
基于时序特征参数的南极磷虾栖息地适宜性模型及长时序变化分析——以宇航员海与迪尔维尔海为例
谭亦杨, 白雁, 李腾, 郑芯瑜, 张银雪, 张异凡
海洋学研究 ›› 2024, Vol. 42 ›› Issue (4) : 43-57.
基于时序特征参数的南极磷虾栖息地适宜性模型及长时序变化分析——以宇航员海与迪尔维尔海为例
Antarctic krill habitat suitability modeling based on timing parameters and long-term change analysis: A case study in the Cosmonauts Sea and D’Urville Sea
南极磷虾(Euphausia superba)是维持南大洋生物多样性的关键物种,是南大洋的重点保护与限制捕捞对象。在气候变化对南大洋生态环境持续显著影响的背景下,亟需了解南极磷虾的时空分布、变化趋势及其栖息地适宜性。本文基于南极磷虾出现记录及长时序遥感与再分析数据,利用藻华物候与海冰消长的时序特征参数及相关环境参数,构建了宇航员海与迪尔维尔海南极磷虾栖息地适宜性的最大熵模型(Maxent)。研究发现,相较于常规单一时刻环境参数,时序特征参数更适合用于南极磷虾栖息地适宜性评估。基于Maxent模型,反演了两个典型海域超过20年的南极磷虾出现时间和频率变化序列,并通过分析多个环境参数的年际变化趋势进行机制解释。南极磷虾出现时的环境参数显示,宇航员海整体叶绿素质量浓度低于迪尔维尔海,无冰期更短,温度更低,南极磷虾出现时间更晚,且主要由沿岸区域的南极磷虾幼体与年轻个体构成。在1997—2019年,宇航员海沿岸区域磷虾出现时间逐渐提前,出现总天数逐年增多,主要是由于沿岸区域藻华起始时间提前,同时叶绿素质量浓度增加也为南极磷虾幼体提供了更充足的食物来源。迪尔维尔海受海水增温、无冰期缩短、叶绿素质量浓度降低等环境变化趋势的影响,该区域磷虾成熟个体或向更适宜环境迁移,南极磷虾每年出现总天数下降。在模型构建基础上,本研究首次获得了宇航员海与迪尔维尔海的南极磷虾长时序分布数据,可为了解气候变化对南大洋生物的影响、南大洋保护区规划与渔业管理提供科学依据。
Antarctic krill (Euphausia superba) is a key species sustaining the biodiversity of the Southern Ocean and is a protected and restricted fishing target. In the context of significant impacts of climate change on the ecological environment of the Southern Ocean, it is urgent to understand the spatio-temporal distribution, change trends, and habitat suitability of Antarctic krill. In this study, based on Antarctic krill presence records and time series satellite and reanalysis data, a Maxent model for habitat suitability in the Cosmonauts Sea and the D’Urville Sea were constructed using timing parameters of phytoplankton phenology and sea-ice dynamics, along with related environmental parameters. It was found that timing parameters were more suitable for assessing habitat suitability for Antarctic krill compared to conventional environmental parameters. Using the Maxent model, the data over 20 years on the occurrence time and frequency of Antarctic krill in these two study areas were retrieved, and the mechanisms through the interannual trends of multiple environmental parameters were analyzed. Environmental parameters at the time of krill occurrence showed that the overall chlorophyll a mass concentration in the Cosmonauts Sea was lower than that in the D’Urville Sea, with a shorter ice-free period, lower temperatures, and later krill presence dates primarily composed of larval and young individuals along the coast. From 1997 to 2019, the presence time of krill in the coastal Cosmonauts Sea gradually advanced, and the number of presence days increased, mainly due to earlier onset of algal blooms, while increased chlorophyll a mass concentration provided more abundant overwintering food for krill larvae. In the D’Urville Sea, influenced by warming water, shortened ice-free period, and reduced chlorophyll a mass concentration, mature krill may migrate to a more suitable environment, leading to a decline in annual presence frequency. Based on the constructed habitat suitability model, this study showed the long-term distribution of Antarctic krill occurrence in the Cosmonauts Sea and the D’Urville Sea for the first time, which can help to understand the impact of climate change on the ecological environment in the Southern Ocean, and the planning of conservation areas and fishery management in the Southern Ocean.
南极磷虾 / 栖息地适宜性 / 海冰密集度 / 卫星遥感 / 时间序列参数 / 最大熵模型 / 宇航员海 / 迪尔维尔海
Antarctic krill (Euphausia superba) / habitat suitability / sea ice concentration / satellite remote sensing / timing parameters / maximum entropy model (Maxent) / Cosmonauts Sea / D’Urville Sea
[1] |
|
[2] |
|
[3] |
Antarctic krill (Euphausia superba) are swarming, oceanic crustaceans, up to two inches long, and best known as prey for whales and penguins - but they have another important role. With their large size, high biomass and daily vertical migrations they transport and transform essential nutrients, stimulate primary productivity and influence the carbon sink. Antarctic krill are also fished by the Southern Ocean's largest fishery. Yet how krill fishing impacts nutrient fertilisation and the carbon sink in the Southern Ocean is poorly understood. Our synthesis shows fishery management should consider the influential biogeochemical role of both adult and larval Antarctic krill.
|
[4] |
|
[5] |
|
[6] |
|
[7] |
|
[8] |
|
[9] |
|
[10] |
|
[11] |
|
[12] |
|
[13] |
|
[14] |
|
[15] |
朱国平. 基于广义可加模型研究时间和环境因子对南极半岛北部南极磷虾渔场的影响[J]. 水产学报, 2012, 36(12):1863-1871.
|
[16] |
|
[17] |
|
[18] |
|
[19] |
|
[20] |
|
[21] |
|
[22] |
|
[23] |
|
[24] |
|
[25] |
|
[26] |
GBIF occurrence download[DS/OL]. (2022-2-09) [2023-2-09]. https://doi.org/10.15468/dl.28z24e
|
[27] |
CCAMLR. Precautionary catch limitation on Euphausia superba in Statistical Division 58.4.2[Z/OL]. [2023-2-09]. https://cm.ccamlr.org/en/measure-51-03-2008
|
[28] |
|
[29] |
|
[30] |
|
[31] |
|
[32] |
|
[33] |
|
[34] |
|
[35] |
|
[36] |
|
[37] |
|
[38] |
|
[39] |
|
[40] |
|
[41] |
|
[42] |
|
[43] |
|
[44] |
|
[45] |
Oxygen loss in the ocean, termed deoxygenation, is a major consequence of climate change and is exacerbated by other aspects of global change. An average global loss of 2% or more has been recorded in the open ocean over the past 50-100 years, but with greater oxygen declines in intermediate waters (100-600 m) of the North Pacific, the East Pacific, tropical waters, and the Southern Ocean. Although ocean warming contributions to oxygen declines through a reduction in oxygen solubility and stratification effects on ventilation are reasonably well understood, it has been a major challenge to identify drivers and modifying factors that explain different regional patterns, especially in the tropical oceans. Changes in respiration, circulation (including upwelling), nutrient inputs, and possibly methane release contribute to oxygen loss, often indirectly through stimulation of biological production and biological consumption. Microbes mediate many feedbacks in oxygen minimum zones that can either exacerbate or ameliorate deoxygenation via interacting nitrogen, sulfur, and carbon cycles. The paleo-record reflects drivers of and feedbacks to deoxygenation that have played out through the Phanerozoic on centennial, millennial, and hundred-million-year timescales. Natural oxygen variability has made it difficult to detect the emergence of a climate-forced signal of oxygen loss, but new modeling efforts now project emergence to occur in many areas in 15-25 years. Continued global deoxygenation is projected for the next 100 or more years under most emissions scenarios, but with regional heterogeneity. Notably, even small changes in oxygenation can have significant biological effects. New efforts to systematically observe oxygen changes throughout the open ocean are needed to help address gaps in understanding of ocean deoxygenation patterns and drivers.
|
[46] |
|
[47] |
|
[48] |
|
[49] |
|
[50] |
|
[51] |
|
/
〈 |
|
〉 |