Centro Oceanográfico de Canarias, Instituto Español de Oceanografía, Consejo Superior de Investigaciones Científicas (IEO-CSIC), 38180 Santa Cruz de Tenerife, Spain.
Centro Oceanográfico de Canarias, Instituto Español de Oceanografía, Consejo Superior de Investigaciones Científicas (IEO-CSIC), 38180 Santa Cruz de Tenerife, Spain; Universidad de La Laguna (ULL), 38200 San Cristóbal de La Laguna, Spain.
Sci Total Environ. 2024 Sep 20;944:173915. doi: 10.1016/j.scitotenv.2024.173915. Epub 2024 Jun 11.
The 2021 Tajogaite eruption in La Palma (Canary Islands, Spain) emitted vast volumes of lava during 85 days, which reached the ocean in several occasions at the western flank of the island. Most of these flows merged to create a primary lava delta, covering an area of 48 ha, with an additional 30 ha underwater. Here we characterize the effects of the lava-seawater interaction on the surrounding marine environment. The area was sampled during two multidisciplinary oceanographic cruises: the first one comprised the days before the lava reached the ocean and after the first contact; and the second took place a month later, when the lava delta was already formed but still receiving lava inputs. Physical-chemical anomalies were found in the whole water column at different depths up to 300 m in all measured parameters, such as turbidity (+9 NTU), dissolved oxygen concentration (-17.17 μmol kg), pH (-0.1), and chlorophyll-a concentration (-0.33 mg m). Surface temperature increased up to +2.3 °C (28.5 °C) and surface salinity showed increases and decreases of -1.01 and +0.70, respectively, in a radius of 4 km around the lava delta. In the water column, the heated waters experimented a lava-induced upwelling, bringing deeper, nutrient-rich waters to shallower depths; however, this feature did not trigger any phytoplankton bloom. In fact, integrated chlorophyll-a showed an abrupt decrease of -41 % in just two days and -69 % a month later, compared to prior conditions. The chlorophyll-a depletion reached a distance larger than 2.5 km (not delimited).
2021 年拉帕尔马(西班牙加那利群岛)的塔霍加泰火山喷发在 85 天内喷出了大量熔岩,其中多次在岛屿的西侧流入海洋。这些熔岩流大部分合并形成了一个主要的熔岩三角洲,覆盖面积为 48 公顷,另有 30 公顷位于水下。在这里,我们描述了熔岩与海水相互作用对周围海洋环境的影响。该地区在两次多学科海洋学考察中进行了采样:第一次是在熔岩到达海洋之前和第一次接触之后的几天;第二次是在一个月后进行的,当时熔岩三角洲已经形成,但仍在接收熔岩输入。在所有测量参数中,从最深处的 300 米到整个水柱中,都发现了物理化学异常,如浊度(+9 NTU)、溶解氧浓度(-17.17 μmol kg)、pH 值(-0.1)和叶绿素-a 浓度(-0.33 mg m)。在熔岩三角洲周围 4 公里的范围内,表层水温上升了+2.3°C(28.5°C),表层盐度分别增加了-1.01 和+0.70。在水柱中,受热的海水经历了由熔岩引起的上升流,将更深、营养更丰富的水带到了较浅的深度;然而,这一特征并没有引发浮游植物的大量繁殖。事实上,与之前的情况相比,在短短两天内,综合叶绿素-a 急剧下降了-41%,一个月后又下降了-69%。叶绿素-a 的消耗达到了超过 2.5 公里(无界限)的距离。