$ falls within the expected range for continental islands535($0.20 < z < 0.35$), confirming that larger islands support disproportionately more species through reduced536extinction rates and increased habitat diversity. The power-law form implies a 10-fold increase in area yields537approximately $10^{0.26} \approx 1.8$-fold increase in species richness.538\end{remark}539540\subsection{Colonization and Relaxation Dynamics}541542\begin{example}[Extinction Debt]543Following habitat fragmentation that reduces area from \py{f"{near_large_area}"} to \py{f"{new_area}"} km$^2$544and increases isolation from \py{f"{near_large_dist}"} to \py{f"{new_distance}"} km, species richness declines545from $S = \py{f"{S_relaxation[0]:.1f}"}$ to a new equilibrium $S^* = \py{f"{S_new_eq:.1f}"}$ over approximately546100 years. This extinction debt represents species temporarily persisting above carrying capacity, gradually547succumbing to increased extinction pressure.548\end{example}549550\subsection{Conservation Implications: The SLOSS Debate}551552\begin{remark}[Reserve Design Trade-offs]553The SLOSS analysis reveals:554\begin{itemize}555\item A single large reserve (\py{f"{total_area}"} km$^2$) supports $S = \py{f"{sloss_results[1]['total']:.1f}"}$ species556\item Ten small reserves (\py{f"{total_area/10:.0f}"} km$^2$ each) collectively support $S \approx \py{f"{sloss_results[10]['total']:.1f}"}$ species557\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 disturbance558\end{itemize}559Modern consensus favors large reserves for area-sensitive species (e.g., top predators) while recognizing that560multiple reserves can protect greater habitat diversity and provide insurance against localized extinctions.561\end{remark}562563\section{Conclusions}564565This computational analysis demonstrates the MacArthur-Wilson Theory of Island Biogeography as a quantitative framework566for understanding and predicting species richness patterns:567568\begin{enumerate}569\item Equilibrium species richness emerges from the balance between immigration and extinction, with near large islands570supporting $S^* = \py{f"{equilibria['Near Large']:.1f}"}$ species compared to $S^* = \py{f"{equilibria['Far Small']:.1f}"}$ for far small islands571\item The species-area relationship $S = cA^z$ yields a fitted exponent $z = \py{f"{z_fitted:.3f}"}$, consistent with572continental island biotas ($R^2 = \py{f"{r_squared:.3f}"}$)573\item Colonization dynamics show asymptotic approach to equilibrium over timescales of decades to centuries574\item Habitat fragmentation creates extinction debt, with species richness relaxing to lower equilibrium values as575isolation increases and area decreases576\item SLOSS analysis indicates that reserve design must balance single-reserve area effects against among-reserve577complementarity and risk-spreading578\end{enumerate}579580The equilibrium theory provides essential insights for conservation biology, particularly in designing nature reserve581networks and predicting biodiversity responses to habitat fragmentation and climate-driven range shifts.582583\section*{Further Reading}584585\begin{itemize}586\item MacArthur, R.H. \& Wilson, E.O. \textit{The Theory of Island Biogeography}. Princeton University Press, 1967.587\item Lomolino, M.V. ``Ecology's most general, yet protean pattern: the species-area relationship.'' \textit{Journal of Biogeography} 27:17--26 (2000).588\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).589\item Whittaker, R.J. \& Fern\'andez-Palacios, J.M. \textit{Island Biogeography: Ecology, Evolution, and Conservation}, 2nd ed. Oxford University Press, 2007.590\item Hanski, I. ``Metapopulation dynamics.'' \textit{Nature} 396:41--49 (1998).591\item Rosenzweig, M.L. \textit{Species Diversity in Space and Time}. Cambridge University Press, 1995.592\item Simberloff, D. \& Abele, L.G. ``Island biogeography theory and conservation practice.'' \textit{Science} 191:285--286 (1976).593\item Tjørve, E. ``Shapes and functions of species-area curves: a review of possible models.'' \textit{Journal of Biogeography} 30:827--835 (2003).594\item Losos, J.B. \& Ricklefs, R.E. (eds.) \textit{The Theory of Island Biogeography Revisited}. Princeton University Press, 2010.595\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).596\item Brooks, T.M. et al. ``Habitat loss and extinction in the hotspots of biodiversity.'' \textit{Conservation Biology} 16:909--923 (2002).597\item Holt, R.D. ``On the evolutionary ecology of species' ranges.'' \textit{Evolutionary Ecology Research} 5:159--178 (2003).598\item Hubbell, S.P. \textit{The Unified Neutral Theory of Biodiversity and Biogeography}. Princeton University Press, 2001.599\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).600\item Pimm, S.L. et al. ``The biodiversity of species and their rates of extinction, distribution, and protection.'' \textit{Science} 344:1246752 (2014).601\item Fahrig, L. ``Effects of habitat fragmentation on biodiversity.'' \textit{Annual Review of Ecology, Evolution, and Systematics} 34:487--515 (2003).602\item Triantis, K.A. et al. ``The island species-area relationship: biology and statistics.'' \textit{Journal of Biogeography} 39:215--231 (2012).603\item Hanski, I. \& Gaggiotti, O.E. (eds.) \textit{Ecology, Genetics and Evolution of Metapopulations}. Academic Press, 2004.604\item Schoener, T.W. ``The MacArthur-Wilson equilibrium model: A chronicle of what it said and how it was tested.'' In Losos \& Ricklefs, 2010.605\item Wilcox, B.A. \& Murphy, D.D. ``Conservation strategy: the effects of fragmentation on extinction.'' \textit{American Naturalist} 125:879--887 (1985).606\end{itemize}607608\end{document}609610611