TY - JOUR
T1 - Climate change impacts on mismatches between phytoplankton blooms and fish spawning phenology
AU - Asch, Rebecca G.
AU - Stock, Charles A.
AU - Sarmiento, Jorge L.
N1 - Funding Information:
This study was supported by the Nippon Foundation‐Nereus Program, the Princeton Environmental Institute, and the Alfred P. Sloan Foundation Research Fellowship Program. M. Long and B. Carter helped us obtain and process the SeaWiFS chlorophyll data used to assess the skill of ESM2M at modeling phytoplankton phe‐ nology. M.R. Tan contributed to this study by examining the sources of the model bias in Southern Ocean phytoplankton phenology. D. Tommasi, C. Petrik, M. Payne, and one additional anonymous re‐ viewer provided useful suggestions that improved the manuscript.
Funding Information:
This study was supported by the Nippon Foundation-Nereus Program, the Princeton Environmental Institute, and the Alfred P. Sloan Foundation Research Fellowship Program. M. Long and B. Carter helped us obtain and process the SeaWiFS chlorophyll data used to assess the skill of ESM2M at modeling phytoplankton phenology. M.R. Tan contributed to this study by examining the sources of the model bias in Southern Ocean phytoplankton phenology. D. Tommasi, C. Petrik, M. Payne, and one additional anonymous reviewer provided useful suggestions that improved the manuscript.
Publisher Copyright:
© 2019 John Wiley & Sons Ltd
PY - 2019/8
Y1 - 2019/8
N2 - Substantial interannual variability in marine fish recruitment (i.e., the number of young fish entering a fishery each year) has been hypothesized to be related to whether the timing of fish spawning matches that of seasonal plankton blooms. Environmental processes that control the phenology of blooms, such as stratification, may differ from those that influence fish spawning, such as temperature-linked reproductive maturation. These different controlling mechanisms could cause the timing of these events to diverge under climate change with negative consequences for fisheries. We use an earth system model to examine the impact of a high-emissions, climate-warming scenario (RCP8.5) on the future spawning time of two classes of temperate, epipelagic fishes: “geographic spawners” whose spawning grounds are defined by fixed geographic features (e.g., rivers, estuaries, reefs) and “environmental spawners” whose spawning grounds move responding to variations in environmental properties, such as temperature. By the century's end, our results indicate that projections of increased stratification cause spring and summer phytoplankton blooms to start 16 days earlier on average (±0.05 days SE) at latitudes >40°N. The temperature-linked phenology of geographic spawners changes at a rate twice as fast as phytoplankton, causing these fishes to spawn before the bloom starts across >85% of this region. “Extreme events,” defined here as seasonal mismatches >30 days that could lead to fish recruitment failure, increase 10-fold for geographic spawners in many areas under the RCP8.5 scenario. Mismatches between environmental spawners and phytoplankton were smaller and less widespread, although sizable mismatches still emerged in some regions. This indicates that range shifts undertaken by environmental spawners may increase the resiliency of fishes to climate change impacts associated with phenological mismatches, potentially buffering against declines in larval fish survival, recruitment, and fisheries. Our model results are supported by empirical evidence from ecosystems with multidecadal observations of both fish and phytoplankton phenology.
AB - Substantial interannual variability in marine fish recruitment (i.e., the number of young fish entering a fishery each year) has been hypothesized to be related to whether the timing of fish spawning matches that of seasonal plankton blooms. Environmental processes that control the phenology of blooms, such as stratification, may differ from those that influence fish spawning, such as temperature-linked reproductive maturation. These different controlling mechanisms could cause the timing of these events to diverge under climate change with negative consequences for fisheries. We use an earth system model to examine the impact of a high-emissions, climate-warming scenario (RCP8.5) on the future spawning time of two classes of temperate, epipelagic fishes: “geographic spawners” whose spawning grounds are defined by fixed geographic features (e.g., rivers, estuaries, reefs) and “environmental spawners” whose spawning grounds move responding to variations in environmental properties, such as temperature. By the century's end, our results indicate that projections of increased stratification cause spring and summer phytoplankton blooms to start 16 days earlier on average (±0.05 days SE) at latitudes >40°N. The temperature-linked phenology of geographic spawners changes at a rate twice as fast as phytoplankton, causing these fishes to spawn before the bloom starts across >85% of this region. “Extreme events,” defined here as seasonal mismatches >30 days that could lead to fish recruitment failure, increase 10-fold for geographic spawners in many areas under the RCP8.5 scenario. Mismatches between environmental spawners and phytoplankton were smaller and less widespread, although sizable mismatches still emerged in some regions. This indicates that range shifts undertaken by environmental spawners may increase the resiliency of fishes to climate change impacts associated with phenological mismatches, potentially buffering against declines in larval fish survival, recruitment, and fisheries. Our model results are supported by empirical evidence from ecosystems with multidecadal observations of both fish and phytoplankton phenology.
KW - earth system model
KW - marine fish reproduction
KW - phenology
KW - phytoplankton blooms
KW - species range shifts
KW - trophic mismatches
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U2 - 10.1111/gcb.14650
DO - 10.1111/gcb.14650
M3 - Article
C2 - 31152499
AN - SCOPUS:85066492835
SN - 1354-1013
VL - 25
SP - 2544
EP - 2559
JO - Global Change Biology
JF - Global Change Biology
IS - 8
ER -